Sarmila/GeoWiki-Features huggingface dataset:
Chang Peak and Mount Waesche appear to be located outside of the Executive Committee Range volcanic lineament. The volcano erupted comendite, hawaiite and mugearite, with the former found at Chang Peak and the latter two at Mount Waesche proper; the parasitic cones have erupted a mugearite-benmoreite succession. The occurrence of rhyolite has also been reported.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
The occurrence of rhyolite has also been reported. There appear to be two groups of volcanic rocks at Mount Waesche. Phenocrysts at Chang Peak include aenigmatite, alkali feldspar, ilmenite and quartz and at Mount Waesche olivine, plagioclase and titanaugite. Granulite and pyroxenite xenoliths have also been found.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Granulite and pyroxenite xenoliths have also been found. Despite their proximity, Mount Sidley and Mount Waesche have erupted distinctly different rocks. Unusually for volcanoes in Marie Byrd Land, the chemistry of volcanic rocks at Mount Waesche appears to have changed over time. The total volume of rocks is about. Eruption history.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
Eruption history. The development of Mount Waesche began in the Pliocene, and Plio-Pleistocene tephra layers found in the Southern Pacific Ocean may originate at Mount Waesche. It appears that volcanism in the Executive Committee Range moved southwards over time, beginning at Mount Hampton and eventually arriving at Mount Waesche which is the young volcanic centre of the range.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Chang Peak grew first, 1.6 million years ago or between 2.01.1 million years ago, while Mount Waesche formed within or about 1 million years ago; the youngest rocks at Waesche are less than 100,000 years old whereas there is no evidence of recent activity at Chang Peak. Argon-argon dating on rocks that today form moraines has yielded ages of about 200,000 years to over 500,000 years.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
The volcano was active during the Holocene and may be a source of tephra found in ice cores. A layer of volcanic ash, about 8,000 years old, that was identified in the region through radar data probably originated at Mount Waesche. The volcano today is considered to be &quot;probably active&quot; or &quot;possibly active&quot;.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
The volcano today is considered to be &quot;probably active&quot; or &quot;possibly active&quot;. A magmatic system may exist south of Mount Waesche at depth below the ice. Present-day seismic activity has been recorded at Mount Waesche, but it might be either volcanic/tectonic or caused by ice movement. Future eruptions are unlikely to have any impact beyond the surroundings of the volcano.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
The volcano today is considered to be &quot;probably active&quot; or &quot;possibly active&quot;. A magmatic system may exist south of Mount Waesche at depth below the ice. Present-day seismic activity has been recorded at Mount Waesche, but it might be either volcanic/tectonic or caused by ice movement. Future eruptions are unlikely to have any impact beyond the surroundings of the volcano.

Geographic entities mentioned:
surface_form: waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
surface_form: mount waesche
instance_of: Mountain
coordinates: lat: -77.166666666667
lon: -126.9
A layer of volcanic ash, about 8,000 years old, that was identified in the region through radar data probably originated at Mount Waesche. The volcano today is considered to be &quot;probably active&quot; or &quot;possibly active&quot;. A magmatic system may exist south of Mount Waesche at depth below the ice.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
It was discovered by the United States Antarctic Service expedition on a flight on December 15, 1940, and named for Vice Admiral Russell R. Waesche, United States Coast Guard, member of the Antarctic Service Executive Committee. Field studies took place in 1999-2000 and 2018–2019. Geography and geomorphology. Mount Waesche lies in Marie Byrd Land, one of the most inaccessible areas of Antarctica.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Field studies took place in 1999-2000 and 2018–2019. Geography and geomorphology. Mount Waesche lies in Marie Byrd Land, one of the most inaccessible areas of Antarctica. It is one of 18 volcanoes in that region, which were active from the Oligocene to recent times. The origin of volcanic activity there has been correlated to the activity of a mantle plume underneath the crust.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Glacial drift lies on the ice-free southwestern flank. In turn, glacial moraines have been overrun by lava flows. Two sets of moraines formed by volcanic debris – one containing ice, the other without – lie on the southern and southwestern flank, reaching heights of and lengths of about.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
The main destinations were famous temples and Shinto shrines around the country, and eating and drinking at the inns and prostitution were one of the main attractions. What people admired most was the visit to Ise Grand Shrine and the summit of Mount Fuji, which are considered the most sacred places in Japan. The Ise Grand Shrine in particular has been visited by an enormous number of visitors.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
It was a once-in-a-lifetime event for people living in remote areas, so they set up a joint fund for each village, saved their travel expenses, and went on a group trip. Local residents of Ise Grand Shrine and Mount Fuji used to send specialized advertising personnel to various parts of Japan to solicit trips to local areas to make money from tourism. Fashion.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
In 1860, the southern extension was completed, including lucrative connections to the Virginia and Tennessee Railroad and the South Side Railroad. The O&A also connected with the Manassas Gap Railroad (chartered in 1850), at Tudor Hall (today named Manassas for this junction) which gave it access to the Shenandoah Valley. The railroad boosted Virginia commerce.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The 84th Regiment was also involved in offensive action in the Thirteen Colonies; including North Carolina, South Carolina, Georgia, Virginia, and what is now Maine, as well as raids upon Lake Champlain and the Mohawk Valley. The regiment consisted of 2,000 men in twenty companies.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: Mohawk Valley
instance_of: Valley
countries: United States
While the presence of bucrania was typically used with the Doric order, the Romans were not strict about this. In a first-century fresco from Boscoreale, protected by the eruption of Mount Vesuvius and now at the Metropolitan Museum of Art, bucrania and cistae mysticae hang on ribbons from pegs that support garlands, evoking joyous &quot;fasti&quot;.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Muota. The Muota is a river in the Swiss canton of Schwyz and a tributary of Lake Lucerne. It has a length of. The Muota rises on the Ruosalp, an alp to the north of the Glatten on the border between the cantons of Schwyz and Uri. Initially, it flows in a northerly direction through the tiny Bisistal before turning west to the villages of Muotathal and Ried.

