Sarmila/GeoWiki-Features huggingface dataset:
Goat Mountain has a subsidiary 6,725 ft summit known as the west peak, and remnants of what was colloquially known as the Swamp Creek Glacier rest on the northern slope between the two summits. The nearest higher neighbor is Mount Chardonnay, to the east. The Silver Tip Mine was located on the south slope of the mountain near the 3,000 ft level. The mine produced silver and gold in the 1940s.

Geographic entities mentioned:
surface_form: Mount Chardonnay
instance_of: Mountain
countries: United States
coordinates: lat: 48.927567
lon: -121.56608
Goat Mountain (Whatcom County). Goat Mountain is a summit in the Skagit Range which is a subset of the North Cascades of Washington state. It is located south of Mount Larrabee and north of Mount Shuksan in the Mount Baker Wilderness, which is managed by the Mount Baker-Snoqualmie National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7742
lon: -114.142
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 61.047222222222
lon: -149.04972222222
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.705
lon: -113.591
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.92846
lon: -121.62625
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.86994
lon: -118.57427
Goat Mountain (Whatcom County). Goat Mountain is a summit in the Skagit Range which is a subset of the North Cascades of Washington state. It is located south of Mount Larrabee and north of Mount Shuksan in the Mount Baker Wilderness, which is managed by the Mount Baker-Snoqualmie National Forest.

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7742
lon: -114.142
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 61.047222222222
lon: -149.04972222222
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.705
lon: -113.591
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.92846
lon: -121.62625
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.86994
lon: -118.57427
It is located south of Mount Larrabee and north of Mount Shuksan in the Mount Baker Wilderness, which is managed by the Mount Baker-Snoqualmie National Forest. Goat Mountain has a subsidiary 6,725 ft summit known as the west peak, and remnants of what was colloquially known as the Swamp Creek Glacier rest on the northern slope between the two summits.

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7742
lon: -114.142
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.7232516
lon: -123.3490055
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 61.047222222222
lon: -149.04972222222
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.705
lon: -113.591
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.92846
lon: -121.62625
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.5625
lon: -72.8444
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.779722222222
lon: -109.53638888889
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.86994
lon: -118.57427
surface_form: west peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.73361111
lon: -112.48416667
The mine produced silver and gold in the 1940s. Precipitation runoff from the mountain drains into tributaries of the Fraser River and the Nooksack River. Climate. Goat Mountain is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7742
lon: -114.142
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 61.047222222222
lon: -149.04972222222
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.705
lon: -113.591
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.92846
lon: -121.62625
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.86994
lon: -118.57427
In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago. The rock of Goat Mountain is Darrington Phyllite of the Easton terrane. During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris.

Geographic entities mentioned:
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7742
lon: -114.142
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 61.047222222222
lon: -149.04972222222
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.705
lon: -113.591
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.92846
lon: -121.62625
surface_form: goat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.86994
lon: -118.57427
Gurkarpo Ri is a glaciated summit in the Himalayas on the China–Nepal border. It is situated northeast of Kathmandu on the boundary shared by Langtang National Park and Qomolangma National Nature Preserve. Precipitation runoff from the mountain's south and west slopes drains to the Trishuli River via Lānṭān Kholā, whereas the northeast slope drains into tributaries of the Bhotekoshi River.

Geographic entities mentioned:
surface_form: Bhotekoshi River
instance_of: Watercourse
countries: Nepal
People's Republic of China
coordinates: lat: 27.712
lon: 85.765
Climate. Based on the Köppen climate classification, Gurkarpo Ri is located in a tundra climate zone with cold, snowy winters, and cool summers. Weather systems coming off the Bay of Bengal are forced upwards by the Himalaya mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Mid-June through early-August is the monsoon season.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Lake Luzerne (New York). Lake Luzerne is located in the town of Lake Luzerne, New York. Fish species present in the lake are northern pike, smallmouth bass, largemouth bass, rainbow trout, brown trout, rock bass, bluegill, yellow perch, pumpkinseed sunfish, brown bullhead, and chain pickerel. There is a boat launch on the west shore off County Route 9.

Geographic entities mentioned:
surface_form: lake luzerne
instance_of: Lake
countries: United States
coordinates: lat: 43.3230504
lon: -73.8325487
Lake Luzerne (New York). Lake Luzerne is located in the town of Lake Luzerne, New York. Fish species present in the lake are northern pike, smallmouth bass, largemouth bass, rainbow trout, brown trout, rock bass, bluegill, yellow perch, pumpkinseed sunfish, brown bullhead, and chain pickerel. There is a boat launch on the west shore off County Route 9.

