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[
"Shoshone Lake",
"country",
"United States of America"
] |
Shoshone Lake is a U.S. backcountry lake with an area of 8,050 acres (33 km2; 13 sq mi) with an elevation of 7,795 feet (2,376 m) in the southwest section of Yellowstone National Park, Wyoming. It lies at the headwaters of the Lewis River, a tributary of the Snake River. The U.S. Fish and Wildlife Service believes that Shoshone Lake is the largest backcountry lake in the lower 48 states that cannot be reached by a road. The Yellowstone Caldera is located within the lake.[1]
| 0
|
[
"Shoshone Lake",
"located in protected area",
"Yellowstone National Park"
] |
Shoshone Lake is a U.S. backcountry lake with an area of 8,050 acres (33 km2; 13 sq mi) with an elevation of 7,795 feet (2,376 m) in the southwest section of Yellowstone National Park, Wyoming. It lies at the headwaters of the Lewis River, a tributary of the Snake River. The U.S. Fish and Wildlife Service believes that Shoshone Lake is the largest backcountry lake in the lower 48 states that cannot be reached by a road. The Yellowstone Caldera is located within the lake.[1]
| 3
|
[
"Shoshone Lake",
"instance of",
"lake"
] |
Shoshone Lake is a U.S. backcountry lake with an area of 8,050 acres (33 km2; 13 sq mi) with an elevation of 7,795 feet (2,376 m) in the southwest section of Yellowstone National Park, Wyoming. It lies at the headwaters of the Lewis River, a tributary of the Snake River. The U.S. Fish and Wildlife Service believes that Shoshone Lake is the largest backcountry lake in the lower 48 states that cannot be reached by a road. The Yellowstone Caldera is located within the lake.[1]
| 4
|
[
"Grand Canyon of the Yellowstone",
"located in protected area",
"Yellowstone National Park"
] |
The Grand Canyon of the Yellowstone is the first large canyon on the Yellowstone River downstream from Yellowstone Falls in Yellowstone National Park in Wyoming. The canyon is approximately 24 miles (39 km) long, between 800 and 1,200 ft (240 and 370 m) deep and from .25 to .75 mi (0.40 to 1.21 km) wide.History
Although trappers and prospectors who visited the Yellowstone region had knowledge of the canyon, the first significant descriptions were publicized after the Cook–Folsom–Peterson Expedition of 1869 and the Washburn-Langford-Doane Expedition of 1870.
When Charles W. Cook first viewed the canyon after traveling west from the Lamar Valley on September 20, 1869, he subsequently wrote these words in his journal:
| 2
|
[
"Grand Canyon of the Yellowstone",
"instance of",
"canyon"
] |
The Grand Canyon of the Yellowstone is the first large canyon on the Yellowstone River downstream from Yellowstone Falls in Yellowstone National Park in Wyoming. The canyon is approximately 24 miles (39 km) long, between 800 and 1,200 ft (240 and 370 m) deep and from .25 to .75 mi (0.40 to 1.21 km) wide.History
Although trappers and prospectors who visited the Yellowstone region had knowledge of the canyon, the first significant descriptions were publicized after the Cook–Folsom–Peterson Expedition of 1869 and the Washburn-Langford-Doane Expedition of 1870.
When Charles W. Cook first viewed the canyon after traveling west from the Lamar Valley on September 20, 1869, he subsequently wrote these words in his journal:
| 4
|
[
"Great Fountain Geyser",
"located in protected area",
"Yellowstone National Park"
] |
The Great Fountain Geyser is a fountain-type geyser located in the Firehole Lake area of Lower Geyser Basin of Yellowstone National Park, Wyoming. It is the only Lower Geyser Basin feature that the park makes predictions for.
| 1
|
[
"Great Fountain Geyser",
"instance of",
"geyser"
] |
The Great Fountain Geyser is a fountain-type geyser located in the Firehole Lake area of Lower Geyser Basin of Yellowstone National Park, Wyoming. It is the only Lower Geyser Basin feature that the park makes predictions for.Eruption
The geyser erupts every 9 to 15 hours. Great Fountain's maximum height ranges from about 75 feet (23 m) to over 220 feet (67 m). Its duration is usually about one hour but durations of over two hours have been seen. The duration of an eruption affects the interval that will elapse before the next eruption, so that if the duration of an eruption is recorded, the time of the following eruption can be predicted to a precision of about two hours. The prediction can be refined, to plus or minus 15 minutes or so, through observation of overflow from the crater during the period between eruptions. While this pattern of behavior is observed most of the time, there are occasional episodes of so-called "wild-phase" activity during which the eruptions are of greatly extended duration and intervals between eruptions may be as long as three days. The geyser is then unpredictable until wild-phase activity ceases and more normal eruptions resume.
Nearby White Dome Geyser, which erupts considerably more frequently (albeit less powerfully) from a large geyserite cone, is easily seen from the same parking lot that affords a viewpoint for Great Fountain. The thermophilic bacterium Thermus aquaticus, important because it produces an enzyme used in polymerase chain reaction laboratory procedures central to modern molecular biology, was first isolated from Mushroom Pool, a non-eruptive hot spring a few hundred feet from White Dome Geyser.
| 3
|
[
"Heart Lake (Wyoming)",
"located in protected area",
"Yellowstone National Park"
] |
Heart Lake el. 7,461 feet (2,274 m) is a large backcountry lake, nestled at the base of Mount Sheridan in Yellowstone National Park. Heart Lake is in the Snake River drainage and is drained by the Heart River.
| 1
|
[
"Heart Lake (Wyoming)",
"instance of",
"lake"
] |
Heart Lake el. 7,461 feet (2,274 m) is a large backcountry lake, nestled at the base of Mount Sheridan in Yellowstone National Park. Heart Lake is in the Snake River drainage and is drained by the Heart River.History
Heart Lake was apparently named sometime prior to 1871 for a local 1840s hunter, Hart Hunney, a fact that was later verified by Hiram Chittenden. In 1871, Captain John W. Barlow thought the name was Heart Lake because of it shape and the name became its official name. During the Arnold Hague Geologic Surveys, Chittenden petitioned Hague to change the name back to Hart, but Hague thought that Heart Lake was named because of the lake's shape and refused to change it. In 1870 a member of the Washburn-Langford-Doane Expedition, the solitary explorer Truman C. Everts, who had become separated from the rest of his party, probably camped on the shores of Heart Lake and named it Bessie Lake after his daughter.
| 4
|
[
"Lewis Lake (Wyoming)",
"country",
"United States of America"
] |
Lewis Lake is located in the U. S. state of Wyoming in the southern part of Yellowstone National Park, about 4 miles (6.4 km) southeast of Shoshone Lake, and approximately 10 miles (16 km) southwest of Yellowstone Lake. Lewis Lake and Shoshone Lake are both located a few miles northeast of the Pitchstone Plateau.The Lewis River is the lake's primary inflow, draining south from Shoshone Lake. The primary outflow of Lewis Lake is also the Lewis River, continuing south to join the Snake River near the southern boundary of Yellowstone National Park. A few small creeks also feed Lewis Lake. There are several hot springs emptying into the lake on its northwestern shore and two more hot springs at the lake's southern end where it empties into the Lewis River. A campground is located on the lake's southeast shore. Yellowstone National Park's South Entrance Road (which is also numbered as U.S. Route 287, U.S. Route 89, and U.S. Route 191), run along the east side of Lewis Lake.Like the river, Lewis Lake is named for Meriweather Lewis, commander of the Lewis and Clark ExpeditionLewis lake holds brown, brook and lake trout and falls within the non-native trout tolerance area of the park. Anglers may keep up to five non-native trout per day but only one brown trout.
| 0
|
[
"Lewis Lake (Wyoming)",
"located in protected area",
"Yellowstone National Park"
] |
Lewis Lake is located in the U. S. state of Wyoming in the southern part of Yellowstone National Park, about 4 miles (6.4 km) southeast of Shoshone Lake, and approximately 10 miles (16 km) southwest of Yellowstone Lake. Lewis Lake and Shoshone Lake are both located a few miles northeast of the Pitchstone Plateau.The Lewis River is the lake's primary inflow, draining south from Shoshone Lake. The primary outflow of Lewis Lake is also the Lewis River, continuing south to join the Snake River near the southern boundary of Yellowstone National Park. A few small creeks also feed Lewis Lake. There are several hot springs emptying into the lake on its northwestern shore and two more hot springs at the lake's southern end where it empties into the Lewis River. A campground is located on the lake's southeast shore. Yellowstone National Park's South Entrance Road (which is also numbered as U.S. Route 287, U.S. Route 89, and U.S. Route 191), run along the east side of Lewis Lake.Like the river, Lewis Lake is named for Meriweather Lewis, commander of the Lewis and Clark ExpeditionLewis lake holds brown, brook and lake trout and falls within the non-native trout tolerance area of the park. Anglers may keep up to five non-native trout per day but only one brown trout.
| 2
|
[
"Lewis Lake (Wyoming)",
"instance of",
"lake"
] |
Lewis Lake is located in the U. S. state of Wyoming in the southern part of Yellowstone National Park, about 4 miles (6.4 km) southeast of Shoshone Lake, and approximately 10 miles (16 km) southwest of Yellowstone Lake. Lewis Lake and Shoshone Lake are both located a few miles northeast of the Pitchstone Plateau.The Lewis River is the lake's primary inflow, draining south from Shoshone Lake. The primary outflow of Lewis Lake is also the Lewis River, continuing south to join the Snake River near the southern boundary of Yellowstone National Park. A few small creeks also feed Lewis Lake. There are several hot springs emptying into the lake on its northwestern shore and two more hot springs at the lake's southern end where it empties into the Lewis River. A campground is located on the lake's southeast shore. Yellowstone National Park's South Entrance Road (which is also numbered as U.S. Route 287, U.S. Route 89, and U.S. Route 191), run along the east side of Lewis Lake.Like the river, Lewis Lake is named for Meriweather Lewis, commander of the Lewis and Clark ExpeditionLewis lake holds brown, brook and lake trout and falls within the non-native trout tolerance area of the park. Anglers may keep up to five non-native trout per day but only one brown trout.
| 4
|
[
"Mount Everts",
"located in protected area",
"Yellowstone National Park"
] |
Mount Everts, elevation 7,846 feet (2,391 m), is a prominent mountain peak in Yellowstone National Park, Wyoming, near Mammoth Hot Springs. The peak was named for Truman C. Everts, a member of the Washburn–Langford–Doane Expedition of 1870. Mount Everts is located immediately due south of Gardiner, Montana and due east of Mammoth Hot Springs.History
Mount Everts was named by Henry D. Washburn shortly after the rescue of Truman C. Everts, who had been lost for 37 days in Yellowstone at the conclusion of the Washburn Expedition. During the expedition, Washburn named a peak (now called Mount Sheridan ) in the Thorofare region south of Yellowstone Lake for Everts but later changed it to the current peak, believing it was very near the location of Everts' rescue. Everts was in fact rescued a few miles to the northeast, near where Blacktail Deer Creek enters the Yellowstone River at the northern park boundary, and the mountain is the dominant feature separating what is now known as Gardiner from the northerly flowing Yellowstone River. Mr. Everts complained until his death that the far more grand Mount Sheridan should have been named after him.