Geographic entities mentioned:
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
After leaving this canyon, the river turns north to reach the village of Ibach in the municipality of Schwyz. At Ibach the river turns west again, then shortly afterwards passes under the A4 motorway and the Gotthard railway line before receiving the Seeweren, which is the outfall stream of Lake Lauerz.

Geographic entities mentioned:
surface_form: Lake Lauerz
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.033611111111
lon: 8.6033333333333
At Ibach the river turns west again, then shortly afterwards passes under the A4 motorway and the Gotthard railway line before receiving the Seeweren, which is the outfall stream of Lake Lauerz. Here it flows south-west to enter Lake Lucerne on the west side of the town of Brunnen in the municipality of Ingenbohl.

Geographic entities mentioned:
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
High Knob (disambiguation). ydx5zwuwcg4orgyn3144gkin6rno" xml:space="preserve">High Knob is a mountain peak in Virginia.

Geographic entities mentioned:
surface_form: High Knob
instance_of: Mountain
countries: United States
coordinates: lat: 36.8926
lon: -82.6296
Hilda Peak. __NOTOC__
Hilda Peak is a mountain summit located at the northern extreme of Banff National Park in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Athabasca, to the southwest. Hilda Peak is situated south of Sunwapta Pass and can be prominently seen from the Icefields Parkway.

Geographic entities mentioned:
surface_form: Mount Athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
Hilda Peak. __NOTOC__
Hilda Peak is a mountain summit located at the northern extreme of Banff National Park in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Athabasca, to the southwest. Hilda Peak is situated south of Sunwapta Pass and can be prominently seen from the Icefields Parkway.

Geographic entities mentioned:
surface_form: hilda peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.19032
lon: -117.17868
Hilda Peak. __NOTOC__
Hilda Peak is a mountain summit located at the northern extreme of Banff National Park in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Athabasca, to the southwest. Hilda Peak is situated south of Sunwapta Pass and can be prominently seen from the Icefields Parkway.

Geographic entities mentioned:
surface_form: hilda peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.19032
lon: -117.17868
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The nearest higher peak is Mount Athabasca, to the southwest. Hilda Peak is situated south of Sunwapta Pass and can be prominently seen from the Icefields Parkway. The Hilda Glacier lies to the south side of the peak, and the Boundary Glacier lies to the west. History. The first ascent of the mountain was made in 1938 by E. Brooks, H. Brooks, R. Cross, and W. Marples.

Geographic entities mentioned:
surface_form: hilda peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.19032
lon: -117.17868
History. The first ascent of the mountain was made in 1938 by E. Brooks, H. Brooks, R. Cross, and W. Marples. The mountain was named Hilda Peak in 1938. The mountain's name was officially adopted in 1985 when approved by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Hilda Peak is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: hilda peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.19032
lon: -117.17868
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain's name was officially adopted in 1985 when approved by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Hilda Peak is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: hilda peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.19032
lon: -117.17868
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Hilda Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Winter temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: hilda peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.19032
lon: -117.17868
Climate. Based on the Köppen climate classification, Hilda Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Winter temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Hilda Peak drains east into Hilda Creek, thence Nigel Creek, tributaries of the North Saskatchewan River.