Geographic entities mentioned:
surface_form: lake luzerne
instance_of: Lake
countries: United States
coordinates: lat: 43.3230504
lon: -73.8325487
surface_form: lake luzerne
instance_of: Lake
countries: United States
coordinates: lat: 43.3230504
lon: -73.8325487
This is dangerous because the water is not very deep in this location. Ivy Island is the sole island in the lake. Access to the island is prohibited without permission from the town of Lake Luzerne. A trespassing fine of $250 has been imposed. According to local lore, the island is so named because of the presence of poison ivy.

Geographic entities mentioned:
surface_form: lake luzerne
instance_of: Lake
countries: United States
coordinates: lat: 43.3230504
lon: -73.8325487
The county can be divided into four major geographic divisions: the low-lying and relatively flat valley of Pumpkin Creek, which occupies about 40% of the county's area; a tableland, in places smooth and in others deeply dissected, occupying the southern one-third of the county; the Wildcat Hills, a highly dissected escarpment that crosses the county's northwestern portion; and a small portion of the North Platte River valley in the county's northeastern corner.

Geographic entities mentioned:
surface_form: Wildcat Hills
instance_of: Landform
countries: United States
coordinates: lat: 41.7022
lon: -103.667
It contained four time trial events, there of which were individual and one a team event. There were eleven stages containing high mountains, of which five had summit finishes: stage 5, to Massiccio del Sirino; stage 8, to Gran Sasso d'Italia; stage 15, to Santuario di Oropa; stage 19, to Alpe di Pampeago; and stage 20, to Madonna di Campiglio. The organizers chose to include one rest day.

Geographic entities mentioned:
surface_form: Massiccio del Sirino
instance_of: Mountain
countries: Italy
coordinates: lat: 40.13277778
lon: 15.83611111
Gråkammen Ridge. Gråkammen Ridge () is a mountainous ridge that includes Tambovskaya Peak and Mount Solov'yev, rising between the Gråhorna Peaks and Aurdalen Valley in the Westliche Petermann Range of the Wohlthat Mountains in Antarctica. It was discovered and plotted from air photos by the Third German Antarctic Expedition, 1938–39.

Geographic entities mentioned:
surface_form: Tambovskaya Peak
instance_of: Mountain
coordinates: lat: -71.6833
lon: 12.3333
surface_form: Mount Solov'yev
instance_of: Mountain
coordinates: lat: -71.68333333
lon: 12.31666667
surface_form: Gråhorna Peaks
instance_of: Mountain
coordinates: lat: -71.6
lon: 12.2667
surface_form: Aurdalen Valley
instance_of: Valley
coordinates: lat: -71.7
lon: 12.366666666667
Elephant Butte (Hidalgo County, New Mexico). Elephant Butte is a summit in Hidalgo County, New Mexico. It lies at an elevation of, on the Cowboy Rim of the Animas Mountains.

Geographic entities mentioned:
surface_form: elephant butte
instance_of: Mountain
countries: United States
coordinates: lat: 48.79251
lon: -121.21861
surface_form: elephant butte
instance_of: Mountain
countries: United States
coordinates: lat: 38.695808
lon: -109.5401075
surface_form: elephant butte
instance_of: Mountain
countries: United States
coordinates: lat: 33.15666667
lon: -107.18444444
surface_form: elephant butte (hidalgo county, new mexico)
instance_of: Mountain
countries: United States
coordinates: lat: 31.61111111
lon: -108.64944444
Elephant Butte (Hidalgo County, New Mexico). Elephant Butte is a summit in Hidalgo County, New Mexico. It lies at an elevation of, on the Cowboy Rim of the Animas Mountains.

Geographic entities mentioned:
surface_form: elephant butte
instance_of: Mountain
countries: United States
coordinates: lat: 48.79251
lon: -121.21861
surface_form: elephant butte
instance_of: Mountain
countries: United States
coordinates: lat: 38.695808
lon: -109.5401075
surface_form: elephant butte
instance_of: Mountain
countries: United States
coordinates: lat: 33.15666667
lon: -107.18444444
surface_form: elephant butte
instance_of: Mountain
countries: United States
coordinates: lat: 31.61111111
lon: -108.64944444
It closed permanently in 1910. Demographics. In the, Westvale had &quot;no people or a very low population&quot;. In the, Westvale had &quot;no people or a very low population&quot;. Education. There are no schools in the locality. The nearest government primary schools are in Kilcoy and Mount Mee. The nearest government secondary schools is in Kilcoy and Toogoolawah.