| 1
|
[
"Mount Everts",
"located in the administrative territorial entity",
"Wyoming"
] |
Mount Everts, elevation 7,846 feet (2,391 m), is a prominent mountain peak in Yellowstone National Park, Wyoming, near Mammoth Hot Springs. The peak was named for Truman C. Everts, a member of the Washburn–Langford–Doane Expedition of 1870. Mount Everts is located immediately due south of Gardiner, Montana and due east of Mammoth Hot Springs.
| 2
|
[
"Mount Everts",
"instance of",
"mountain"
] |
Mount Everts, elevation 7,846 feet (2,391 m), is a prominent mountain peak in Yellowstone National Park, Wyoming, near Mammoth Hot Springs. The peak was named for Truman C. Everts, a member of the Washburn–Langford–Doane Expedition of 1870. Mount Everts is located immediately due south of Gardiner, Montana and due east of Mammoth Hot Springs.History
Mount Everts was named by Henry D. Washburn shortly after the rescue of Truman C. Everts, who had been lost for 37 days in Yellowstone at the conclusion of the Washburn Expedition. During the expedition, Washburn named a peak (now called Mount Sheridan ) in the Thorofare region south of Yellowstone Lake for Everts but later changed it to the current peak, believing it was very near the location of Everts' rescue. Everts was in fact rescued a few miles to the northeast, near where Blacktail Deer Creek enters the Yellowstone River at the northern park boundary, and the mountain is the dominant feature separating what is now known as Gardiner from the northerly flowing Yellowstone River. Mr. Everts complained until his death that the far more grand Mount Sheridan should have been named after him.
| 3
|
[
"Spindle Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Spindle Geyser is a geyser in the Lower Geyser Basin of Yellowstone National Park in the U.S. state of Wyoming.
Spindle Geyser is part of the White Creek Group which includes A-0 Geyser and Botryoidal Spring. It is found along the bank of White Creek about 1⁄2 mile (0.8 km) southeast of the Surprise Pool parking area.It erupts for a duration of a few seconds with an interval of 1–3 minutes between eruptions. Eruptions tend to be small, sometimes no more than a vigorous roiling of the pool but can reach 1 to 3 feet (0.3 to 0.9 m). Prior to 1985, Spindle had eruptions as large as 10 feet (3.0 m). Spindle also generates subterranean thumps that can be felt when standing near the geyser.
| 1
|
[
"Narcissus Geyser",
"country",
"United States of America"
] |
Narcissus Geyser is a geyser in the Lower Geyser Basin of Yellowstone National Park in the United States. Narcissus Geyser is part of the Pink Cone Group. Other geysers in this group are Bead Geyser, Box Spring, Dilemma Geyser, Labial Geyser, Labial's Satellite Geyser, Pink Geyser, and Pink Cone Geyser.
| 0
|
[
"Narcissus Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Narcissus Geyser is a geyser in the Lower Geyser Basin of Yellowstone National Park in the United States. Narcissus Geyser is part of the Pink Cone Group. Other geysers in this group are Bead Geyser, Box Spring, Dilemma Geyser, Labial Geyser, Labial's Satellite Geyser, Pink Geyser, and Pink Cone Geyser.
| 1
|
[
"North Entrance Road Historic District",
"country",
"United States of America"
] |
The North Entrance Road Historic District comprises Yellowstone National Park's North Entrance Road from Gardiner, Montana to the park headquarters at Mammoth Hot Springs, Wyoming, a distance of a little over five miles (8 km). The North Entrance Road was the first major road in the park, necessary to join the U.S. Army station at Fort Yellowstone to the Northern Pacific Railroad station at Gardiner. The road includes the Roosevelt Arch at the northern boundary of the park and winds through rolling terrain before crossing the Gardner River and joining the Grand Loop Road.The North Entrance Road is an unsigned portion of US 89.
| 0
|
[
"North Entrance Road Historic District",
"continent",
"North America"
] |
The North Entrance Road Historic District comprises Yellowstone National Park's North Entrance Road from Gardiner, Montana to the park headquarters at Mammoth Hot Springs, Wyoming, a distance of a little over five miles (8 km). The North Entrance Road was the first major road in the park, necessary to join the U.S. Army station at Fort Yellowstone to the Northern Pacific Railroad station at Gardiner. The road includes the Roosevelt Arch at the northern boundary of the park and winds through rolling terrain before crossing the Gardner River and joining the Grand Loop Road.The North Entrance Road is an unsigned portion of US 89.
| 1
|
[
"North Entrance Road Historic District",
"located in protected area",
"Yellowstone National Park"
] |
The North Entrance Road Historic District comprises Yellowstone National Park's North Entrance Road from Gardiner, Montana to the park headquarters at Mammoth Hot Springs, Wyoming, a distance of a little over five miles (8 km). The North Entrance Road was the first major road in the park, necessary to join the U.S. Army station at Fort Yellowstone to the Northern Pacific Railroad station at Gardiner. The road includes the Roosevelt Arch at the northern boundary of the park and winds through rolling terrain before crossing the Gardner River and joining the Grand Loop Road.The North Entrance Road is an unsigned portion of US 89.
| 2
|
[
"North Entrance Road Historic District",
"instance of",
"historic district"
] |
The North Entrance Road Historic District comprises Yellowstone National Park's North Entrance Road from Gardiner, Montana to the park headquarters at Mammoth Hot Springs, Wyoming, a distance of a little over five miles (8 km). The North Entrance Road was the first major road in the park, necessary to join the U.S. Army station at Fort Yellowstone to the Northern Pacific Railroad station at Gardiner. The road includes the Roosevelt Arch at the northern boundary of the park and winds through rolling terrain before crossing the Gardner River and joining the Grand Loop Road.The North Entrance Road is an unsigned portion of US 89.
| 7
|
[
"North Entrance Road Historic District",
"heritage designation",
"National Register of Historic Places listed place"
] |
The North Entrance Road Historic District comprises Yellowstone National Park's North Entrance Road from Gardiner, Montana to the park headquarters at Mammoth Hot Springs, Wyoming, a distance of a little over five miles (8 km). The North Entrance Road was the first major road in the park, necessary to join the U.S. Army station at Fort Yellowstone to the Northern Pacific Railroad station at Gardiner. The road includes the Roosevelt Arch at the northern boundary of the park and winds through rolling terrain before crossing the Gardner River and joining the Grand Loop Road.The North Entrance Road is an unsigned portion of US 89.
| 8
|
[
"Opal Pool",
"located in protected area",
"Yellowstone National Park"
] |
Opal Pool is a hot spring in the Midway Geyser Basin of Yellowstone National Park, Wyoming. Opal Pool usually has a temperature of approximately 132 °F (56 °C). Though usually active as a hot spring, Opal Pool is considered a fountain-type geyser.The first recorded eruption of Opal Pool was in 1947, recurring in 1949, 1952 and 1953, then ceasing. Eruptions resumed in 1979, happening at least once in most following years. Eruption heights are typically under 30 feet (9.1 m) in height, but some eruptions have been seen with heights of 70 feet (21 m) to 80 feet (24 m). Eruptions occur suddenly following visible convection in the pool, but are unpredictable. An eruption consists of one, huge, burst that throws water 20–80 feet high, making Opal Pool the largest active geyser at Midway Geyser Basin. Much smaller splashes seconds apart stretch the total duration to about 1 minute. In 2005 Opal completely drained, but refilled as a vivid green pool in 2008.
| 1
|
[
"Opal Pool",
"located in the administrative territorial entity",
"Wyoming"
] |
Opal Pool is a hot spring in the Midway Geyser Basin of Yellowstone National Park, Wyoming. Opal Pool usually has a temperature of approximately 132 °F (56 °C). Though usually active as a hot spring, Opal Pool is considered a fountain-type geyser.The first recorded eruption of Opal Pool was in 1947, recurring in 1949, 1952 and 1953, then ceasing. Eruptions resumed in 1979, happening at least once in most following years. Eruption heights are typically under 30 feet (9.1 m) in height, but some eruptions have been seen with heights of 70 feet (21 m) to 80 feet (24 m). Eruptions occur suddenly following visible convection in the pool, but are unpredictable. An eruption consists of one, huge, burst that throws water 20–80 feet high, making Opal Pool the largest active geyser at Midway Geyser Basin. Much smaller splashes seconds apart stretch the total duration to about 1 minute. In 2005 Opal completely drained, but refilled as a vivid green pool in 2008.
| 2
|
[
"Opal Pool",
"instance of",
"hot spring"
] |
Opal Pool is a hot spring in the Midway Geyser Basin of Yellowstone National Park, Wyoming. Opal Pool usually has a temperature of approximately 132 °F (56 °C). Though usually active as a hot spring, Opal Pool is considered a fountain-type geyser.The first recorded eruption of Opal Pool was in 1947, recurring in 1949, 1952 and 1953, then ceasing. Eruptions resumed in 1979, happening at least once in most following years. Eruption heights are typically under 30 feet (9.1 m) in height, but some eruptions have been seen with heights of 70 feet (21 m) to 80 feet (24 m). Eruptions occur suddenly following visible convection in the pool, but are unpredictable. An eruption consists of one, huge, burst that throws water 20–80 feet high, making Opal Pool the largest active geyser at Midway Geyser Basin. Much smaller splashes seconds apart stretch the total duration to about 1 minute. In 2005 Opal completely drained, but refilled as a vivid green pool in 2008.
| 3
|
[
"Lion Geyser",
"country",
"United States of America"
] |
Lion Geyser is a cone-type geyser in the Upper Geyser Basin of Yellowstone National Park in the United States. It is located in the Geyser Hill complex.It was named for the roaring sound of steam releasing during an eruption. Eruptions can reach 90 feet (27 m) and last from 1 to 7 minutes. Lion is the largest of the Lion Group which includes Little Cub Geyser and the currently inactive Big Cub and Lioness geysers.
| 0
|
[
"Lion Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Lion Geyser is a cone-type geyser in the Upper Geyser Basin of Yellowstone National Park in the United States. It is located in the Geyser Hill complex.It was named for the roaring sound of steam releasing during an eruption. Eruptions can reach 90 feet (27 m) and last from 1 to 7 minutes. Lion is the largest of the Lion Group which includes Little Cub Geyser and the currently inactive Big Cub and Lioness geysers.
| 1
|
[
"Lion Geyser",
"instance of",
"geyser"
] |
Lion Geyser is a cone-type geyser in the Upper Geyser Basin of Yellowstone National Park in the United States. It is located in the Geyser Hill complex.It was named for the roaring sound of steam releasing during an eruption. Eruptions can reach 90 feet (27 m) and last from 1 to 7 minutes. Lion is the largest of the Lion Group which includes Little Cub Geyser and the currently inactive Big Cub and Lioness geysers.
| 2
|
[
"Red Cloud's War",
"participant",
"United States of America"
] |
Red Cloud's War (also referred to as the Bozeman War or the Powder River War) was an armed conflict between an alliance of the Lakota, Northern Cheyenne, and Northern Arapaho peoples against the United States and the Crow Nation that took place in the Wyoming and Montana territories from 1866 to 1868. The war was fought over control of the western Powder River Country in present north-central Wyoming.