Geographic entities mentioned:
surface_form: hilda peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.19032
lon: -117.17868
The nearest higher peak is Mount Athabasca, to the southwest. Hilda Peak is situated south of Sunwapta Pass and can be prominently seen from the Icefields Parkway. The Hilda Glacier lies to the south side of the peak, and the Boundary Glacier lies to the west. History. The first ascent of the mountain was made in 1938 by E. Brooks, H. Brooks, R. Cross, and W. Marples.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. The first ascent of the mountain was made in 1938 by E. Brooks, H. Brooks, R. Cross, and W. Marples. The mountain was named Hilda Peak in 1938. The mountain's name was officially adopted in 1985 when approved by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Hilda Peak is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Note that the original edition was in German and the title can be translated as &quot;Condition of Farm Labour in Eastern Germany&quot;. In 1890 an association (known as the) of scholars, government officials and other specialists decided to study the situation of landowners in Germany. Weber assumed responsibility for reviewing data from German provinces east of the Elbe River.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Sula Valley. The Valley of Sula (also, Sula Valley) is the largest alluvial valley of Honduras. It is located in the northwest of the country, and within it lie several of Honduras's most important cities, such as San Pedro Sula, El Progreso, Choloma, Puerto Cortés, Villanueva, and Tela.

Geographic entities mentioned:
surface_form: sula valley
instance_of: Valley
countries: Honduras
coordinates: lat: 15.45
lon: -87.85
McClintock Peak. McClintock Peak () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. McClintock Peak is situated along the Continental Divide. The Lake of the Seven Winds sits below the east slopes of the peak and Mount Morgan is to the south. Geology.

Geographic entities mentioned:
surface_form: mcclintock peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.525
lon: -113.473
state of Montana. McClintock Peak is situated along the Continental Divide. The Lake of the Seven Winds sits below the east slopes of the peak and Mount Morgan is to the south. Geology. Like other mountains in Glacier National Park, the mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: Lake of the Seven Winds
instance_of: Lake
countries: United States
coordinates: lat: 48.5233
lon: -113.465
surface_form: mount morgan
instance_of: Mountain
countries: United States
coordinates: lat: 48.5139
lon: -113.473
surface_form: mount morgan
instance_of: Mountain
countries: United States
coordinates: lat: 37.4053
lon: -118.733
surface_form: mount morgan
instance_of: Mountain
countries: United States
coordinates: lat: 37.5113
lon: -118.78
Many of the artifacts on display were uncovered during the Townsend Archaeological Project, which was conducted just up the road from 1999 to 2001. The pioneer gallery includes late-19th and early-20th century items commonly used in rural areas around the region, including a bedroom suite, and tools such as a horseshoeing box and a banjo once played by a resident of Cades Cove.

Geographic entities mentioned:
surface_form: Cades Cove
instance_of: Valley
countries: United States
coordinates: lat: 35.594166666667
lon: -83.841944444444
It is up to about and covers and area of 381.9 square kilometres. It is a large, terraced landscape that is part of the Iller-Lech Plateau in the Alpine Foreland of south Germany. It lies southwest of the city of Ulm in the counties of Alb-Donau-Kreis and Biberach in Upper Swabia and rises above the valley floors by about 75 metres. Mountains and hills.

Geographic entities mentioned:
surface_form: Alpine Foreland
instance_of: Plateau
countries: Germany
coordinates: lat: 48
lon: 12
Jugurtha Tableland. The Jugurtha Tableland is a large mesa near the town of Kalaat es Senan, Tunisia, which stands almost above the Ez-Zghalma plain. long and wide, it covers a total area of nearly 80 hectares. The Tableland is a geologic feature known as an inverted relief. Millions of years ago, the hard limestone top of the mesa was actually the bottom of a valley.

Geographic entities mentioned:
surface_form: jugurtha tableland
instance_of: Mountain
countries: Tunisia
coordinates: lat: 35.74429
lon: 8.37903
Millions of years ago, the hard limestone top of the mesa was actually the bottom of a valley. Over the years, the softer surrounding hills were worn away by erosion, leaving the Tableland – and former low point – as the highest point on a plain. Local drinking water comes from the Ain Senan spring at the edge of the Jugurtha Tableland. History.

Geographic entities mentioned:
surface_form: jugurtha tableland
instance_of: Mountain
countries: Tunisia
coordinates: lat: 35.74429
lon: 8.37903
Similar rocks elsewhere. Blue, unbanded fluorite occurs in many localities around the world. Within the UK, blue fluorspars are also found in County Durham, especially Weardale. Elsewhere, blue fluorspar is known in the Ardennes region of Belgium; the Cave-in-Rock area of Illinois in the United States; and at various localities in Mexico and China. Blue-banded fluorite is very rare.