Geographic entities mentioned:
surface_form: Mount Mee
instance_of: Mountain
countries: Australia
coordinates: lat: -27.074166666667
lon: 152.76972222222
The majority of the park is in Todd Township along Pennsylvania Route 994, east of the unincorporated village of Entriken. Huntingdon is the nearest borough. The park borders Rothrock State Forest and Raystown Lake National Recreation Area. There is a growing population of bald eagles at the lake. Fourteen eagles were spotted in January 2007.

Geographic entities mentioned:
surface_form: Raystown Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.433611111111
lon: -78.006666666667
Geology. Trough Creek State Park is in the southern section of the Ridge and Valley region of Pennsylvania. Great Trough Creek carved a valley through the Broad Top in the Appalachian Mountains, which have been greatly reduced in size by the effects of wind and water erosion.

Geographic entities mentioned:
surface_form: Broad Top
instance_of: Plateau
countries: United States
coordinates: lat: 40.205
lon: -78.146
Fishing is quite popular at Trough Creek State Park. Stream fishing is available in Great Trough Creek. Lake fishing is available in a cove of Raystown Lake that is within the park boundaries. Great Trough Creek holds a variety of fish including, trout, panfish, rock bass, sucker and smallmouth bass. Shad can be caught during their run at the mouths of the streams that feed into Raystown Lake.

Geographic entities mentioned:
surface_form: Raystown Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.433611111111
lon: -78.006666666667
Valley of Heart's Delight. &quot;Valley of Heart's Delight&quot; is a 2023 studio album by American country musician Margo Cilker. The album has received positive reviews from critics and investigates Cilker's childhood growing up in the Santa Clara Valley. Reception.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Sind Valley. The Sind Valley is a Himalayan sub-valley of the Kashmir Valley in the Indian union territory of Jammu and Kashmir. The entrance of the Sind Valley lies northeast of Srinagar the capital of Jammu and Kashmir. It is a long gorge valley with an average width of. History. The Sind Valley had a strategic importance on the ancient Silk Road.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
surface_form: sind valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
Geography. The Sind Valley is situated within the jurisdiction of Kangan tehsil, of Ganderbal district. It is bordered by the Kashmir Valley in the west, Zojila in the east, Gurez Valley of the Kishanganga River in the north and the Lidder Valley in the south.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
surface_form: Lidder Valley
instance_of: Valley
countries: India
coordinates: lat: 33.7764
lon: 75.2133
It is bordered by the Kashmir Valley in the west, Zojila in the east, Gurez Valley of the Kishanganga River in the north and the Lidder Valley in the south. It has a length of and reaches a maximum length of at village Preng towards the north through a stream Wangath Nala which flows down from Gangabal Lake.

Geographic entities mentioned:
surface_form: Gangabal Lake
instance_of: Lake
countries: India
coordinates: lat: 34.4325
lon: 74.925
It has a length of and reaches a maximum length of at village Preng towards the north through a stream Wangath Nala which flows down from Gangabal Lake. At some places the width is less than which gives only space to NH 1D, a National Highway which connects Ladakh and the Kashmir Valley. It is formed by the flow of the Sind River which flows down from east to west.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Sind Valley. The Sind Valley is a Himalayan sub-valley of the Kashmir Valley in the Indian union territory of Jammu and Kashmir. The entrance of the Sind Valley lies northeast of Srinagar the capital of Jammu and Kashmir. It is a long gorge valley with an average width of. History. The Sind Valley had a strategic importance on the ancient Silk Road.

Geographic entities mentioned:
surface_form: sind valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
The entrance of the Sind Valley lies northeast of Srinagar the capital of Jammu and Kashmir. It is a long gorge valley with an average width of. History. The Sind Valley had a strategic importance on the ancient Silk Road. It worked as a bridge between India, China and Central Asia along with Srinagar-Skardu Route. First Hinduism and Buddhism and then Islam spread in Kashmir through this route.

Geographic entities mentioned:
surface_form: sind valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
It worked as a bridge between India, China and Central Asia along with Srinagar-Skardu Route. First Hinduism and Buddhism and then Islam spread in Kashmir through this route. The Sind Valley still connects Ladakh with the rest of India through a National Highway NH 1D, though it remains closed during winter due to heavy snowfall at Zojila. Geography.

