Sarmila/GeoWiki-Features huggingface dataset:
There are three major UNESCO World Culture and Natural Heritage Sites in the ecoregion – the Golden Mountains of Altai, consisting of the Altai and Katun Natural Reserves, Lake Teletskoye, Belukha Mountain, and the Ukok Plateau; Lake Baikal, which forms part of the eastern border of the region, and Uvs Nuur Basin in the Great Lakes Hollow.

Geographic entities mentioned:
surface_form: Lake Teletskoye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 51.529166666667
lon: 87.714722222222
surface_form: Belukha Mountain
instance_of: Mountain
countries: Russia
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 49.806944444444
lon: 86.589722222222
surface_form: Ukok Plateau
instance_of: Plateau
countries: Russia
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 49.3077
lon: 87.5947
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
In May 1885, Fort Pitt was once again visited by Wandering Spirit and Big Bear's Cree. By this time, the Cree Camp had grown to an estimated 300 men, 700 women and children, as well as containing hostages, dogs, and horses. The Cree once again took the resources form the fort, this time departing to Frenchman Butte. Upon the departure the Cree set fire to many of the buildings at Fort Pitt.

Geographic entities mentioned:
surface_form: Frenchman Butte
instance_of: Mountain
countries: Canada
coordinates: lat: 53.6272
lon: -109.576
Rogen moraine. A Rogen moraine, also called ribbed moraine'&quot;, is a subglacially (&quot;i.e.&quot; under a glacier or ice sheet) formed type of moraine landform, that mainly occurs in Fennoscandia, Scotland, Ireland and Canada. It is one of the three main types of hummocky moraines.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Lauvdal. Lauvdal is a village in the municipality of Bygland in Agder county, Norway. It's located along the Norwegian National Road 9 on the east side of Byglandsfjorden. The village lies about south of the village of Bygland and about the same distance north of the village of Longerak. The population (2001) was 41 residents. The lake Longerakvatnet is located about southeast of the village.

Geographic entities mentioned:
surface_form: Byglandsfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.708333333333
lon: 7.8069444444444
Alperschällihorn. Alperschällihorn is a mountain of the Lepontine Alps, overlooking Splügen in the canton of Graubünden. The mountains is situated between the Safien valley (north) and the Hinterrhein valley (south).

Geographic entities mentioned:
surface_form: Safien valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.696666666667
lon: 9.3244444444444
Alperschällihorn. Alperschällihorn is a mountain of the Lepontine Alps, overlooking Splügen in the canton of Graubünden. The mountains is situated between the Safien valley (north) and the Hinterrhein valley (south).

Geographic entities mentioned:
surface_form: alperschällihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.586944444444
lon: 9.3072222222222
The medieval Lords of the manor took &quot;de Stavelegh&quot; as their name, later becoming &quot;Stayley&quot; or &quot;Staley&quot;. The lordship of Longdendale was one of the ancient feudal estates of Cheshire and included the area of Stalybridge. Buckton Castle, near Stalybridge, was probably built by one of the earls of Chester in the 12th century.

Geographic entities mentioned:
surface_form: Longdendale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.471666666666664
lon: -1.9505555555555554
Mottram Road and Huddersfield Road, Millbrook were flooded by water from a stream leading from the Walkerwood Reservoir. In late June 2018, many properties in Stalybridge were threatened by a large wildfire advancing from Saddleworth Moor. 50 properties in the Carrbrook area of Stalybridge were evacuated on 26 June as the wildfire advanced towards them.

Geographic entities mentioned:
surface_form: Saddleworth Moor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.543333333333
lon: -1.9558333333333
Environment. Much of the upland areas of the town are grouse moors. Boar Flat is part of the Dark Peak Site of Special Scientific Interest, as classified by Natural England. The slopes below the moors, particularly beneath Harridge Pike, are used for sheep grazing by the hill farms. The Stalybridge Country Park centres on two areas.