In 1863, European Americans had blazed the Bozeman Trail through the heart of the traditional territory of the Cheyenne, Arapaho, and Lakota. It was the shortest and easiest route from Fort Laramie and the Oregon Trail to the Montana gold fields. From 1864 to 1866, the trail was traversed by about 3,500 miners, emigrant settlers and others, who competed with the Indians for the diminishing resources near the trail.The United States named the war after Red Cloud, a prominent Oglala Lakota chief allied with the Cheyenne and Arapaho. The United States army had built forts in response to attacks on civilian travelers, using a treaty right to "establish roads, military and other post". All three forts were located in 1851 Crow Indian territory and accepted by these Indians. The Crow believed they guarded their interests best by cooperating with the US army.Red Cloud's War consisted mostly of constant small-scale Indian raids and attacks on the soldiers and civilians at the three forts in the Powder River country, wearing down those garrisons. The largest action of the war, the Fetterman Fight (with 81 men killed on the U.S. side), was the worst military defeat suffered by the U.S. on the Great Plains until the Battle of the Little Bighorn in the Crow Indian reservation ten years later. " ... the most dramatic battles between the army and the Dakota [in the 1860s and 1870s] were on lands those Indians had taken from other tribes since 1851."With peace achieved under the Treaty of Fort Laramie in 1868, the Lakota and their allies were victorious. They gained legal control of the western Powder River country, took down the forts and permanently closed the Bozeman trail. The Crow lost their hunting grounds in the Powder River region to their enemies. With the treaty, "... the [United States] government had in effect betrayed the Crows, who had willingly helped the army to hold the posts for two years". The victory of the Lakota and their allies, however, only endured for eight years until the Great Sioux War of 1876, when the US started to take some of their territories again, including the sacred Black Hills.
| 1
|
[
"Red Cloud's War",
"instance of",
"war"
] |
Red Cloud's War (also referred to as the Bozeman War or the Powder River War) was an armed conflict between an alliance of the Lakota, Northern Cheyenne, and Northern Arapaho peoples against the United States and the Crow Nation that took place in the Wyoming and Montana territories from 1866 to 1868. The war was fought over control of the western Powder River Country in present north-central Wyoming.
In 1863, European Americans had blazed the Bozeman Trail through the heart of the traditional territory of the Cheyenne, Arapaho, and Lakota. It was the shortest and easiest route from Fort Laramie and the Oregon Trail to the Montana gold fields. From 1864 to 1866, the trail was traversed by about 3,500 miners, emigrant settlers and others, who competed with the Indians for the diminishing resources near the trail.The United States named the war after Red Cloud, a prominent Oglala Lakota chief allied with the Cheyenne and Arapaho. The United States army had built forts in response to attacks on civilian travelers, using a treaty right to "establish roads, military and other post". All three forts were located in 1851 Crow Indian territory and accepted by these Indians. The Crow believed they guarded their interests best by cooperating with the US army.Red Cloud's War consisted mostly of constant small-scale Indian raids and attacks on the soldiers and civilians at the three forts in the Powder River country, wearing down those garrisons. The largest action of the war, the Fetterman Fight (with 81 men killed on the U.S. side), was the worst military defeat suffered by the U.S. on the Great Plains until the Battle of the Little Bighorn in the Crow Indian reservation ten years later. " ... the most dramatic battles between the army and the Dakota [in the 1860s and 1870s] were on lands those Indians had taken from other tribes since 1851."With peace achieved under the Treaty of Fort Laramie in 1868, the Lakota and their allies were victorious. They gained legal control of the western Powder River country, took down the forts and permanently closed the Bozeman trail. The Crow lost their hunting grounds in the Powder River region to their enemies. With the treaty, "... the [United States] government had in effect betrayed the Crows, who had willingly helped the army to hold the posts for two years". The victory of the Lakota and their allies, however, only endured for eight years until the Great Sioux War of 1876, when the US started to take some of their territories again, including the sacred Black Hills.
| 3
|
[
"Red Cloud's War",
"located in the administrative territorial entity",
"Wyoming"
] |
Red Cloud's War (also referred to as the Bozeman War or the Powder River War) was an armed conflict between an alliance of the Lakota, Northern Cheyenne, and Northern Arapaho peoples against the United States and the Crow Nation that took place in the Wyoming and Montana territories from 1866 to 1868. The war was fought over control of the western Powder River Country in present north-central Wyoming.
In 1863, European Americans had blazed the Bozeman Trail through the heart of the traditional territory of the Cheyenne, Arapaho, and Lakota. It was the shortest and easiest route from Fort Laramie and the Oregon Trail to the Montana gold fields. From 1864 to 1866, the trail was traversed by about 3,500 miners, emigrant settlers and others, who competed with the Indians for the diminishing resources near the trail.The United States named the war after Red Cloud, a prominent Oglala Lakota chief allied with the Cheyenne and Arapaho. The United States army had built forts in response to attacks on civilian travelers, using a treaty right to "establish roads, military and other post". All three forts were located in 1851 Crow Indian territory and accepted by these Indians. The Crow believed they guarded their interests best by cooperating with the US army.Red Cloud's War consisted mostly of constant small-scale Indian raids and attacks on the soldiers and civilians at the three forts in the Powder River country, wearing down those garrisons. The largest action of the war, the Fetterman Fight (with 81 men killed on the U.S. side), was the worst military defeat suffered by the U.S. on the Great Plains until the Battle of the Little Bighorn in the Crow Indian reservation ten years later. " ... the most dramatic battles between the army and the Dakota [in the 1860s and 1870s] were on lands those Indians had taken from other tribes since 1851."With peace achieved under the Treaty of Fort Laramie in 1868, the Lakota and their allies were victorious. They gained legal control of the western Powder River country, took down the forts and permanently closed the Bozeman trail. The Crow lost their hunting grounds in the Powder River region to their enemies. With the treaty, "... the [United States] government had in effect betrayed the Crows, who had willingly helped the army to hold the posts for two years". The victory of the Lakota and their allies, however, only endured for eight years until the Great Sioux War of 1876, when the US started to take some of their territories again, including the sacred Black Hills.
| 4
|
[
"Red Cloud's War",
"participant",
"Crazy Horse"
] |
Colonel Carrington said he ordered Fetterman not to cross Lodge Trail Ridge, where relief from the fort would be difficult, and that he told Grummond to remind Fetterman of his order. Upon leaving the fort, Fetterman, instead of marching down the wood road to the relief of the wood train, turned north and crossed the Sullivant Hills toward Lodge Trail Ridge. Within a few minutes of their departure, a Lakota decoy party including Oglala warrior Crazy Horse appeared on Lodge Trail Ridge. Fetterman took the bait; several of the warriors stood on their ponies and insultingly waggled their bare buttocks at the troopers. Fetterman and his company were joined by Grummond at the crossing of the creek; they deployed in skirmish line and marched over the Ridge in pursuit. They raced into the Peno Valley, where an estimated 1,000-3,000 Indians were concealed. They had fought the soldiers there on December 6.The ambush was not observed from the fort, but around noon, men at the fort heard gunfire, beginning with a few shots followed immediately by sustained firing. When the Oglala and Cheyenne sprang their trap, the soldiers had no escape; none survived. Evidence indicated the cavalry probably had charged the Indians; the bodies of the cavalry's most advanced group were found nearly a mile down the ridge beyond the infantry.
Reports from the burial party sent to collect the remains said the soldiers had died in three groups. The most advanced, and probably most effective, were the two civilians, armed with 16-shot Henry repeating rifles, and a small number of cavalrymen who had dismounted and taken cover in the rocks. Up the slope behind them were the bodies of most of the retreating cavalrymen, armed with new 7-shot Spencer carbines, but encumbered by their horses and lacking cover. Further up the slope were Fetterman, Brown, and the infantrymen. They had nearly obsolete Civil War muzzle-loading muskets; the Indians were armed with equally obsolete weaponry. These foot soldiers fought from cover for a short while, until their ammunition ran out and they were overrun.Carrington heard the gunfire and immediately sent out a 40-man support force on foot under Captain Tenedor Ten Eyck. Shortly after, the 30 remaining cavalrymen of Company C were sent dismounted to reinforce Ten Eyck, followed by two wagons, the first loaded with hastily loaded ammunition and escorted by another 40 men. Carrington called for an immediate muster of troops to defend the post. Including the wood train detail, the detachments had left only 119 troops remaining inside the fort.
Ten Eyck took a roundabout route and reached the ridgetop just as the firing ceased about 12:45 p.m. He sent back a message reporting that he could not see Fetterman's force, but the valley was filled with groups of Indians taunting him to come down. Ten Eyck suffered severe criticism for not marching straight to battle, though doing so would have resulted only in the destruction of his force, too. Ten Eyck reached and recovered the bodies of Fetterman's men. Because of continuing Indian threat, they could not recover those of the cavalry for two days.By that time, Fetterman and his entire 81-man detachment were dead. Carrington's official report said that Fetterman and Brown shot each other to avoid capture. Army autopsies recorded Fetterman's death wound as a knife slash. It remains a subject of debate. The warriors mutilated most of the bodies of the soldiers. Most of the dead soldiers were scalped, beheaded, dismembered, disemboweled, and often castrated, facts widely publicized by the newspapers. The only body left untouched was that of a young teenage bugler, Adolph Metzler. He was believed to have fought several Indians with just his bugle as a bludgeon. Aside from his fatal head and chest injuries, his body was left untouched and covered with a buffalo robe by the Indians. The reason for this remains unknown.