Geographic entities mentioned:
surface_form: sind valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
Geography. The Sind Valley is situated within the jurisdiction of Kangan tehsil, of Ganderbal district. It is bordered by the Kashmir Valley in the west, Zojila in the east, Gurez Valley of the Kishanganga River in the north and the Lidder Valley in the south.

Geographic entities mentioned:
surface_form: sind valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
The River originates from the inner Himalayas at Drass in Machoi Glacier and runs through green forests of pine and fir and alpine meadows of Sonamarg. The Sind Valley contributes heavily to the economy of the State, through generation of hydroelectricity, provides fresh water supply to other districts and irrigation for agriculture.

Geographic entities mentioned:
surface_form: sind valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
The main towns in the valley are Gund, Mammer, Kangan, Wangath, Preng, Wussan and Manigam. Geology. The Sind Valley has formed over a period of several thousand years as the Sind River cuts into the Himalayan mountains. The glaciers of the valley are shrinking. Today, the river continues to deposit the sheets of sand in the lower areas of Ganderbal.

Geographic entities mentioned:
surface_form: sind valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
Gradual erosive processes have washed away side forests and created a deep gorge at many places. Ecology. The Sind Valley has many glacier fed streams, the tributaries of the Sind River are home to different types of trout among of which is the brown trout. The valley is the natural habitat of Himalayan black bear, the Himalayan brown bear, musk deer, snow leopard and hangul.

Geographic entities mentioned:
surface_form: sind valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
Ecology. The Sind Valley has many glacier fed streams, the tributaries of the Sind River are home to different types of trout among of which is the brown trout. The valley is the natural habitat of Himalayan black bear, the Himalayan brown bear, musk deer, snow leopard and hangul. Markhor and ibex are also spotted in Sonamarg of the Sind Valley.

Geographic entities mentioned:
surface_form: sind valley
instance_of: Valley
countries: India
coordinates: lat: 34.2892
lon: 74.8125
Mun Tung Estate. Mun Tung Estate () is a public housing estate in Tung Chung, Lantau Island, New Territories, Hong Kong near Yat Tung Estate, Hong Chi Shiu Pong Morninghope School, YMCA of Hong Kong Christian College, Caritas Charles Vath College and Tung Chung River. It consists of four residential buildings completed in 2018. Transportation.

Geographic entities mentioned:
surface_form: Tung Chung River
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 22.28
lon: 113.9295
Roman Empire. The first historically confirmed intensive use of the North Sea was by the Romans in 12 BC, when Nero Claudius Drusus built and launched a fleet of over a thousand ships into the North Sea conquering the indigenous tribes, including the Frisii and the Chauci. By 5 BC the Roman knowledge of the Sea was greatly expanded as far as the Elbe by a military expedition under Tiberius.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Coregonus fera. &quot;Coregonus fera&quot;, commonly called the &quot;true fera&quot;, is a presumed extinct freshwater fish from Lake Geneva in Switzerland and France. Description. The fera is a freshwater whitefish that typically grows to between 35 and 40 centimeters in length. It is a member of the common whitefish complex (&quot;Coregonus lavaretus&quot; sensu lato).

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
It is a member of the common whitefish complex (&quot;Coregonus lavaretus&quot; sensu lato). The identity of the fera is disputed. In 1950, Emile Dottrens described &quot;Coregonus fera&quot; as native to both Lake Geneva and Lake Constance. The coregonines from Lake Constance were named &quot;Sandfelchen&quot;.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Piz de Trescolmen. Piz de Trescolmen is a mountain of the Lepontine Alps, situated in the canton of Graubünden, Switzerland. It has several summits: the highest at 2,652 metres and the southern at 2,581 metres. On its southern side it overlooks the Trescolmen Pass (2,161 m).

Geographic entities mentioned:
surface_form: piz de trescolmen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.407083333333
lon: 9.1845555555556
Opuvani do. The Opuvani do (Serbian: &quot;Windy valley&quot;) is a sinkhole at the northern slope of the Velika Jastrebica in the Orjen mountain range located in Montenegro. It creates a major refugium to arcto-alpine and alpine biota in a region with warm winters.

Geographic entities mentioned:
surface_form: Velika Jastrebica
instance_of: Mountain
countries: Bosnia and Herzegovina
Montenegro
coordinates: lat: 42.59788889
lon: 18.5439
surface_form: opuvani do
instance_of: Mountain
countries: Montenegro
Topography and Geology. The Opuvani do is on Mt Orjen on the Bijela gora, which is part of the High Karst nappe. It is formed of Triassic-Paleogene shallow water calcareous sediments, which were interrupted by a short episode of Middle Triassic deepening and rifting-related volcanism, which is characteristic for the larger Adriatic carbonate platform.