Geographic entities mentioned:
surface_form: Dark Peak
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 53.4
lon: -1.8
Firstly, the Brushes Valley, with its four reservoirs running up into the Pennine Moors, and secondly Carrbrook, lying in the shadow of Buckton Castle. Linking the two areas, although outside the country park boundaries, is a good rights of way network, and areas of designated access land which take visitors into the Tame Valley, Longdendale and the Peak District.

Geographic entities mentioned:
surface_form: Longdendale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.471666666666664
lon: -1.9505555555555554
Linking the two areas, although outside the country park boundaries, is a good rights of way network, and areas of designated access land which take visitors into the Tame Valley, Longdendale and the Peak District. The country park affords views of the Cheshire Plain, Jodrell Bank and on very clear days the mountains of Snowdonia.

Geographic entities mentioned:
surface_form: Cheshire Plain
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2
lon: -2.4666666666667
Warner Valley. The Warner Valley is a valley in south-central Oregon in the United States. It is a remote valley at the northwestern corner of North America's Basin and Range Province. The valley is home to a chain of lakes and wetlands known as the Warner Lakes. Native Americans were present in the Warner Valley for thousands of years before European explorers arrived in the 19th century.

Geographic entities mentioned:
surface_form: Warner Lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Coyote Hills are the western boundary through the middle of the North Warner Valley, with the Rabbit Hills bounding the northwest corner of the valley. From the hills, the ground slopes up to the crest of Abert Rim. The eastern boundary of the valley is Hart Mountain, a massive cliff face that rises above the valley floor. Warner Peak is the highest point on Hart Mountain.

Geographic entities mentioned:
surface_form: Hart Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.4597
lon: -119.741
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The eastern cliffs run the entire length of the valley, while the western wall turns into rolling hills at the north end of the valley. The Coyote Hills are the western boundary through the middle of the North Warner Valley, with the Rabbit Hills bounding the northwest corner of the valley. From the hills, the ground slopes up to the crest of Abert Rim.

Geographic entities mentioned:
surface_form: coyote hills
instance_of: Landform
countries: United States
coordinates: lat: 44.9207
lon: -117.901
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Starting at the south end of the valley, the largest of the Warner Lakes are Pelican Lake, Crump Lake, Hart Lake, Anderson Lake, Swamp Lake, Mugwump Lake, Flagstaff Lake, Upper Campbell Lake, Lower Campbell Lake, Stone Corral Lake, Turpin Lake, and Bluejoint Lake. Because the valley slopes away to the north, Crump Lake is higher in elevation than Bluejoint Lake. Geology.

Geographic entities mentioned:
surface_form: anderson lake
instance_of: Lake
countries: United States
coordinates: lat: 47.7892
lon: -90.8028
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.57611111
lon: -94.17611111
surface_form: crump lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2946
lon: -119.8252
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5041
lon: -89.2035
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 37.95017
lon: -122.77537
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.6985
lon: -96.0198
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0611
lon: -92.9
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
surface_form: anderson lake
instance_of: Lake
countries: United States
coordinates: lat: 45.278567
lon: -97.252895
surface_form: anderson lake
instance_of: Lake
countries: United States
coordinates: lat: 48.0188527
lon: -122.8012455
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: anderson lake
instance_of: Lake
countries: United States
coordinates: lat: 40.1997
lon: -90.1847
surface_form: warner lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 46.05777778
lon: -95.80222222
surface_form: pelican lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0925246
lon: -96.9136823
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: flagstaff lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5825
lon: -119.80027777778
surface_form: anderson lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6017
lon: -121.484
surface_form: campbell lake
instance_of: Lake
countries: United States
coordinates: lat: 44.93861111
lon: -94.0125
surface_form: campbell lake
instance_of: Lake
countries: United States
coordinates: lat: 44.93861111
lon: -94.0125
surface_form: campbell lake
instance_of: Lake
countries: United States
coordinates: lat: 61.1324772
lon: -149.9413973
surface_form: campbell lake
instance_of: Lake
countries: United States
coordinates: lat: 61.1324772
lon: -149.9413973
The valley has two regions commonly referred to as the South Warner Valley and the North Warner Valley. The two areas transition between Crump Lake and Hart Lake at a point where the valley narrows to about in width. Both sides of the South Warner Valley have steep cliffs rising from above the valley floor.