| 5
|
[
"Red Cloud's War",
"participant",
"Lakota people"
] |
The Powder River country encompasses the numerous rivers (the Bighorn, Rosebud, Tongue and Powder) that flow northeastward from the Bighorn Mountains to the Yellowstone. The Cheyenne had been the first tribe in this area, followed by bands of Lakota. As more of the northern plains became occupied by white settlement, this region became the last unspoiled hunting ground of the Northern Cheyenne and Arapaho and several of the seven bands of the Lakota.The treaty breaking annexation of the Crow's Powder River area in the 1850s by the Lakotas was the basis for Red Cloud's War against the United States on exactly the same soil a decade later. The United States vs. the Lakota was a conflict between "... two expanding empires, with the most dramatic battles occurring on lands only recently taken by the Sioux from other tribes".In 1865, Maj. Gen. Grenville M. Dodge ordered the Powder River Expedition against the Lakota, Cheyenne and Arapaho. Three columns of soldiers numbering 2,675 men, commanded by Patrick E. Connor, moved into the Powder River country. The expedition failed to defeat the Indians in any decisive battles, although it destroyed an Arapaho village at the Battle of the Tongue River. The expedition was a failure in most respects as Lakota Indian resistance to white emigrants traveling the Bozeman Trail became more determined than ever.After the Powder River Expedition, the U.S. attempted to negotiate safe passage for settlers through Indian territory. In autumn 1865, it negotiated several treaties with Lakota, Cheyenne, and Arapaho leaders. The treaties provided monetary compensation to the Indians in exchange for their agreement to withdraw from the overland routes, established and to be established, in the Powder River country. However, the signatories to these treaties were "Laramie loafers"—Indians who lived near Fort Laramie and lived off handouts. For a treaty to be effective, the Indians who had fought Connor, especially Red Cloud, had to be engaged. No white man could be found to undertake a dangerous mission to find Red Cloud and bring him to Fort Laramie for negotiations, so several of the "loafers" took the task. On March 12, 1866, Red Cloud and his Oglala rode into Fort Laramie. Red Cloud committed to remain peacefully at the Fort until such time as the U.S.'s chief negotiator, E. B. Taylor, arrived with presents for the assembled Indians.Crows such as Wolf Bow tried to push the whites to take action against the Indian intruders: "Put the Sioux Indians in their own country, and keep them from troubling us. Don't stop fighting them". When possible, the Crow warned the troops of imminent attacks from hostile Indians and they joined soldiers in fending off attempts to capture horses. The strikes and attacks on the soldiers by the Lakota "... appeared to be a great Sioux war to protect their land. And it was - but the Sioux had only recently conquered this land from other tribes and now defending the territory both from other tribes and from the advance of white settlers".
| 7
|
[
"Red Cloud's War",
"location",
"Powder River Country"
] |
The Powder River country encompasses the numerous rivers (the Bighorn, Rosebud, Tongue and Powder) that flow northeastward from the Bighorn Mountains to the Yellowstone. The Cheyenne had been the first tribe in this area, followed by bands of Lakota. As more of the northern plains became occupied by white settlement, this region became the last unspoiled hunting ground of the Northern Cheyenne and Arapaho and several of the seven bands of the Lakota.The treaty breaking annexation of the Crow's Powder River area in the 1850s by the Lakotas was the basis for Red Cloud's War against the United States on exactly the same soil a decade later. The United States vs. the Lakota was a conflict between "... two expanding empires, with the most dramatic battles occurring on lands only recently taken by the Sioux from other tribes".In 1865, Maj. Gen. Grenville M. Dodge ordered the Powder River Expedition against the Lakota, Cheyenne and Arapaho. Three columns of soldiers numbering 2,675 men, commanded by Patrick E. Connor, moved into the Powder River country. The expedition failed to defeat the Indians in any decisive battles, although it destroyed an Arapaho village at the Battle of the Tongue River. The expedition was a failure in most respects as Lakota Indian resistance to white emigrants traveling the Bozeman Trail became more determined than ever.After the Powder River Expedition, the U.S. attempted to negotiate safe passage for settlers through Indian territory. In autumn 1865, it negotiated several treaties with Lakota, Cheyenne, and Arapaho leaders. The treaties provided monetary compensation to the Indians in exchange for their agreement to withdraw from the overland routes, established and to be established, in the Powder River country. However, the signatories to these treaties were "Laramie loafers"—Indians who lived near Fort Laramie and lived off handouts. For a treaty to be effective, the Indians who had fought Connor, especially Red Cloud, had to be engaged. No white man could be found to undertake a dangerous mission to find Red Cloud and bring him to Fort Laramie for negotiations, so several of the "loafers" took the task. On March 12, 1866, Red Cloud and his Oglala rode into Fort Laramie. Red Cloud committed to remain peacefully at the Fort until such time as the U.S.'s chief negotiator, E. B. Taylor, arrived with presents for the assembled Indians.Crows such as Wolf Bow tried to push the whites to take action against the Indian intruders: "Put the Sioux Indians in their own country, and keep them from troubling us. Don't stop fighting them". When possible, the Crow warned the troops of imminent attacks from hostile Indians and they joined soldiers in fending off attempts to capture horses. The strikes and attacks on the soldiers by the Lakota "... appeared to be a great Sioux war to protect their land. And it was - but the Sioux had only recently conquered this land from other tribes and now defending the territory both from other tribes and from the advance of white settlers".
| 10
|
[
"Red Cloud's War",
"location",
"Bozeman Trail"
] |
War
Carrington and his caravan reached Fort Reno on June 28, and left two companies (about 100 men) there to relieve the two companies of the 5th U.S. Volunteers (nicknamed the "Galvanized Yankees"), who had garrisoned the fort over the winter. Proceeding north, on July 14, Carrington founded Fort Phil Kearny on Piney Creek, near present-day Buffalo, Wyoming.
From there two companies of the 18th advanced 91 miles to the northwest, where on August 13, they established a third post, Fort C. F. Smith on the Bighorn River. Given the typically early and severe winters of the high plains, the middle of August was very late in the year to begin constructing forts, but Carrington's march had been slowed by having to transport a large mechanical "grass-cutting machine." With replacements and reinforcements, Carrington's total force did not much exceed 700, of whom 400 were located at Fort Kearny.
Carrington was an engineer and political appointee, inexperienced in combat. He spent manpower resources building superior fortifications. Arriving in the region in mid-July, he tried to prepare for winter. Given the severity of the Wyoming winters, this was reasonable, but many of his junior officers, anxious for battle, were infuriated. Most were Civil War veterans, but they were unfamiliar with Indian fighting and believed the warriors could be easily defeated.On July 16, a group of Cheyenne, including Dull Knife and Two Moons, visited Carrington at Fort Reno and proclaimed their desire for peace. They said that Red Cloud was nearby with 500 warriors. Two white civilians were killed that day, and the Lakota campaign against the forts along the Trail began the next day. Red Cloud's warriors infiltrated the picket lines near the fort and stampeded 175 horses and mules. About 200 soldiers pursued the Indians in a running 15 mile fight, attempting unsuccessfully to recover the animals and suffering two men killed and three wounded. Returning to the fort, they found the bodies of six civilian traders killed by the Indians.On July 20, Red Cloud's warriors attacked a wagon train of 37 soldiers and civilians, killing two, at Crazy Woman Fork of the Powder River. After they attacked other civilian wagon trains, nearly all civilian traffic on the Bozeman Trail ceased. Carrington could only be re-supplied with food and ammunition by heavily guarded wagon trains. In the weeks and months that followed, the Indians repeatedly attacked the wagon trains that sallied out of Fort Kearny to cut construction timber in a forest six miles away. For defense, the wood trains were large, consisting of two parallel lines of 24 to 40 wagons guarded by mounted soldiers on either flank. In the event of an attack, the wagons were quickly drawn into an corral for defense. Fifteen Indian attacks near Fort Kearny between July 16 and September 27 resulted in the deaths of 6 soldiers and 28 civilians and the loss of several hundred horses, mules, and cattle. Carrington's hay-cutting machine was also destroyed.
| 13
|
[
"Red Cloud's War",
"participant",
"Arapaho people"
] |
The Powder River country encompasses the numerous rivers (the Bighorn, Rosebud, Tongue and Powder) that flow northeastward from the Bighorn Mountains to the Yellowstone. The Cheyenne had been the first tribe in this area, followed by bands of Lakota. As more of the northern plains became occupied by white settlement, this region became the last unspoiled hunting ground of the Northern Cheyenne and Arapaho and several of the seven bands of the Lakota.The treaty breaking annexation of the Crow's Powder River area in the 1850s by the Lakotas was the basis for Red Cloud's War against the United States on exactly the same soil a decade later. The United States vs. the Lakota was a conflict between "... two expanding empires, with the most dramatic battles occurring on lands only recently taken by the Sioux from other tribes".In 1865, Maj. Gen. Grenville M. Dodge ordered the Powder River Expedition against the Lakota, Cheyenne and Arapaho. Three columns of soldiers numbering 2,675 men, commanded by Patrick E. Connor, moved into the Powder River country. The expedition failed to defeat the Indians in any decisive battles, although it destroyed an Arapaho village at the Battle of the Tongue River. The expedition was a failure in most respects as Lakota Indian resistance to white emigrants traveling the Bozeman Trail became more determined than ever.After the Powder River Expedition, the U.S. attempted to negotiate safe passage for settlers through Indian territory. In autumn 1865, it negotiated several treaties with Lakota, Cheyenne, and Arapaho leaders. The treaties provided monetary compensation to the Indians in exchange for their agreement to withdraw from the overland routes, established and to be established, in the Powder River country. However, the signatories to these treaties were "Laramie loafers"—Indians who lived near Fort Laramie and lived off handouts. For a treaty to be effective, the Indians who had fought Connor, especially Red Cloud, had to be engaged. No white man could be found to undertake a dangerous mission to find Red Cloud and bring him to Fort Laramie for negotiations, so several of the "loafers" took the task. On March 12, 1866, Red Cloud and his Oglala rode into Fort Laramie. Red Cloud committed to remain peacefully at the Fort until such time as the U.S.'s chief negotiator, E. B. Taylor, arrived with presents for the assembled Indians.Crows such as Wolf Bow tried to push the whites to take action against the Indian intruders: "Put the Sioux Indians in their own country, and keep them from troubling us. Don't stop fighting them". When possible, the Crow warned the troops of imminent attacks from hostile Indians and they joined soldiers in fending off attempts to capture horses. The strikes and attacks on the soldiers by the Lakota "... appeared to be a great Sioux war to protect their land. And it was - but the Sioux had only recently conquered this land from other tribes and now defending the territory both from other tribes and from the advance of white settlers".
| 16
|
[
"Lake Hotel",
"architectural style",
"Colonial architecture"
] |
The Lake Hotel, also known as Lake Yellowstone Hotel is one of a series of hotels built to accommodate visitors to Yellowstone National Park in the late 19th and early 20th century. Built in 1891, it is the oldest operating hotel in the park. It was re-designed and substantially expanded by Robert Reamer, architect of the Old Faithful Inn in 1903. In contrast to the Old Faithful Inn and many other western park facilities, the Lake Hotel is a relatively plain clapboarded Colonial Revival structure with three large Ionic porticoes facing Yellowstone Lake. It was designated a National Historic Landmark in 2015.