Geographic entities mentioned:
surface_form: Bijela gora
instance_of: Plateau
countries: Montenegro
Bosnia and Herzegovina
coordinates: lat: 42.585
lon: 18.57
Opuvani do. The Opuvani do (Serbian: &quot;Windy valley&quot;) is a sinkhole at the northern slope of the Velika Jastrebica in the Orjen mountain range located in Montenegro. It creates a major refugium to arcto-alpine and alpine biota in a region with warm winters.

Geographic entities mentioned:
surface_form: opuvani do
instance_of: Mountain
countries: Montenegro
Route 231 (US 231) in St. Clair County near Pell City to US 431 at Alexandria in Calhoun County. The highway is two lanes for its entire length. The highway also crosses the Coosa River using the bridge across the Neely Henry Dam. History. Until 1997, the section of SR 144 between SR 77 and US 431 was designated as SR 62. SR 62 is now assigned to a short highway in Marshall County.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Lake Alamosa. Lake Alamosa is a former lake in Colorado. It existed from the Pliocene to the middle Pleistocene in the San Luis Valley, fed by glacial meltwater from surrounding mountain ranges.

Geographic entities mentioned:
surface_form: San Luis Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
Groundwater resources are contained trapped between sediments left by the former lake. Description. The lake was in southern Colorado, at high altitude, covering most of the San Luis Valley/San Luis Basin north of the San Luis Hills. It reached an elevation of at highstand. Westwards, Lake Alamosa spread to the San Juan Mountains close to Monte Vista to the west.

Geographic entities mentioned:
surface_form: San Luis Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Northwards, it almost reached the present-day location of Saguache. It was about long in north-south direction and reached a maximum width of, making it one of North America's largest high elevation lakes, comparable only to the historic Lake Texcoco in Mexico. The surface area may have exceeded at highstand.

Geographic entities mentioned:
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
According to modelling, ongoing sedimentation in the lake basin would have led to gradually increasing water levels during each stadial over time. Aside from climatic influences, the Bishop Tuff eruption of the Long Valley caldera in California and the Huckleberry Ridge eruption of the Yellowstone Caldera deposited tephra in Lake Alamosa.