Geographic entities mentioned:
surface_form: crump lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2946
lon: -119.8252
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Starting at the south end of the valley, the largest of the Warner Lakes are Pelican Lake, Crump Lake, Hart Lake, Anderson Lake, Swamp Lake, Mugwump Lake, Flagstaff Lake, Upper Campbell Lake, Lower Campbell Lake, Stone Corral Lake, Turpin Lake, and Bluejoint Lake. Because the valley slopes away to the north, Crump Lake is higher in elevation than Bluejoint Lake. Geology.

Geographic entities mentioned:
surface_form: crump lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2946
lon: -119.8252
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
There are 239 species of birds that live in the area or migrate through the Warner Valley. Species that nest in the areas around Crump Lake and Hart Lake include American white pelicans, double-crested cormorants, willets, Wilson's phalaropes, Canada geese, gadwalls, northern shovelers, black-crowned night herons, and numerous varieties of ducks and terns.

Geographic entities mentioned:
surface_form: crump lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2946
lon: -119.8252
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
In February 1867, General George Crook visited the Warner Valley outpost. Crook directed that the camp be moved to the Honey Creek site west of the lakes. To get the Army’s wagons across the wetlands, Crook ordered the construction of a bridge across the narrow channel between Hart Lake and Crump Lake. Shortly after the bridge was begun a second detachment was sent ahead to build the new fort.