Geographic entities mentioned:
surface_form: Weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
Sakeny River. The Sakeny River is a river in Western Madagascar. It is a tributary of the Tsiribihina River. The Sakeny originates on the northern Makay Massif in northern Beroroha District of Atsimo-Andrefana Region.

Geographic entities mentioned:
surface_form: Tsiribihina River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.8833
lon: 44.45
Healy Creek. Healy Creek is a stream in Banff National Park, Alberta, Canada. It is a tributary of the Bow River. Healy Creek has the name of John J. Healy, a businessperson in the mining industry. During World War II, an alternative service camp for conscientious objectors, largely Mennonites, was established at Healy Creek.

Geographic entities mentioned:
surface_form: healy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.13332
lon: -115.70211
Geography. The commune is situated on the Transylvanian Plateau, on the left bank of the Mureș River, across from the county seat, Alba Iulia. It borders Sântimbru and Berghin communes to the north, Oarda de Jos village to the south, the city of Alba Iulia to the west, and Daia Română commune to the east.

Geographic entities mentioned:
surface_form: Transylvanian Plateau
instance_of: Plateau
countries: Romania
coordinates: lat: 46.5
lon: 24.5
They are bounded to the west and north-west by the Fulda valley, and to the east and north-east by the Werra valley. The southern boundary is less clearly defined, as the range merges into the gentler hills of the Söhrewald to the south-west, and climbs towards the high plateau of the Hoher Meißner to the south-east.

Geographic entities mentioned:
surface_form: Hoher Meißner
instance_of: Mountain
countries: Germany
coordinates: lat: 51.207777777778
lon: 9.8472222222222
The present tower was erected in 1889 and extended to its present height of in 1960; it offers panoramic views across the region. Other peaks include Mühlenstein (),
Haferberg (), Langenberg (), Großer Steinberg () and Kleiner Steinberg ().

Geographic entities mentioned:
surface_form: Mühlenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 51.305
lon: 9.7677777777778
Angulalik's trade partners included distant Copper Inuit bands such as the &quot;Hanningajurmiut&quot; of Garry Lake (&quot;Hanningajuq&quot;, meaning &quot;sideways&quot; or &quot;crooked&quot;).

Geographic entities mentioned:
surface_form: Garry Lake
instance_of: Lake
countries: Canada
coordinates: lat: 65.966667
lon: -100.3
The language of instruction is English. History. The Lebanese International University was established in April, 2001, as &quot;The Bekaa University&quot; under Presidential Decree No.5294 as, with its campus constructed within the western region of the Beqaa Valley; at Al-Khyara, the West Beqaa (al-Beqaa al-Gharbi).

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Ford led the Antelope Hills expedition into the Comancheria, winning the Battle of Antelope Hills in May. Later in the year, the Rangers fought an inconclusive battle in the Rio Grande Valley against Mexican bandit Juan Cortina. Despite these efforts, the Rangers failed to secure peace on the frontier.

Geographic entities mentioned:
surface_form: Rio Grande Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 26.22
lon: -98.12
It is a popular area for hikers, camping, fishing and sightseers seeking to see mountain goats that frequent the western hillside of the lake. Hiking to Twin Lakes is approximately 4 miles from Marble Pass. The highest point in the range is Rock Creek Butte, located on the northern ridge above the lakes. Other alpine lakes are found a short distance from Twin Lakes.

Geographic entities mentioned:
surface_form: Rock Creek Butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.816666666667
lon: -118.10361111111
Hiking to Twin Lakes is approximately 4 miles from Marble Pass. The highest point in the range is Rock Creek Butte, located on the northern ridge above the lakes. Other alpine lakes are found a short distance from Twin Lakes. To the north over the northern skirt of Rock Creek Butte is Rock Creek Lake and Bucket Lake and to the east is Goodrich Lake over the Elkhorn Crest trail. Ecology.

Geographic entities mentioned:
surface_form: Rock Creek Lake
instance_of: Lake
countries: United States
surface_form: rock creek butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.816666666667
lon: -118.10361111111
Twin Lakes (Baker County, Oregon). Twin Lakes is the name of a set of two alpine lakes along the Elkhorn Crest trail in the southern end of the Elkhorn Mountains in Baker County, eastern Oregon. It is a popular area for hikers, camping, fishing and sightseers seeking to see mountain goats that frequent the western hillside of the lake.