Geographic entities mentioned:
surface_form: Long Valley caldera
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
Additional islands were located in its southern basin; today they are hills. The city of Alamosa and possibly also the town of Center, Colorado are located within the former lake's floor. San Luis Lake presently occupies a small basin in the former lake floor; the basin was previously occupied by a leftover of Lake Alamosa, Lake Sipapu.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
South of Lake Alamosa an even older lake, Lake Sunshine, occupied the Sunshine Valley during the Pliocene. Many lakes in western North America are cyclical, becoming deep and large during stadials and shallow and small during interstadials. Lake Alamosa briefly reached elevations of at Hansen Bluff four times during its history.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
From there water would have flowed across the Costilla Plain and the Taos Plateau to join the Rio Grande and Red River west of Questa, New Mexico. Faulting had weakened rocks at the overflow threshold, thus facilitating erosion of the threshold. More than one channel may have been active as overflow path before the flow became focused on the present-day path of the Rio Grande.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Saddleback Mountain was an island in Lake Alamosa, and its northern side was swept by waves during storms owing to the lake's long fetch. Additional islands were located in its southern basin; today they are hills. The city of Alamosa and possibly also the town of Center, Colorado are located within the former lake's floor.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Geologic history. The San Luis Basin is the largest basin of the Rio Grande Rift and is bordered to the east by a fault. It constitutes an east-tilted half-graben that is subdivided by additional fault systems. Its southern reaches are covered by the volcanic Servilleta Formation. The valley forms the headwaters of the Rio Grande.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
The glaciation was ending at that time, and meltwater from declining glaciers may have helped raise the water levels until the lake overflowed. Continuing uplift in the Southern Rocky Mountains may also have played a role. Lake Alamosa overflowed through the Costilla Plain into New Mexico, in a gap between the Fairy Hills and the Brownie Hills.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Lake Alamosa. Lake Alamosa is a former lake in Colorado. It existed from the Pliocene to the middle Pleistocene in the San Luis Valley, fed by glacial meltwater from surrounding mountain ranges.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
Description. The lake was in southern Colorado, at high altitude, covering most of the San Luis Valley/San Luis Basin north of the San Luis Hills. It reached an elevation of at highstand. Westwards, Lake Alamosa spread to the San Juan Mountains close to Monte Vista to the west. Northwards, it almost reached the present-day location of Saguache.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
The surface area may have exceeded at highstand. It is likely that some water seeped out of the lake before its final overflow as groundwater. Saddleback Mountain was an island in Lake Alamosa, and its northern side was swept by waves during storms owing to the lake's long fetch. Additional islands were located in its southern basin; today they are hills.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
San Luis Lake presently occupies a small basin in the former lake floor; the basin was previously occupied by a leftover of Lake Alamosa, Lake Sipapu. Because of the old age of Lake Alamosa, shorelines and shoreline features are often buried or eroded; in many places former shorelines are only highlighted by changes in vegetation patterns or slope angle.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
Because of the old age of Lake Alamosa, shorelines and shoreline features are often buried or eroded; in many places former shorelines are only highlighted by changes in vegetation patterns or slope angle. Barrier bars, lagoons and spits formed in Lake Alamosa when it reached its highest stand.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
Wind-eroded rock structures occur along its former southeastern shore. Climate. During the glacial times of Lake Alamosa's existence, the basin was colder than today and possibly also drier. The lake was nourished by glacial meltwater coming from the San Juan, Sawatch, and Sangre de Cristo Mountains.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
The valley forms the headwaters of the Rio Grande. Lake Alamosa existed for about 3 million years, from the Pliocene to the middle Pleistocene. Rocks in the San Luis horst stretch across the entire Alamosa Basin and together with 4.8-3.7 million years old basaltic lava flows of the Taos Plateau blocked the basin from draining to the south.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
Tectonic uplift of the Jemez lineament, tectonic subsidence of the Lake Alamosa area and the emplacement of these lava flows may have obstructed former drainages, but evidence of prior southwards drainage has been found only recently. South of Lake Alamosa an even older lake, Lake Sunshine, occupied the Sunshine Valley during the Pliocene.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
Many lakes in western North America are cyclical, becoming deep and large during stadials and shallow and small during interstadials. Lake Alamosa briefly reached elevations of at Hansen Bluff four times during its history. According to modelling, ongoing sedimentation in the lake basin would have led to gradually increasing water levels during each stadial over time.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
Continuing uplift in the Southern Rocky Mountains may also have played a role. Lake Alamosa overflowed through the Costilla Plain into New Mexico, in a gap between the Fairy Hills and the Brownie Hills. From there water would have flowed across the Costilla Plain and the Taos Plateau to join the Rio Grande and Red River west of Questa, New Mexico.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
The water would have reached the Culebra Creek and eventually the Red River at La Junta Point; the Red River constituted the headwater of the Rio Grande during that time. The overflow of Lake Alamosa into the Rio Grande expanded its catchment by about -, adding the high, glaciated San Juan Mountains, the upper Sangre de Cristo Mountains and Sawatch Range to its watershed.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
The decline probably was not as quick as during the Bonneville flood of Lake Bonneville, another example of a lake overflow event in North America, as the rocks at Lake Alamosa were more solid and there is no clear indication of a catastrophic overflow flood.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
Creeks cut into the lake floor, forming valleys that later filled with alluvium. The Alamosa Formation, a geological formation, fills the basin of Lake Alamosa; it represents the deep water deposits of Lake Alamosa. Impermeable deposits of the lake such as the &quot;blue clay&quot; generate groundwater accumulations that are exploited for irrigation purposes.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
The Alamosa Formation, a geological formation, fills the basin of Lake Alamosa; it represents the deep water deposits of Lake Alamosa. Impermeable deposits of the lake such as the &quot;blue clay&quot; generate groundwater accumulations that are exploited for irrigation purposes. The Verdos Alluvium of the Denver Basin may correlate to certain deposits on the shores of Lake Alamosa.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
The Verdos Alluvium of the Denver Basin may correlate to certain deposits on the shores of Lake Alamosa. While it was formerly thought that the Great Sand Dunes were formed from sediments on the floor of Lake Alamosa but later research indicated that these sediments probably played an only minor role.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
While it was formerly thought that the Great Sand Dunes were formed from sediments on the floor of Lake Alamosa but later research indicated that these sediments probably played an only minor role. The development of the dunes however certainly post-dated the disappearance of Lake Alamosa as the lake would have impeded the transport of sand across the San Luis Valley. Research history.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
In the same year proof of the existence of the lake was found in well logs. Later, the geologist Ferdinand Vandeveer Hayden in 1875 wrote a more detailed account of the former lake, although he got some details wrong, and proposed the name &quot;Coronado's lakes&quot; for Lake Alamosa and another lake he believed to have existed in the Costilla Plain.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
It took almost a century after 1910 until a more detailed analysis of the deposits of the former lake - including identifying its former maximum elevation - was possible, however. Most information on the history of Lake Alamosa's water levels has been obtained at the &quot;Bachus pit&quot; gravel pit in Alamosa County, as elsewhere lake deposits have been altered.