Geographic entities mentioned:
surface_form: crump lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2946
lon: -119.8252
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 47.289722222222
lon: -94.752777777778
surface_form: hart lake
instance_of: Lake
countries: United States
coordinates: lat: 45.27444444
lon: -96.08694444
Warner Valley. The Warner Valley is a valley in south-central Oregon in the United States. It is a remote valley at the northwestern corner of North America's Basin and Range Province. The valley is home to a chain of lakes and wetlands known as the Warner Lakes. Native Americans were present in the Warner Valley for thousands of years before European explorers arrived in the 19th century.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
It is a remote valley at the northwestern corner of North America's Basin and Range Province. The valley is home to a chain of lakes and wetlands known as the Warner Lakes. Native Americans were present in the Warner Valley for thousands of years before European explorers arrived in the 19th century. It is the site of Fort Warner, built by the United States Army in 1867.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
The fort was used as a supply depot and administrative headquarters during a protracted Army campaign against Northern Paiute bands in eastern Oregon and northern California. Today, livestock ranching is the main commercial activity in the valley. The Warner Valley offers a number of recreational opportunities including hunting, fishing, bird watching, and wildlife viewing. Geography.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
The Warner Valley offers a number of recreational opportunities including hunting, fishing, bird watching, and wildlife viewing. Geography. The Warner Valley is located in south-central Oregon. It is approximately long and wide. Most of the valley is in Lake County; however, the north end of the valley extends about into Harney County.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
It is approximately long and wide. Most of the valley is in Lake County; however, the north end of the valley extends about into Harney County. The valley has two regions commonly referred to as the South Warner Valley and the North Warner Valley. The two areas transition between Crump Lake and Hart Lake at a point where the valley narrows to about in width.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The two areas transition between Crump Lake and Hart Lake at a point where the valley narrows to about in width. Both sides of the South Warner Valley have steep cliffs rising from above the valley floor. The eastern cliffs run the entire length of the valley, while the western wall turns into rolling hills at the north end of the valley.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Because the valley slopes away to the north, Crump Lake is higher in elevation than Bluejoint Lake. Geology. The country to the north and east of the Warner Valley is a high volcanic plateau which has undergone considerable erosion. The Warner Valley was probably a similar high plateau before massive faulting dropped the valley floor and uplifted the land around it, forming high valley walls.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
Geology. The country to the north and east of the Warner Valley is a high volcanic plateau which has undergone considerable erosion. The Warner Valley was probably a similar high plateau before massive faulting dropped the valley floor and uplifted the land around it, forming high valley walls. The Warner Lakes formed in the valley bottom after the faulting stopped.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Warner Lakes formed in the valley bottom after the faulting stopped. The Warner Valley is bounded by high escarpment walls on the east and west. The main line of perpendicular displacement is along the foot of the cliffs to the east of the Warner Lakes. This scarp feature is known as Hart Mountain. The main cliff face of Hart Mountain towers above the valley floor.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
These cliffs expose hundreds of feet of Miocene and Oligocene lava flows and ignimbrites, which include Steens basalt and various andesite, trachyandesite, and tuff flows. The mountain mass forming the western border of the South Warner Valley is a steep fault scarp. This cliff face rises over above the valley floor.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
The mountain mass forming the western border of the South Warner Valley is a steep fault scarp. This cliff face rises over above the valley floor. Warner Valley is an alluvial basin containing numerous lakes, remnants of a single great lake that covered the valley floor up to a depth of during the Pleistocene epoch. Today, steep cliffs rise above a chain of endorheic lakes. Climate.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Today, steep cliffs rise above a chain of endorheic lakes. Climate. The climate in the Warner Valley is typical of the high desert country of south-central Oregon. However, the high escarpments forming the western wall of the South Warner Valley tend to protect the southern part of the valley from the prevailing westerly winds.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
Today, steep cliffs rise above a chain of endorheic lakes. Climate. The climate in the Warner Valley is typical of the high desert country of south-central Oregon. However, the high escarpments forming the western wall of the South Warner Valley tend to protect the southern part of the valley from the prevailing westerly winds.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
However, the high escarpments forming the western wall of the South Warner Valley tend to protect the southern part of the valley from the prevailing westerly winds. The absence of a high rim along much of the North Warner Valley increases the harshness of the fall and winter seasons at the north end of the valley.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
These winds are strongest at places where canyons, such as Deep Creek Canyon, open into the valley. In the Warner Valley, frost is common until late spring and begins again in early fall. As a result, the growing season in the valley is limited to about 100 days. The Warner Valley gets most of its rain in May and June, while the summer and fall months tend to be very dry.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
In the Warner Valley, frost is common until late spring and begins again in early fall. As a result, the growing season in the valley is limited to about 100 days. The Warner Valley gets most of its rain in May and June, while the summer and fall months tend to be very dry. The winter snowfall in the valley bottom is generally very light; however, winter temperatures can get very cold.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
This snowpack feeds the streams that drain into the valley. Ecology. The Warner Valley provides a number of unique animal habitats. These include lake, marsh, riparian, grasslands, sage steppe, dry forest, and rimrock. They range in elevation from approximately above sea level at the valley floor to over at the summit of Warner Peak. Marsh grasses are common along the lake shores.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
In the riparian areas, wild roses, choke cherry, wild plum, cottonwood, and willow are found. Beyond the wetlands, the valley becomes quite dry. Much of the North Warner Valley is semi-desert, where dwarf sagebrush, greasewood, and Western Juniper are the dominant vegetation. The valley’s wildlife includes common high desert mammal species, resident birds, and migrant waterfowl.

Geographic entities mentioned:
surface_form: warner valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
The valley’s wildlife includes common high desert mammal species, resident birds, and migrant waterfowl. There are forty-two mammal species that live in the Warner Valley-Hart Mountain area. These include pronghorn, bighorn sheep, elk, mule deer, cougar, bobcat, and coyotes. Smaller mammals include jackrabbits, ground squirrels, and chipmunks.

Geographic entities mentioned:
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There are forty-two mammal species that live in the Warner Valley-Hart Mountain area. These include pronghorn, bighorn sheep, elk, mule deer, cougar, bobcat, and coyotes. Smaller mammals include jackrabbits, ground squirrels, and chipmunks. There are 239 species of birds that live in the area or migrate through the Warner Valley.

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The larger birds include great horned owls, long-eared owls, prairie falcons, golden eagles, and bald eagles. History. Native Americans used the Warner Valley for thousands of years before the first Europeans arrived. The valley has scores of petroglyphs, some estimated to be 12,000 years old.

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The valley has scores of petroglyphs, some estimated to be 12,000 years old. The Greaser Petroglyph Site, in the South Warner Valley, is listed on the National Register of Historic Places. The first European explorer to enter the valley was probably John Work, who headed a Hudson's Bay Company trapping expedition in 1832.