Geographic entities mentioned:
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.6181
lon: -119.008
surface_form: twin lakes (baker county, oregon)
instance_of: Lake
countries: United States
coordinates: lat: 44.8079
lon: -118.0867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 40.7433
lon: -115.283
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.0183
lon: -73.3867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.23888889
lon: -111.86472222
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 60.638888888889
lon: -153.86305555556
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 48.6494
lon: -113.718
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.7487796
lon: -84.4527626
surface_form: twin lakes
instance_of: Lake
countries: United States
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.6375
lon: -89.41583333333334
Twin Lakes (Baker County, Oregon). Twin Lakes is the name of a set of two alpine lakes along the Elkhorn Crest trail in the southern end of the Elkhorn Mountains in Baker County, eastern Oregon. It is a popular area for hikers, camping, fishing and sightseers seeking to see mountain goats that frequent the western hillside of the lake.

Geographic entities mentioned:
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
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It is a popular area for hikers, camping, fishing and sightseers seeking to see mountain goats that frequent the western hillside of the lake. Hiking to Twin Lakes is approximately 4 miles from Marble Pass. The highest point in the range is Rock Creek Butte, located on the northern ridge above the lakes. Other alpine lakes are found a short distance from Twin Lakes.

Geographic entities mentioned:
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Hiking to Twin Lakes is approximately 4 miles from Marble Pass. The highest point in the range is Rock Creek Butte, located on the northern ridge above the lakes. Other alpine lakes are found a short distance from Twin Lakes. To the north over the northern skirt of Rock Creek Butte is Rock Creek Lake and Bucket Lake and to the east is Goodrich Lake over the Elkhorn Crest trail. Ecology.

Geographic entities mentioned:
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coordinates: lat: 44.6375
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Other alpine lakes are found a short distance from Twin Lakes. To the north over the northern skirt of Rock Creek Butte is Rock Creek Lake and Bucket Lake and to the east is Goodrich Lake over the Elkhorn Crest trail. Ecology. Twin Lakes is surrounded by an open forest with scattered old growth spruce and Douglas-fir trees. It is surrounded by open hillside meadows with wildflowers in the summer.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 27.893888888889
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Ecology. Twin Lakes is surrounded by an open forest with scattered old growth spruce and Douglas-fir trees. It is surrounded by open hillside meadows with wildflowers in the summer. Resident osprey and bluebirds nest in the area around Twin Lakes. Mountain goats are often seen in their haunts on the ridge west of the Twin Lakes basin. Mountain Goats.

Geographic entities mentioned:
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countries: United States
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It is surrounded by open hillside meadows with wildflowers in the summer. Resident osprey and bluebirds nest in the area around Twin Lakes. Mountain goats are often seen in their haunts on the ridge west of the Twin Lakes basin. Mountain Goats. The Twin Lakes basin is a frequented location by mountain goats.

Geographic entities mentioned:
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countries: United States
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Resident osprey and bluebirds nest in the area around Twin Lakes. Mountain goats are often seen in their haunts on the ridge west of the Twin Lakes basin. Mountain Goats. The Twin Lakes basin is a frequented location by mountain goats. A census in 2019 yielded 100 goats in the Twin Lakes basin, approximately a third of the goats in the Elkhorn mountain range.

Geographic entities mentioned:
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countries: United States
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Mountain Goats. The Twin Lakes basin is a frequented location by mountain goats. A census in 2019 yielded 100 goats in the Twin Lakes basin, approximately a third of the goats in the Elkhorn mountain range. The population was established after 21 goats were released between 1983 and 1986 along the Pine Creek drainage, a short distance north of the Twin Lakes.

Geographic entities mentioned:
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A census in 2019 yielded 100 goats in the Twin Lakes basin, approximately a third of the goats in the Elkhorn mountain range. The population was established after 21 goats were released between 1983 and 1986 along the Pine Creek drainage, a short distance north of the Twin Lakes. These individuals had been purposefully trapped in Idaho, Washington and Alaska.

Geographic entities mentioned:
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countries: United States
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Goats are now trapped by wildlife management within the Elkhorn Mountains for transplant to other regions of Oregon, including the neighboring Wallowa Mountains, Hells Canyon. Geology. Twin Lakes lay within the Lake Creek Glacier which was fed by two cirques and is a location of unknown age. The glacier generated ice water flowed southeast from the ridge and then veered south at the cirque.

Geographic entities mentioned:
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countries: United States
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The Elkhorn Ridge Argillite surrounds the cirques and is primarily composed of deformed sedimentary rock, primarily dark-colored siliceous argillite. Activities. Twin Lakes is located along Elkhorn Crest trail, the highest trail in the Blue Mountains. Twin lakes is a frequent stop for hunters, day hikers, backpackers, mountain bikers and horseback riders that travel along Elkhorn Crest trail.

Geographic entities mentioned:
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