The original 1891 hotel was a large three-story structure with projecting bays at each end. Its construction was supervised by R.R. Cummins for the Northern Pacific Railway, which was building two other, similar hotels in the park. Reamer's 1903 remodeling changed these projections to the present Ionic porticoes. An eastward extension was added at this time, with a third matching portico. In 1922-23 a further extension to the east was undertaken, this with a flat roof. In 1928 a two-story west wing was added, expanding the dining room and adding a solarium to the front. The entire hotel was extensively renovated from 1984 to 1990.The Lake Hotel is adjoined by the Lake Fish Hatchery Historic District and the Grand Loop Road Historic District.
The west wing of the Lake Hotel was renovated in the winter and spring of 2012, including the formal dining room and beautiful sun room/lounge. The remaining rooms in the east end of the hotel will be renovated during the fall and winter of 2013-2014.
Lake Yellowstone Hotel & Cabins is a member of Historic Hotels of America, the official program of the National Trust for Historic Preservation.
| 4
|
[
"Lake Hotel",
"heritage designation",
"National Historic Landmark"
] |
The Lake Hotel, also known as Lake Yellowstone Hotel is one of a series of hotels built to accommodate visitors to Yellowstone National Park in the late 19th and early 20th century. Built in 1891, it is the oldest operating hotel in the park. It was re-designed and substantially expanded by Robert Reamer, architect of the Old Faithful Inn in 1903. In contrast to the Old Faithful Inn and many other western park facilities, the Lake Hotel is a relatively plain clapboarded Colonial Revival structure with three large Ionic porticoes facing Yellowstone Lake. It was designated a National Historic Landmark in 2015.
The original 1891 hotel was a large three-story structure with projecting bays at each end. Its construction was supervised by R.R. Cummins for the Northern Pacific Railway, which was building two other, similar hotels in the park. Reamer's 1903 remodeling changed these projections to the present Ionic porticoes. An eastward extension was added at this time, with a third matching portico. In 1922-23 a further extension to the east was undertaken, this with a flat roof. In 1928 a two-story west wing was added, expanding the dining room and adding a solarium to the front. The entire hotel was extensively renovated from 1984 to 1990.The Lake Hotel is adjoined by the Lake Fish Hatchery Historic District and the Grand Loop Road Historic District.
The west wing of the Lake Hotel was renovated in the winter and spring of 2012, including the formal dining room and beautiful sun room/lounge. The remaining rooms in the east end of the hotel will be renovated during the fall and winter of 2013-2014.
Lake Yellowstone Hotel & Cabins is a member of Historic Hotels of America, the official program of the National Trust for Historic Preservation.
| 7
|
[
"Big Cub Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Big Cub Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Big Cub is part of the Lion's Group of geysers, a cluster of geysers that all share an underground connection. The other geysers in this group are Lion Geyser, Lioness Geyser, and Little Cub Geyser.== References ==
| 1
|
[
"Big Cub Geyser",
"located in the administrative territorial entity",
"Wyoming"
] |
== References ==
| 2
|
[
"Big Cub Geyser",
"instance of",
"geyser"
] |
Big Cub Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Big Cub is part of the Lion's Group of geysers, a cluster of geysers that all share an underground connection. The other geysers in this group are Lion Geyser, Lioness Geyser, and Little Cub Geyser.== References ==
| 3
|
[
"Clepsydra Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Clepsydra Geyser is a geyser in the Lower Geyser Basin of Yellowstone National Park in the United States.
Clepsydra plays nearly continuously to heights of 45 feet (14 m). It was named by T. B. Comstock during the 1878 Captain Jones expedition, with its nomenclature derived from the Greek word for water clock. Prior to the 1959 Hebgen Lake earthquake, it erupted regularly every three minutes.== References ==
| 1
|
[
"Roosevelt Arch",
"significant event",
"foundation stone laying ceremony"
] |
The Roosevelt Arch is a rusticated triumphal arch at the north entrance to Yellowstone National Park in Gardiner, Montana, United States. Constructed under the supervision of the US Army at Fort Yellowstone, its cornerstone was laid down by President Theodore Roosevelt in 1903. The top of the arch is inscribed with a quote from the Organic Act of 1872, the legislation which created Yellowstone, which reads: "For the Benefit and Enjoyment of the People".
The idea of the arch is attributed to Hiram Martin Chittenden, who felt that the area surrounding Gardiner was not sufficiently impressive and required an emphatic statement of arrival at the famous park. Before 1903, trains brought visitors to Cinnabar, Montana, which was a few miles northwest of Gardiner, Montana, where people would transfer onto horse-drawn coaches to enter the park. In 1903, the railway finally came to Gardiner. With the development of the Gardiner train station, the arch was proposed as part of the station ensemble.
| 0
|
[
"Grotto Geyser",
"country",
"United States of America"
] |
Grotto Geyser is a fountain-type geyser located in the Upper Geyser Basin in Yellowstone National Park in the United States. Grotto Geyser is the namesake for the group of geysers that includes Grotto Fountain Geyser, South Grotto Fountain Geyser, Indicator Spring, Spa Geyser, Startling Geyser, and Rocket Geyser.History
On September 18, 1870 members of the Washburn-Langford-Doane Expedition entered the Upper Geyser Basin where in a day and a half of exploration, they named seven geysers of which Grotto was one. Nathaniel P. Langford described the Grotto in his 1871 Scribner's account:
| 0
|
[
"Grotto Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Grotto Geyser is a fountain-type geyser located in the Upper Geyser Basin in Yellowstone National Park in the United States. Grotto Geyser is the namesake for the group of geysers that includes Grotto Fountain Geyser, South Grotto Fountain Geyser, Indicator Spring, Spa Geyser, Startling Geyser, and Rocket Geyser.History
On September 18, 1870 members of the Washburn-Langford-Doane Expedition entered the Upper Geyser Basin where in a day and a half of exploration, they named seven geysers of which Grotto was one. Nathaniel P. Langford described the Grotto in his 1871 Scribner's account:
| 1
|
[
"Grotto Geyser",
"located in the administrative territorial entity",
"Wyoming"
] |
History
On September 18, 1870 members of the Washburn-Langford-Doane Expedition entered the Upper Geyser Basin where in a day and a half of exploration, they named seven geysers of which Grotto was one. Nathaniel P. Langford described the Grotto in his 1871 Scribner's account:
| 2
|
[
"Solitary Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Solitary Geyser is a fountain-type geyser in Yellowstone National Park, located above the Upper Geyser Basin. Eruptions last about a minute and are four to eight minutes apart; most eruptions are less than six feet (1.8 m) in height. It is very distinctive with clear blue water underneath and a base that is tinted orange. Solitary Geyser is accessible via the Observation Point loop trail behind Old Faithful.
Originally this geyser was a hot spring known as Solitary Spring, which did not erupt. When water was diverted to a swimming pool, the water level was lowered sufficiently to cause eruptions. Since then the diversion of water has been stopped and the water has returned to its previous level, but eruptions continue.
| 1
|
[
"Spasmodic Geyser",
"instance of",
"geyser"
] |
Spasmodic Geyser is a geyser located in the Upper Geyser Basin in Yellowstone National Park in the United States.
Spasmodic Geyser's eruptions from the two craters can be up to 15 feet (4.6 m) high. Water can also erupt from a few inches to ten feet high from the approximately 20 vents. The intervals between eruptions are irregular, but most are in the 1-3 hour range. Spasmodic Geyser was named by A.C. Peale, from the 1878 Hayden survey team, for its erratic eruptions. Its temperature is about 92 °C (198 °F). Spasmodic Geyser is also connected to the nearby Penta Geyser, which is smaller. While Penta Geyser is erupting, there is no activity from Spasmodic Geyser. Activity from Spasmodic Geyser usually precede eruptions from Sawmill Geyser and Penta Geyser.
| 3
|
[
"Giantess Geyser",
"instance of",
"geyser"
] |
Giantess Geyser is a fountain-type geyser in the Upper Geyser Basin of Yellowstone National Park. It is known for its violent and infrequent eruptions of multiple water bursts that reach from 100 to 200 feet (30 to 61 m). Eruptions generally occur 2 to 6 times a year. The surrounding area may shake from underground steam explosions just before the initial water and/or steam eruptions. Eruptions may occur twice hourly, experience a tremendous steam phase, and continue activity for 4 to 48 hours. The Geyser last erupted on August 26, 2020 after a six year, 210 day hiatus. A follow up eruption occurred 15 days later on 10 September 2020. Another eruption occurred on 11 August 2021
| 3
|
[
"Bijou Geyser",
"instance of",
"geyser"
] |
Bijou Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
| 2
|
[
"Bijou Geyser",
"located in the administrative territorial entity",
"Teton County"
] |
Eruptions
Bijou erupts nearly continuously reaching a height of 15 feet (4.6 m). At times, the water fountain turns to a steam phase when Bijou emits a column of steam.
| 3
|
[
"Fountain Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Fountain Geyser is a geyser in the Lower Geyser Basin of Yellowstone National Park in the United States.
Fountain is the dominant member of a group of geysers at the Fountain Paint Pots thermal area. Morning Geyser, which erupts from a vent close to Fountain's, is larger, but is inactive during most years. Fountain, by contrast, is usually active. It is a fountain-type geyser that erupts jets ranging in height up to 80 feet (24 m) or more, with most eruptions containing at least a few bursts that reach 40 to 50 feet. Intervals (= eruption start to eruption start) vary from year to year but are commonly about 4.5 to 6 hours, with occasional longer intervals of 11 to 12 hours. Durations of eruptions are typically about 30 minutes. Occasionally, Fountain departs from its usual behavior and enters so-called "wild-phase" eruption, during which the height is much reduced but the duration can be as long as two weeks.