Geographic entities mentioned:
surface_form: lake alamosa
instance_of: Lake
coordinates: lat: 37.2
lon: -105.41666666666667
His mother was an ardent Carlist, active in the female organization Margaritas. Aldaz later claimed that growing up a Traditionalist was a natural way of maturing for him, that since childhood he participated in annual rallies at Montejurra, Montserrat or Isuskiza, and that as a boy he knew many Carlist Navarrese personalities. One of them, Amadeo Marco Ilincheta, was his godfather.

Geographic entities mentioned:
surface_form: Montejurra
instance_of: Mountain
countries: Spain
coordinates: lat: 42.631111111111
lon: -2.0447222222222
The mountain is named for Remus, who along with his twin brother Romulus were the mythological founders of Ancient Rome. The name was officially adopted by the Geographical Names Board of Canada in 1940. Mount Remus' nearest higher peak is Mount Romulus, to the west-southwest. __NOTOC__
Geology. Mount Remus is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: Mount Romulus
instance_of: Mountain
countries: Canada
coordinates: lat: 50.78336
lon: -114.98531
surface_form: mount remus
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7944
lon: -114.9709
Mount Remus. Mount Remus is a mountain summit located in the Little Elbow River Valley of Kananaskis Country in the Canadian Rockies of Alberta, Canada. The mountain is named for Remus, who along with his twin brother Romulus were the mythological founders of Ancient Rome. The name was officially adopted by the Geographical Names Board of Canada in 1940.

Geographic entities mentioned:
surface_form: mount remus
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7944
lon: -114.9709
Mount Remus. Mount Remus is a mountain summit located in the Little Elbow River Valley of Kananaskis Country in the Canadian Rockies of Alberta, Canada. The mountain is named for Remus, who along with his twin brother Romulus were the mythological founders of Ancient Rome. The name was officially adopted by the Geographical Names Board of Canada in 1940.

Geographic entities mentioned:
surface_form: mount remus
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7944
lon: -114.9709
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Remus' nearest higher peak is Mount Romulus, to the west-southwest. __NOTOC__
Geology. Mount Remus is composed of sedimentary rock laid down during 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: mount remus
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7944
lon: -114.9709
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, Mount Remus is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mount remus
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7944
lon: -114.9709
Mount Remus. Mount Remus is a mountain summit located in the Little Elbow River Valley of Kananaskis Country in the Canadian Rockies of Alberta, Canada. The mountain is named for Remus, who along with his twin brother Romulus were the mythological founders of Ancient Rome. The name was officially adopted by the Geographical Names Board of Canada in 1940.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: twin
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
lon: -131.21166667
He joined 5th Reinforcements in 1941. He later served with 23 NZ Battalion in North Africa and Italy. He also took part in the battles of Monte Cassino. He was twice wounded. Batchelor's first DCM was awarded for gallantry, while in command of a forward platoon, during a fierce close quarter fight in a small house behind German lines at San Donato, on 21 July 1944, in the advance to Florence.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Legacy. Cowles Mountain was losing the name that honored George Cowles, becoming locally known as Black Mountain, a second one in the county; and/or 'S' Mountain, from the large white 'S' painted on its face for San Diego State University. However, the historically significant Cowles Mountain name has been used by Mission Trails Regional Park, which it has been within since 1974.

Geographic entities mentioned:
surface_form: Cowles Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.8128
lon: -117.032
Ustárroz. Ustárroz is a locality located in the municipality of Valle de Egüés, in Navarre province, Spain, Spain. As of 2020, it has a population of 13. Geography. Ustárroz is located 14km east of Pamplona.

Geographic entities mentioned:
surface_form: Valle de Egüés
instance_of: Valley
countries: Spain
coordinates: lat: 42.823722222222
lon: -1.5573611111111
The most important crop is cassava, while other important products are maize, onions, chili pepper and tomato. Industry and services provide both employment for 2% of the population. Boanamary is situated at 36 km South-East of Mahajanga in the estuary of the Betsiboka River. Larger surfaces of the municipality are covered by mangroves on which natural silk is won.