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The first European explorer to enter the valley was probably John Work, who headed a Hudson's Bay Company trapping expedition in 1832. While it is not certain that he visited the valley, he was in the area and left a description of a &quot;valley of lakes&quot; that correspond closely to the Warner Valley. The next explorer to arrive in the valley was Captain John C.

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Fremont, who led a party through the valley in December 1843. Fremont named it Christmas Valley since his party spent Christmas Day camped near Hart Lake. However, early mapmakers mistakenly sited Christmas Valley at another location northwest of the Warner Valley, leaving the valley unnamed on an early map. In 1849, the valley was explored by Captain William H.

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However, early mapmakers mistakenly sited Christmas Valley at another location northwest of the Warner Valley, leaving the valley unnamed on an early map. In 1849, the valley was explored by Captain William H. Warner, an Army topographical engineer. On 26 September 1849, Warner was ambushed and killed by Indians just south of the Warner Valley. In 1864, Lieutenant Colonel C. S.

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Drew named the valley in honor of Warner, who he believed had been killed there. In 1865, the Army decided it needed a fort in the Warner Valley to facilitate the interdiction of Indian raiding parties passing through the area. Army scouts selected a site along Honey Creek on the west side of the Warner Lakes. In 1866, a detachment from Fort Boise was sent to establish the fort.

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The soldiers arrived on the east side of the lakes in late summer. Unable to cross the chain of lakes and marshes, the soldiers built a winter camp on the east side of the lakes. The camp was sited poorly and the men had a very difficult winter. In February 1867, General George Crook visited the Warner Valley outpost. Crook directed that the camp be moved to the Honey Creek site west of the lakes.

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As a result, road surveyors laid out a route designed to pass through as much well-watered, desirable land as possible. The route of the military road came through the Warner Valley, crossing over the Warner Lakes at the Stone Bridge before passing south of Hart Mountain through what is today the Hart Mountain National Antelope Refuge and heading east.

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In reality, the Oregon Central Military Wagon Road was a venture designed to acquire public lands at little or no cost to the road company’s investors. Nevertheless, the construction company was able to secure thousands of acres of valuable grazing land in the Warner Valley.

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Its first postmaster was David R. Jones. The Adel post office was opened in 1896. Human activity. Today, agriculture is the primary source of income in the Warner Valley. Most of the private land in the valley is used for cattle ranching. Crops are generally used for winter feed. Because of the short growing season, the valley’s principal crops are wild hay, alfalfa, clover, and timothy-grass.

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Because of the short growing season, the valley’s principal crops are wild hay, alfalfa, clover, and timothy-grass. Grains such as wheat, oats, rye, and barley can also be grown in the Warner Valley. Three crops of alfalfa per season can be raised over much of the South Warner Valley, while the less favorable climate in the North Warner Valley makes one or two crops the norm.

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Grains such as wheat, oats, rye, and barley can also be grown in the Warner Valley. Three crops of alfalfa per season can be raised over much of the South Warner Valley, while the less favorable climate in the North Warner Valley makes one or two crops the norm. Much of the valley is public land administered by the Bureau of Land Management.

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The next explorer to arrive in the valley was Captain John C. Fremont, who led a party through the valley in December 1843. Fremont named it Christmas Valley since his party spent Christmas Day camped near Hart Lake. However, early mapmakers mistakenly sited Christmas Valley at another location northwest of the Warner Valley, leaving the valley unnamed on an early map.

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Air movements brought about by the uneven temperatures in the valley and on the surrounding higher plateaus and mountains give rise to local winds. These winds are strongest at places where canyons, such as Deep Creek Canyon, open into the valley. In the Warner Valley, frost is common until late spring and begins again in early fall.

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However, some of these activities are dependent on the water level of the Warner Lakes, which can fluctuate dramatically. Crappie, smallmouth bass, and bullhead catfish are common in the lakes while trout including Great Basin redband trout are found in Twentymile Creek, Deep Creek, and Honey Creek.