Fountain is not to be confused with similarly named, and nearby (and larger), Great Fountain Geyser, another of the major features of Lower Geyser Basin, adjacent to the Firehole Lake road.
| 1
|
[
"Daisy Geyser",
"country",
"United States of America"
] |
Daisy Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Daisy Geyser is part of the Daisy Group. It was named prior to 1890 by the Hague Party. It erupts every 110 to 240 minutes for a period of 3 to 5 minutes and is one of the most predictable geysers in the park. Its fountain erupts at an angle to the ground and reaches a height of 75 feet (23 m). The interval between eruptions can be temporarily altered by an eruption of nearby Splendid Geyser. To a smaller degree, Brilliant Pool and Comet Geyser are influenced by Splendid and Daisy.Daisy Geyser was one of the Yellowstone geysers that had its eruption interval disrupted by the 2002 Denali earthquake, in Alaska. Immediately after the quake, the interval rapidly decreased but returned to previous intervals over the course of a few weeks.
| 0
|
[
"Daisy Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Daisy Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Daisy Geyser is part of the Daisy Group. It was named prior to 1890 by the Hague Party. It erupts every 110 to 240 minutes for a period of 3 to 5 minutes and is one of the most predictable geysers in the park. Its fountain erupts at an angle to the ground and reaches a height of 75 feet (23 m). The interval between eruptions can be temporarily altered by an eruption of nearby Splendid Geyser. To a smaller degree, Brilliant Pool and Comet Geyser are influenced by Splendid and Daisy.Daisy Geyser was one of the Yellowstone geysers that had its eruption interval disrupted by the 2002 Denali earthquake, in Alaska. Immediately after the quake, the interval rapidly decreased but returned to previous intervals over the course of a few weeks.
| 1
|
[
"Daisy Geyser",
"instance of",
"geyser"
] |
Daisy Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Daisy Geyser is part of the Daisy Group. It was named prior to 1890 by the Hague Party. It erupts every 110 to 240 minutes for a period of 3 to 5 minutes and is one of the most predictable geysers in the park. Its fountain erupts at an angle to the ground and reaches a height of 75 feet (23 m). The interval between eruptions can be temporarily altered by an eruption of nearby Splendid Geyser. To a smaller degree, Brilliant Pool and Comet Geyser are influenced by Splendid and Daisy.Daisy Geyser was one of the Yellowstone geysers that had its eruption interval disrupted by the 2002 Denali earthquake, in Alaska. Immediately after the quake, the interval rapidly decreased but returned to previous intervals over the course of a few weeks.
| 3
|
[
"Anemone Geyser",
"country",
"United States of America"
] |
Anemone Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States. Anemone is actually two closely related geysers. The larger of the two is known as Big or North Anemone while the smaller is known as Little or South Anemone. The two geysers were named after the anemone flower by the Hague Party in 1904. Both vents have a pale yellow color and shape similar to the flower.
| 0
|
[
"Anemone Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Anemone Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States. Anemone is actually two closely related geysers. The larger of the two is known as Big or North Anemone while the smaller is known as Little or South Anemone. The two geysers were named after the anemone flower by the Hague Party in 1904. Both vents have a pale yellow color and shape similar to the flower.
| 1
|
[
"Jet Geyser",
"instance of",
"geyser"
] |
Jet Geyser is a geyser in the Lower Geyser Basin of Yellowstone National Park in the United States. Jet Geyser is in the Fountain Group that includes Fountain Geyser, Morning Geyser, Red Spouter and Silex Spring.Jet Geyser is a very accessible and intimate geyser, being close to a park road and alongside a boardwalk.
Jet usually erupts in long-duration series. During series, eruptions are relatively frequent and less than one minute in duration. Jet Geyser's behavior is influenced by nearby (and much bigger) Fountain Geyser. Jet eruptions usually occur every 7 to 30 minutes, with the frequency increasing as a Fountain Geyser eruption nears. Jet erupts every 1 to 4 minutes during most Fountain Geyser eruptions. After Fountain has quit, Jet usually quits. Approximately mid-way through a Fountain Geyser interval, Jet often starts a new eruption series.
Jet is a cone-type geyser with at least five vents that erupt in different directions (vertical, angled, and subhorizontal). The vents produce varying quantities of water and steam for about 0.25 to 1 minute. The central vent will usually erupt to about 20 feet (6.1 m).
| 2
|
[
"Excelsior Geyser",
"instance of",
"geyser"
] |
Excelsior Geyser Crater, formerly known as Excelsior Geyser, is a dormant fountain-type geyser in the Midway Geyser Basin of Yellowstone National Park in the United States. Excelsior was named by the Hayden Geological Survey of 1871.Description
The Excelsior Geyser pool discharges 4,000 to 4,500 gallons (15,100–17,000 L) of 199 °F (93 °C) water per minute directly into the Firehole River. In the late 19th century (and possibly 1901), it was an active geyser that erupted frequently. Most eruptions were about 100 feet high, although some exceeded 300 feet (91 m) in both height and width. It is believed that the powerful eruptions damaged its internal plumbing system, and it now boils as a productive hot spring most of the time.
| 2
|
[
"Comet Geyser",
"country",
"United States of America"
] |
Comet Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Comet Geyser is part of the Daisy Group which includes Daisy Geyser, Splendid Geyser and Brilliant Pool. As opposed to the other features in this group, Comet erupts almost continuously. Every few minutes it surges to a height of 6 feet (1.8 m). This constant eruption has led to it having the biggest sinter cone of any of the geysers in this group.Comet might be interconnected with Daisy and Splendid Geysers, albeit to a lesser degree than Brilliant Pool. After an eruption of Splendid and sometimes after Daisy, the action of Comet slows but quickly returns to its normal level.Comet Geyser was named by the Hague Party in 1904.
| 0
|
[
"Comet Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Comet Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Comet Geyser is part of the Daisy Group which includes Daisy Geyser, Splendid Geyser and Brilliant Pool. As opposed to the other features in this group, Comet erupts almost continuously. Every few minutes it surges to a height of 6 feet (1.8 m). This constant eruption has led to it having the biggest sinter cone of any of the geysers in this group.Comet might be interconnected with Daisy and Splendid Geysers, albeit to a lesser degree than Brilliant Pool. After an eruption of Splendid and sometimes after Daisy, the action of Comet slows but quickly returns to its normal level.Comet Geyser was named by the Hague Party in 1904.
| 1
|
[
"Comet Geyser",
"instance of",
"geyser"
] |
Comet Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Comet Geyser is part of the Daisy Group which includes Daisy Geyser, Splendid Geyser and Brilliant Pool. As opposed to the other features in this group, Comet erupts almost continuously. Every few minutes it surges to a height of 6 feet (1.8 m). This constant eruption has led to it having the biggest sinter cone of any of the geysers in this group.Comet might be interconnected with Daisy and Splendid Geysers, albeit to a lesser degree than Brilliant Pool. After an eruption of Splendid and sometimes after Daisy, the action of Comet slows but quickly returns to its normal level.Comet Geyser was named by the Hague Party in 1904.
| 3
|
[
"Economic Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Economic Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Economic Geyser is a small, usually inactive geyser located between the Giant Geyser group and the Grand Geyser group. Economic Geyser was once a popular, frequently-erupting geyser until it became essentially dormant in the 1920s.Economic Geyser is believed to be named for its behavior during its active days. It is reported that most of the water ejected drained back into the vent after the eruption, thus making the geyser appear to conserve its water. It was most likely named by Frank Jay Haynes, the park photographer from 1883-1916.The temperature of the water in geyser pools and other geothermal features can be judged by the color of the bacteria living in the water. Changes in the size and color of bacteria mats at Economic Geyser imply that the geyser is heating up. Photographs of the geyser vent taken in the 1990s show a quiet pool very dark with algae. Photographs of the vent taken in 2006 show a pool of clear water with traces of the bacterial colors associated with higher temperatures.
| 1
|
[
"A-0 Geyser",
"located in protected area",
"Yellowstone National Park"
] |
A-0 Geyser is a geyser in the Lower Geyser Basin of Yellowstone National Park in the United States.
A-0 Geyser is part of the White Creek Group which includes Spindle Geyser and Botryoidal Spring. It can be identified by its shallow, round basin with a round vent in the middle found 100 feet (30 m) southeast of the Surprise Pool parking area.
It erupts for a duration of about 30 to 40 seconds with intervals of 20 to 26 minutes between eruptions. The fountain reaches a height of 5 to 10 feet (1.5 to 3.0 m).The name A-0 is an unofficial name based on the proximity of this geyser to the dormant A-1 and A-2 geysers.The RCN location of this geyser has been unintentionally switched with Dilemma Geyser, elsewhere in the Lower Geyser Basin.
| 1
|
[
"Craig Pass",
"located in protected area",
"Yellowstone National Park"
] |
Craig Pass (el.8,262 feet (2,518 m)), is a mountain pass located on the Continental Divide in Yellowstone National Park in Wyoming. The Grand Loop Road crosses the pass approximately 8 miles (13 km) east of Old Faithful Geyser.
The pass was named by Hiram Chittenden for Ida M. Craig (Wilcox), the daughter of a close friend, General James Craig. Ida Craig was purportedly the first tourist to cross the pass after it was completed in September, 1891. Roads are usually open throughout the year, but they may be closed for a short time during winter when the weather is bad.
The small Isa Lake is located just west of the pass on the Grand Loop Road and is noted for striding the Continental Divide and draining into two different watersheds—the Atlantic via the Missouri River and the Pacific via the Snake River.
| 1
|
[
"Craig Pass",
"located in the administrative territorial entity",
"Wyoming"
] |
Craig Pass (el.8,262 feet (2,518 m)), is a mountain pass located on the Continental Divide in Yellowstone National Park in Wyoming. The Grand Loop Road crosses the pass approximately 8 miles (13 km) east of Old Faithful Geyser.
The pass was named by Hiram Chittenden for Ida M. Craig (Wilcox), the daughter of a close friend, General James Craig. Ida Craig was purportedly the first tourist to cross the pass after it was completed in September, 1891. Roads are usually open throughout the year, but they may be closed for a short time during winter when the weather is bad.
The small Isa Lake is located just west of the pass on the Grand Loop Road and is noted for striding the Continental Divide and draining into two different watersheds—the Atlantic via the Missouri River and the Pacific via the Snake River.
| 2
|
[
"Craig Pass",
"instance of",
"mountain pass"
] |
Craig Pass (el.8,262 feet (2,518 m)), is a mountain pass located on the Continental Divide in Yellowstone National Park in Wyoming. The Grand Loop Road crosses the pass approximately 8 miles (13 km) east of Old Faithful Geyser.
The pass was named by Hiram Chittenden for Ida M. Craig (Wilcox), the daughter of a close friend, General James Craig. Ida Craig was purportedly the first tourist to cross the pass after it was completed in September, 1891. Roads are usually open throughout the year, but they may be closed for a short time during winter when the weather is bad.
The small Isa Lake is located just west of the pass on the Grand Loop Road and is noted for striding the Continental Divide and draining into two different watersheds—the Atlantic via the Missouri River and the Pacific via the Snake River.
| 5
|
[
"Sylvan Pass (Wyoming)",
"located in protected area",
"Yellowstone National Park"
] |
Sylvan Pass (el. 8,524 feet (2,598 m)) is a mountain pass located in the Absaroka Range in Yellowstone National Park in Wyoming. The pass provides access to the park from the east entrance.
The pass was named after nearby Sylvan Lake (derived from medieval Latin sylvānus, from Latin Silvānus, god of the woods, from silva, forest), and was formed by frost action breaking the rocks. The park road through the pass was closed during winter but is now open to visitors throughout winter. The road is maintained to allow access via snowmobile, snow coach, and cross-country skiing. In the 2007–08 season it cost the parks service in excess of $200,000 to keep it open and avalanche control measures were put in place.
The Sylvan Pass route is the only way to enter/exit Yellowstone National Park from the East Entrance.