Geographic entities mentioned:
surface_form: Betsiboka River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -18.35868
lon: 47.485374
Geography. Val de Bagnes is traversed by the Drance de Bagnes. In the upper part of the valley is the Lac de Mauvoisin and towards the southern end of the valley the Glacier de Fenêtre and the Chanrion Hut. From Val de Bagnes, the Aosta Valley can be reached via the Fenêtre de Durand in the Grand Combin. At Sembrancher, the Val de Bagnes flows into the Val d’Entremont. Tourism.

Geographic entities mentioned:
surface_form: grand combin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.9375
lon: 7.2991666666667
surface_form: val de bagnes
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.05
lon: 7.267
Val de Bagnes. Val de Bagnes, also called the Vallée de Bagnes (German: Bangital or Baniental) is a valley located in the Entremont District in the Canton of Valais of Switzerland. Geography. Val de Bagnes is traversed by the Drance de Bagnes. In the upper part of the valley is the Lac de Mauvoisin and towards the southern end of the valley the Glacier de Fenêtre and the Chanrion Hut.

Geographic entities mentioned:
surface_form: val de bagnes
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.05
lon: 7.267
In the upper part of the valley is the Lac de Mauvoisin and towards the southern end of the valley the Glacier de Fenêtre and the Chanrion Hut. From Val de Bagnes, the Aosta Valley can be reached via the Fenêtre de Durand in the Grand Combin. At Sembrancher, the Val de Bagnes flows into the Val d’Entremont. Tourism. Tourism emerged in Val de Bagnes at the end of the 19th century.

Geographic entities mentioned:
surface_form: val de bagnes
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.05
lon: 7.267
At Sembrancher, the Val de Bagnes flows into the Val d’Entremont. Tourism. Tourism emerged in Val de Bagnes at the end of the 19th century. Numerous infrastructure projects have been carried out for tourism; the Médran chairlift was built in 1950 (winter tourism); Summer tourism began in Fionnay as early as 1890, then also in Bruson and Verbier.

Geographic entities mentioned:
surface_form: val de bagnes
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.05
lon: 7.267
Mynydd Moel. Mynydd Moel is the second highest summit of Cadair Idris in the Snowdonia National Park, in Gwynedd, northwest Wales. Geography. It lies to the east of Cadair Idris and is often climbed as a horseshoe along with Craig Cwm Amarch and Cadair Idris. The summit is bare and rocky and marked with a cairn. The north face like Cadair Idris has large cliffs.

Geographic entities mentioned:
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
surface_form: mynydd moel
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.705782
lon: -3.884874
Mynydd Moel. Mynydd Moel is the second highest summit of Cadair Idris in the Snowdonia National Park, in Gwynedd, northwest Wales. Geography. It lies to the east of Cadair Idris and is often climbed as a horseshoe along with Craig Cwm Amarch and Cadair Idris. The summit is bare and rocky and marked with a cairn. The north face like Cadair Idris has large cliffs.

Geographic entities mentioned:
surface_form: Craig Cwm Amarch
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.69117704828421
lon: -3.910197414956989
surface_form: cadair idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
surface_form: cadair idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
Geography. It lies to the east of Cadair Idris and is often climbed as a horseshoe along with Craig Cwm Amarch and Cadair Idris. The summit is bare and rocky and marked with a cairn. The north face like Cadair Idris has large cliffs. To the east is a lower broad plateau topped by the summit of Gau Graig.

Geographic entities mentioned:
surface_form: cadair idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
Mynydd Moel. Mynydd Moel is the second highest summit of Cadair Idris in the Snowdonia National Park, in Gwynedd, northwest Wales. Geography. It lies to the east of Cadair Idris and is often climbed as a horseshoe along with Craig Cwm Amarch and Cadair Idris. The summit is bare and rocky and marked with a cairn. The north face like Cadair Idris has large cliffs.

Geographic entities mentioned:
surface_form: mynydd moel
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.705782
lon: -3.884874
Geography. Joseph Canyon contains Joseph Creek, a tributary of the Grande Ronde River, which flows into the Snake River, a tributary of the Columbia. The geology is typical of the Columbia Plateau, formed by the Columbia River Basalt Group, and the exposed canyon walls provide a striking view of flood basalt flows and dikes. The canyon floor contains sediments deposited by the Missoula Floods.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889