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From the hills, the ground slopes up to the crest of Abert Rim. The eastern boundary of the valley is Hart Mountain, a massive cliff face that rises above the valley floor. Warner Peak is the highest point on Hart Mountain. The summit is above sea level. The valley floor is occupied by a chain of lakes known collectively as the Warner Lakes.

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The Warner Lakes formed in the valley bottom after the faulting stopped. The Warner Valley is bounded by high escarpment walls on the east and west. The main line of perpendicular displacement is along the foot of the cliffs to the east of the Warner Lakes. This scarp feature is known as Hart Mountain. The main cliff face of Hart Mountain towers above the valley floor.

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The main line of perpendicular displacement is along the foot of the cliffs to the east of the Warner Lakes. This scarp feature is known as Hart Mountain. The main cliff face of Hart Mountain towers above the valley floor. It runs the length of the valley, eventually being lost in a series of smaller fault scarps at the north end of the valley.

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The fort was used as a supply depot and administrative headquarters during a protracted Army campaign against Northern Paiute bands in eastern Oregon and northern California. Today, livestock ranching is the main commercial activity in the valley. The Warner Valley offers a number of recreational opportunities including hunting, fishing, bird watching, and wildlife viewing. Geography.

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Geography. The Warner Valley is located in south-central Oregon. It is approximately long and wide. Most of the valley is in Lake County; however, the north end of the valley extends about into Harney County. The valley has two regions commonly referred to as the South Warner Valley and the North Warner Valley.

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Both sides of the South Warner Valley have steep cliffs rising from above the valley floor. The eastern cliffs run the entire length of the valley, while the western wall turns into rolling hills at the north end of the valley. The Coyote Hills are the western boundary through the middle of the North Warner Valley, with the Rabbit Hills bounding the northwest corner of the valley.

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Warner Peak is the highest point on Hart Mountain. The summit is above sea level. The valley floor is occupied by a chain of lakes known collectively as the Warner Lakes. The entire valley was once covered by a single vast lake; however, the water level gradually receded, leaving a chain of lakes at the low spots with marshland between the lakes.

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The Warner Valley was probably a similar high plateau before massive faulting dropped the valley floor and uplifted the land around it, forming high valley walls. The Warner Lakes formed in the valley bottom after the faulting stopped. The Warner Valley is bounded by high escarpment walls on the east and west.

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This scarp feature is known as Hart Mountain. The main cliff face of Hart Mountain towers above the valley floor. It runs the length of the valley, eventually being lost in a series of smaller fault scarps at the north end of the valley. These smaller scarps generally run from the east side of the valley to the northwest. The south end of the valley is more complex.

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This scarp feature is known as Hart Mountain. The main cliff face of Hart Mountain towers above the valley floor. It runs the length of the valley, eventually being lost in a series of smaller fault scarps at the north end of the valley. These smaller scarps generally run from the east side of the valley to the northwest. The south end of the valley is more complex.

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It runs the length of the valley, eventually being lost in a series of smaller fault scarps at the north end of the valley. These smaller scarps generally run from the east side of the valley to the northwest. The south end of the valley is more complex. In that area, the valley floor is bounded on three sides by perpendicular cliffs from high, the result of numerous fault events.

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The south end of the valley is more complex. In that area, the valley floor is bounded on three sides by perpendicular cliffs from high, the result of numerous fault events. These cliffs expose hundreds of feet of Miocene and Oligocene lava flows and ignimbrites, which include Steens basalt and various andesite, trachyandesite, and tuff flows.

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The mountain mass forming the western border of the South Warner Valley is a steep fault scarp. This cliff face rises over above the valley floor. Warner Valley is an alluvial basin containing numerous lakes, remnants of a single great lake that covered the valley floor up to a depth of during the Pleistocene epoch. Today, steep cliffs rise above a chain of endorheic lakes. Climate.

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The absence of a high rim along much of the North Warner Valley increases the harshness of the fall and winter seasons at the north end of the valley. Air movements brought about by the uneven temperatures in the valley and on the surrounding higher plateaus and mountains give rise to local winds. These winds are strongest at places where canyons, such as Deep Creek Canyon, open into the valley.

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