Sylvan Pass is the low point of the saddle between Hoyt Peak and Top Notch Peak.
The original road through the pass was designed by Captain Hiram Chittenden of the Army Corps of Engineers.
| 1
|
[
"Sylvan Pass (Wyoming)",
"located in the administrative territorial entity",
"Wyoming"
] |
Sylvan Pass (el. 8,524 feet (2,598 m)) is a mountain pass located in the Absaroka Range in Yellowstone National Park in Wyoming. The pass provides access to the park from the east entrance.
The pass was named after nearby Sylvan Lake (derived from medieval Latin sylvānus, from Latin Silvānus, god of the woods, from silva, forest), and was formed by frost action breaking the rocks. The park road through the pass was closed during winter but is now open to visitors throughout winter. The road is maintained to allow access via snowmobile, snow coach, and cross-country skiing. In the 2007–08 season it cost the parks service in excess of $200,000 to keep it open and avalanche control measures were put in place.
The Sylvan Pass route is the only way to enter/exit Yellowstone National Park from the East Entrance.
Sylvan Pass is the low point of the saddle between Hoyt Peak and Top Notch Peak.
The original road through the pass was designed by Captain Hiram Chittenden of the Army Corps of Engineers.
| 2
|
[
"Sylvan Pass (Wyoming)",
"instance of",
"mountain pass"
] |
Sylvan Pass (el. 8,524 feet (2,598 m)) is a mountain pass located in the Absaroka Range in Yellowstone National Park in Wyoming. The pass provides access to the park from the east entrance.
The pass was named after nearby Sylvan Lake (derived from medieval Latin sylvānus, from Latin Silvānus, god of the woods, from silva, forest), and was formed by frost action breaking the rocks. The park road through the pass was closed during winter but is now open to visitors throughout winter. The road is maintained to allow access via snowmobile, snow coach, and cross-country skiing. In the 2007–08 season it cost the parks service in excess of $200,000 to keep it open and avalanche control measures were put in place.
The Sylvan Pass route is the only way to enter/exit Yellowstone National Park from the East Entrance.
Sylvan Pass is the low point of the saddle between Hoyt Peak and Top Notch Peak.
The original road through the pass was designed by Captain Hiram Chittenden of the Army Corps of Engineers.
| 3
|
[
"Sylvan Pass (Wyoming)",
"mountain range",
"Absaroka Range"
] |
Sylvan Pass (el. 8,524 feet (2,598 m)) is a mountain pass located in the Absaroka Range in Yellowstone National Park in Wyoming. The pass provides access to the park from the east entrance.
The pass was named after nearby Sylvan Lake (derived from medieval Latin sylvānus, from Latin Silvānus, god of the woods, from silva, forest), and was formed by frost action breaking the rocks. The park road through the pass was closed during winter but is now open to visitors throughout winter. The road is maintained to allow access via snowmobile, snow coach, and cross-country skiing. In the 2007–08 season it cost the parks service in excess of $200,000 to keep it open and avalanche control measures were put in place.
The Sylvan Pass route is the only way to enter/exit Yellowstone National Park from the East Entrance.
Sylvan Pass is the low point of the saddle between Hoyt Peak and Top Notch Peak.
The original road through the pass was designed by Captain Hiram Chittenden of the Army Corps of Engineers.
| 4
|
[
"Old Faithful Inn",
"member of",
"Historic Hotels of America"
] |
The Old Faithful Inn is a hotel in the western United States with a view of the Old Faithful Geyser, located in Yellowstone National Park, Wyoming. The Inn has a multi-story log lobby, flanked by long frame wings containing guest rooms. In the western portion of the park, it sits at an approximate elevation of 7,350 feet (2,240 m) above sea level.
With its log and limb lobby and massive (500-short-ton or 450-metric-ton, 85-foot or 26-meter) stone fireplace, the inn is an example of the "Golden Age" of rustic resort architecture, a style which is also known as National Park Service Rustic. It is one of the few log hotels still standing in the United States, and was the first of the great park lodges of the American west.
Initial construction was carried out over the winter of 1903–1904, largely using locally obtained materials including lodgepole pine and rhyolite stone. When the Old Faithful Inn first opened in the spring of 1904, it boasted electric lights and steam heat.
The structure is the largest log hotel in the world; possibly even the largest log building in the world. In 2007 the American Institute of Architects conducted a survey to determine the 150 favorite buildings in America; the Old Faithful Inn ranked 36. The Inn, which was designated a National Historic Landmark in 1987, is itself part of the Old Faithful Historic District. Old Faithful Inn is a member of Historic Hotels of America, the official program of the National Trust for Historic Preservation.
| 3
|
[
"Old Faithful Inn",
"architect",
"Robert Reamer"
] |
Design
The inn's architect was 29-year-old Robert Reamer, an architect for the Yellowstone Park Company, which was affiliated with the Northern Pacific Railway. Reamer was hired by Harry W. Child, the president of the Yellowstone Park Company, who had met Reamer in San Diego through mutual acquaintances. Reamer designed the lobby and the initial phase of guest rooms, known as the Old House, which was built in 1903–1904, much of it in the long winter. The east wing was extended in 1913–14, and the west wing in 1927, creating a single structure almost 700 feet (210 m) long. The Old House is rotated 90 degrees with respect to Old Faithful so that a view of the geyser is framed by the entrance porch for arriving visitors. The porch roof provides a viewing platform for viewing eruptions of Old Faithful and other geysers, while the main facade faces Geyser Hill across the Firehole River, where the old Circuit Road once ran through the geyser basin.The central feature of the Old House is a tall gabled log structure housing the lobby, dominated by a deep, steeply-pitching shingled roof. The Old House uses load-bearing log lower exterior walls with a log pole interior framework supporting seven stories, six of which are the roof structure. The upper gable walls are of milled lumber framing with shingle sheathing. The front slope of the shingled roof is accented by shed and gabled dormers, some of which are purely decorative. Both interior and exterior framing is supported by twisted or curved branches, giving the entire structure a strongly rustic air. There are two levels of balconies, the lower encircling the lobby and the upper on two sides. Stairs climb from the second balcony to a platform in the framing known as the "Crow's Nest" which once was used by musicians to entertain guests, then on to the crown of the gable 92 feet (28 m) above the lobby floor. The entire structure is crowned by a roof walk that once held searchlights to illuminate Old Faithful Geyser at night. The original guest wings are 3+1⁄2 stories tall on either side of the lobby. It is anchored to the ground by a rhyolite foundation that extends to the first floor window sills.Offset to the southeast corner, the stone fireplace measures sixteen feet (5 m) square at the base. It features four main hearths, one on each face, with smaller hearths, each with a flue, at the corners. The stone extends to the roof, and until it was damaged by earthquake, a brick flue extended above the roof, covered in log cribbing. An ironwork clock decorates the north face of the upper chimney in the lobby. The fireplace is centered in a shallow depression in the lobby floor that sets the area around its hearths apart from the rest of the lobby. Custom ironwork, most notable in the main entrance door and the clock, was forged at the site by an ironmonger named Colpitts.
The dining room extends to the south of the lobby, with log scissors trusses supporting a more shallowly-pitched roof at right angles to the lobby roof. The dining room has its own stone fireplace, less massive than the lobby's, but still large. The Old House guest rooms retain much of their original character.The east and west wings were purposely designed by Reamer to be less prominent than the central house. The wings are three to four stories in height with a mansarded top floor and a flat roof. The east wing is straight, originally with 100 rooms. The west wing is Y-shaped, with 150 guest rooms as built. The interiors of the wings are unremarkable compared with the Old House.
| 10
|
[
"Vent Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Vent Geyser is a geyser in the Upper Geyser Basin of Yellowstone National Park in the United States.
Vent Geyser belongs to the Grand Group (or Grand Geyser Complex), and its eruption is tied to Grand Geyser. Normally, it erupts immediately after Grand and continues to erupt intermittently for about an hour afterward along with Turban Geyser. On rare occasions, it has erupted before Grand or completely by itself. Its fountain reaches a height of 75 feet (23 m) initially then subsides to 20 to 40 feet (6–12 m). At times, it is not possible to see Vent erupting through the steam and spray of Grand Geyser.
| 1
|
[
"Isa Lake",
"country",
"United States of America"
] |
Isa Lake is located in Yellowstone National Park, in the U.S. state of Wyoming. The lake straddles the continental divide at Craig Pass. Indigenous peoples have lived in the Yellowstone region for at least 11,000 years. In the 1800s, at the time of the first European exploration of the area, the region was home to several Indigenous Nations including the Nimíipuu, Absaroke, and Shoshone Nations. Hiram M. Chittenden became the first known European to sight the lake in 1891, while searching for the best routes connecting Old Faithful and the West Thumb Geyser Basin. Chittenden named the lake after Miss Isabel Jelke, from Cincinnati, though it is not clear why.
| 0
|
[
"Isa Lake",
"located in protected area",
"Yellowstone National Park"
] |
Isa Lake is located in Yellowstone National Park, in the U.S. state of Wyoming. The lake straddles the continental divide at Craig Pass. Indigenous peoples have lived in the Yellowstone region for at least 11,000 years. In the 1800s, at the time of the first European exploration of the area, the region was home to several Indigenous Nations including the Nimíipuu, Absaroke, and Shoshone Nations. Hiram M. Chittenden became the first known European to sight the lake in 1891, while searching for the best routes connecting Old Faithful and the West Thumb Geyser Basin. Chittenden named the lake after Miss Isabel Jelke, from Cincinnati, though it is not clear why.
| 2
|
[
"Isa Lake",
"instance of",
"lake"
] |
Isa Lake is located in Yellowstone National Park, in the U.S. state of Wyoming. The lake straddles the continental divide at Craig Pass. Indigenous peoples have lived in the Yellowstone region for at least 11,000 years. In the 1800s, at the time of the first European exploration of the area, the region was home to several Indigenous Nations including the Nimíipuu, Absaroke, and Shoshone Nations. Hiram M. Chittenden became the first known European to sight the lake in 1891, while searching for the best routes connecting Old Faithful and the West Thumb Geyser Basin. Chittenden named the lake after Miss Isabel Jelke, from Cincinnati, though it is not clear why.Isa Lake is believed to be one of the few natural lakes in the world which drain to two different oceans, another being Wollaston Lake. (For similar cases see List of unusual drainage systems.) The east side of the lake drains by way of the Lewis River to the Pacific Ocean and the west side of the lake drains by way of the Firehole River to the Gulf of Mexico.
The lake is easy to visit as it is adjacent to the road that now connects the Old Faithful and West Thumb geysers basins, on what is known as the "lower loop" of the figure-eight roadway which traverses through Yellowstone. The great yellow pond-lily thrives in the lake.
| 3
|
[
"Atomizer Geyser",
"country",
"United States of America"
] |
Atomizer Geyser is a cone geyser in the Upper Geyser Basin (Old Faithful area) of Yellowstone National Park in the United States. Atomizer Geyser is part of the Cascade Group which also includes Artemisia Geyser. The geyser is named for a fine mist resembling the spray from an atomizer that is ejected during major eruptions.
| 0
|
[
"Atomizer Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Atomizer Geyser is a cone geyser in the Upper Geyser Basin (Old Faithful area) of Yellowstone National Park in the United States. Atomizer Geyser is part of the Cascade Group which also includes Artemisia Geyser. The geyser is named for a fine mist resembling the spray from an atomizer that is ejected during major eruptions.Geology
Atomizer has two 3 foot (1 m) tall cones. One of the cones is the jetting cone from which all water jets come. The other cone sprays a fine mist during major eruptions, giving the geyser its name. The geyser erupts in series. The series consists of three to five minor eruptions and one major eruption. Minor eruptions last about one minute and reach to 30 feet (9.1 m). Major eruptions last 8 to 10 minutes and reach 40 to 50 feet (12 to 15 m). Major eruptions have a steam phase following the water phase.Atomizer overflows its pool every few minutes for two to four hours until the first minor eruption occurs. Six to eight minor eruptions occur about one hour apart. Between 15 minutes and 1½ hours after the last minor eruption, the major eruption will begin. After a major eruption, the water pool takes about six hours to refill.
| 1
|
[
"Old Faithful Lodge",
"located in protected area",
"Yellowstone National Park"
] |
Old Faithful Lodge in Yellowstone National Park is located opposite the more famous Old Faithful Inn, facing Old Faithful geyser. The Lodge was built as a series of detached buildings through 1923 and was consolidated into one complex by architect Gilbert Stanley Underwood in 1926-27. The Lodge is included in the Old Faithful Historic District.Compared with the Inn, which is a full-service hotel, the Lodge provides only dining, social, administrative and registration services for lodgers, who are accommodated in detached cabins surrounding the Lodge. Several earlier buildings were consolidated by Underwood into the single rambling structure, with the help of National Park Service architect Daniel Ray Hull, in 1926-27.
| 1
|
[
"Old Faithful Lodge",
"architect",
"Gilbert Stanley Underwood"
] |
Old Faithful Lodge in Yellowstone National Park is located opposite the more famous Old Faithful Inn, facing Old Faithful geyser. The Lodge was built as a series of detached buildings through 1923 and was consolidated into one complex by architect Gilbert Stanley Underwood in 1926-27. The Lodge is included in the Old Faithful Historic District.Compared with the Inn, which is a full-service hotel, the Lodge provides only dining, social, administrative and registration services for lodgers, who are accommodated in detached cabins surrounding the Lodge. Several earlier buildings were consolidated by Underwood into the single rambling structure, with the help of National Park Service architect Daniel Ray Hull, in 1926-27.
| 4
|
[
"Old Faithful Lodge",
"instance of",
"lodge"
] |
Old Faithful Lodge in Yellowstone National Park is located opposite the more famous Old Faithful Inn, facing Old Faithful geyser. The Lodge was built as a series of detached buildings through 1923 and was consolidated into one complex by architect Gilbert Stanley Underwood in 1926-27. The Lodge is included in the Old Faithful Historic District.Compared with the Inn, which is a full-service hotel, the Lodge provides only dining, social, administrative and registration services for lodgers, who are accommodated in detached cabins surrounding the Lodge. Several earlier buildings were consolidated by Underwood into the single rambling structure, with the help of National Park Service architect Daniel Ray Hull, in 1926-27.
| 6
|
[
"Artesia Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Artesia Geyser is a geyser in the Lower Geyser Basin of Yellowstone National Park in the United States. Artesia Geyser is located on the edge of Firehole Lake and is part of the Black Warrior Group which includes Young Hopeful Geyser, Grey Bulger Geyser, and Steady Geyser.
| 1
|
[
"Artesia Geyser",
"instance of",
"geyser"
] |
Artesia Geyser is a geyser in the Lower Geyser Basin of Yellowstone National Park in the United States. Artesia Geyser is located on the edge of Firehole Lake and is part of the Black Warrior Group which includes Young Hopeful Geyser, Grey Bulger Geyser, and Steady Geyser.Geology
Artesia is a perpetual geyser that never stops ejecting water from at least one of its two vents, usually no more than 5 ft (1.5 m). One vent is angled toward the boardwalk that passes the geyser and the other is angled toward Firehole Lake.During a period in 1999, one of the vents jetted to a distance of 12 ft (3.7 m) while the other emitted only steam.In 2012, Artesia was having prominent, vertical eruptions about once a minute, with minimal activity between. From 2014 to 2017, it was a low perpetual spouter only. In summer 2018, Artesia resumed having prominent eruptions once a minute, with column heights reaching four to five meters high.
| 3
|
[
"Bead Geyser",
"located in protected area",
"Yellowstone National Park"
] |
Bead Geyser is a cone-type geyser in the Lower Geyser Basin of Yellowstone National Park in the United States.
Bead Geyser is part of the Pink Cone Group. Other geysers in this groups are Box Spring, Dilemma Geyser, Labial Geyser, Labial's Satellite Geyser, Narcissus Geyser, Pink Geyser, and Pink Cone Geyser. Eruptions of Bead Geyser last about 2½ minutes and are 25 feet (7.6 m) high. Bead is an extremely regular geyser. The interval between eruptions is 28–36 minutes. This changes with time but the average for any given time hardly varies. The duration is also highly regular at about 150 seconds.Bead Geyser was named after the geyser eggs, loose spherical pieces of geyserite, that used to be found near the geyser. Over the decades since it was discovered, souvenir hunters have removed all of the geyser eggs.
| 1
|
[
"Abiathar Peak",
"country",
"United States of America"
] |
Abiathar Peak is a mountain peak with an elevation of 10,928 feet (3,331 m) in the northeastern section of Yellowstone National Park, in the Absaroka Range of the U.S. state of Wyoming. The peak was named by members of the 1885 Hague Geological Survey to honor Charles Abiathar White, a geologist and paleontologist who had participated in early western geological surveys. White never visited Yellowstone.
| 0
|
[
"Abiathar Peak",
"located in protected area",
"Yellowstone National Park"
] |
Abiathar Peak is a mountain peak with an elevation of 10,928 feet (3,331 m) in the northeastern section of Yellowstone National Park, in the Absaroka Range of the U.S. state of Wyoming. The peak was named by members of the 1885 Hague Geological Survey to honor Charles Abiathar White, a geologist and paleontologist who had participated in early western geological surveys. White never visited Yellowstone.
| 1
|
[
"Abiathar Peak",
"located in the administrative territorial entity",
"Wyoming"
] |
Abiathar Peak is a mountain peak with an elevation of 10,928 feet (3,331 m) in the northeastern section of Yellowstone National Park, in the Absaroka Range of the U.S. state of Wyoming. The peak was named by members of the 1885 Hague Geological Survey to honor Charles Abiathar White, a geologist and paleontologist who had participated in early western geological surveys. White never visited Yellowstone.
| 2
|
[
"Abiathar Peak",
"instance of",
"mountain"
] |
Abiathar Peak is a mountain peak with an elevation of 10,928 feet (3,331 m) in the northeastern section of Yellowstone National Park, in the Absaroka Range of the U.S. state of Wyoming. The peak was named by members of the 1885 Hague Geological Survey to honor Charles Abiathar White, a geologist and paleontologist who had participated in early western geological surveys. White never visited Yellowstone.
| 3
|
[
"Abiathar Peak",
"mountain range",
"Absaroka Range"
] |
Abiathar Peak is a mountain peak with an elevation of 10,928 feet (3,331 m) in the northeastern section of Yellowstone National Park, in the Absaroka Range of the U.S. state of Wyoming. The peak was named by members of the 1885 Hague Geological Survey to honor Charles Abiathar White, a geologist and paleontologist who had participated in early western geological surveys. White never visited Yellowstone.
| 4
|
[
"Abiathar Peak",
"named after",
"Charles Abiathar White"
] |
Abiathar Peak is a mountain peak with an elevation of 10,928 feet (3,331 m) in the northeastern section of Yellowstone National Park, in the Absaroka Range of the U.S. state of Wyoming. The peak was named by members of the 1885 Hague Geological Survey to honor Charles Abiathar White, a geologist and paleontologist who had participated in early western geological surveys. White never visited Yellowstone.
| 5
|
[
"Artist Point",
"located in the administrative territorial entity",
"Park County"
] |
Artist Point is an overlook point on the edge of a cliff on the south rim of the Grand Canyon of the Yellowstone in Yellowstone National Park, Wyoming. The point is located east-northeast of Yellowstone Falls on the Yellowstone River. Artist Point was originally named in 1883 by Frank Jay Haynes who improperly believed that the point was the place at which painter Thomas Moran sketched his 1872 depictions of the falls. Later work determined that the sketches were made from the north rim, but the name Artist Point stuck.
| 5
|
[
"Atkins Peak",
"country",
"United States of America"
] |
Atkins Peak, elevation 10,928 feet (3,331 m), is a mountain peak in the eastern section of the Absaroka Range in Yellowstone National Park, in the U.S. state of Wyoming.
| 0
|
[
"Atkins Peak",
"located in protected area",
"Yellowstone National Park"
] |
Atkins Peak, elevation 10,928 feet (3,331 m), is a mountain peak in the eastern section of the Absaroka Range in Yellowstone National Park, in the U.S. state of Wyoming.== Notes ==
| 1
|
[
"Atkins Peak",
"located in the administrative territorial entity",
"Wyoming"
] |
Atkins Peak, elevation 10,928 feet (3,331 m), is a mountain peak in the eastern section of the Absaroka Range in Yellowstone National Park, in the U.S. state of Wyoming.See also
Mountains and mountain ranges of Yellowstone National Park== Notes ==
| 2
|
[
"Atkins Peak",
"mountain range",
"Absaroka Range"
] |
Atkins Peak, elevation 10,928 feet (3,331 m), is a mountain peak in the eastern section of the Absaroka Range in Yellowstone National Park, in the U.S. state of Wyoming.
| 3
|
[
"Atkins Peak",
"instance of",
"mountain"
] |
Atkins Peak, elevation 10,928 feet (3,331 m), is a mountain peak in the eastern section of the Absaroka Range in Yellowstone National Park, in the U.S. state of Wyoming.
| 4
|
[
"Bannock Peak",
"located in the administrative territorial entity",
"Wyoming"
] |
== Notes ==
| 2
|
[
"Bannock Peak",
"instance of",
"mountain"
] |
Bannock Peak is a mountain peak in the southern section of the Gallatin Range in Yellowstone National Park, in the U.S. state of Montana. It has an elevation of 10,292 feet (3,137 m).
| 3
|
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