Sarmila/GeoWiki-Features huggingface dataset:
In addition, degraded parts of the Threemile Creek habitat include Threemile Reservoir. Early history. Native Americans used the Catlow Valley for thousands of years before the first European explorers arrived. The valley has a number of petroglyph sites. Some of these petroglyphs may be up to 12,000 years old. When he first excavated Catlow Cave in 1934, archaeologist Luther S.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 34.155833333333334
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19th century. The first European explorer to enter the valley may have been John Work, who headed a Hudson's Bay Company trapping expedition that explored the area in 1831. While it is not certain that he visited the Catlow Valley, Work is known to have passed through the Steens Mountain area as well as the neighboring Warner Valley, west of Hart Mountain. In 1864, Lieutenant Colonel Charles S.

Geographic entities mentioned:
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countries: United States
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However, the road was little more than a trail, and it was rarely used. Cattle ranchers began using the Catlow Valley in the latter part of the 19th century. The first to arrive was Peter French in 1872, locating one of his five ranches in the valley. Another cattle rancher, John Catlow, followed in 1874. Catlow never owned land in the valley, but he grazed cattle there in the mid-1870s.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
coordinates: lat: 61.3833
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countries: United States
coordinates: lat: 47.7174
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The first to arrive was Peter French in 1872, locating one of his five ranches in the valley. Another cattle rancher, John Catlow, followed in 1874. Catlow never owned land in the valley, but he grazed cattle there in the mid-1870s. David Shirk, one of Catlow's foremen, named the valley after his boss. Shirk was soon joined by his brother, William.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
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coordinates: lat: 47.7174
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Another cattle rancher, John Catlow, followed in 1874. Catlow never owned land in the valley, but he grazed cattle there in the mid-1870s. David Shirk, one of Catlow's foremen, named the valley after his boss. Shirk was soon joined by his brother, William. In 1876, the two Shirk brothers established a ranch in the Catlow Valley, near water sources around Home and Threemile creeks.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
coordinates: lat: 61.3833
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countries: United States
coordinates: lat: 47.7174
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20th century. In the early 1900s, a surge of dry-land farmers arrived in the Catlow Valley. They were drawn by the prospect of free land offered by the federal government's Homestead Act. People's interest in the area was increased by newspaper articles promising that a railroad would soon be built through the valley. By 1916, there were over 700 settlers living in the Catlow Valley.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
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coordinates: lat: 47.7174
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People's interest in the area was increased by newspaper articles promising that a railroad would soon be built through the valley. By 1916, there were over 700 settlers living in the Catlow Valley. To support these settlers, small unincorporated communities were established across the valley. These sites included Beckley, Delaine, Catlow, Berdugeo, Sageview, Tiara, and Blitzen.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 34.155833333333334
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The Catlow post office was opened in 1914 and remained open until 1923. The Berdugo post office was opened near the Roaring Springs Ranch in 1915. It closed two years later. Sageview was located on the west side of the valley. A post office was the only building at the site. The post office was opened in 1916 and closed in 1918. The Tiara post office was open from May 1916 to January 1917.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 34.155833333333334
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Human activity. Today, there are no incorporated towns or unincorporated communities in the Catlow Valley, but only a few scattered ranches. Agriculture is the primary source of income for those living in the valley. Much of the private land in the valley is used to grow winter feed for local cattle herds.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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Today, there are no incorporated towns or unincorporated communities in the Catlow Valley, but only a few scattered ranches. Agriculture is the primary source of income for those living in the valley. Much of the private land in the valley is used to grow winter feed for local cattle herds. Wells provide groundwater for large irrigation circles and pipe irrigation systems in the valley.

Geographic entities mentioned:
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
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surface_form: the valley
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countries: United States
coordinates: lat: 47.7174
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Agriculture is the primary source of income for those living in the valley. Much of the private land in the valley is used to grow winter feed for local cattle herds. Wells provide groundwater for large irrigation circles and pipe irrigation systems in the valley. Because of the short growing season, the valley's principal crops are wild hay and alfalfa.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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coordinates: lat: 47.7174
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Much of the private land in the valley is used to grow winter feed for local cattle herds. Wells provide groundwater for large irrigation circles and pipe irrigation systems in the valley. Because of the short growing season, the valley's principal crops are wild hay and alfalfa. The largest ranch in the Catlow Valley is the Roaring Springs Ranch.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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Among the most popular game animals for hunters are mule deer, pronghorn, and chukars. Several of the canyon streams that flow into the valley offer the opportunity for trout fishing. There are no developed campgrounds in the valley; however, dispersed camping is allowed on land administered by the BLM. The availability of potable water is a limiting factor for both day-use visitors and campers.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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The availability of potable water is a limiting factor for both day-use visitors and campers. High Desert Discovery Scenic Byway. The nearest town to the Catlow Valley is Burns, Oregon, the county seat of Harney County. Burns is approximately north of the valley. To reach the Catlow Valley from Burns, follow the High Desert Discovery Scenic Byway south. The drive takes several hours.

Geographic entities mentioned:
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countries: United States
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It follows Catlow Rim approximately before turning east towards Fields, located on the far side of Steens Mountain. The High Desert Discovery Scenic Byway ends at Fields. The main east–west road through the Catlow Valley is a rough gravel road that connects to Route 205 at the north end of the valley. It is not part of the High Desert Discovery Scenic Byway.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
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The Catlow Valley is bounded by Hart Mountain on the west and Steens Mountain on the east, and Beatys Butte is southwest of the valley. Warner Peak is the highest point on Hart Mountain. The summit of Warner Peak is above sea level. From the crest of the Hart Mountain, the land slopes gently down to the floor of the valley. Steens Mountain's western boundary is Catlow Rim.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 42.459722222222
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This road is not passable year-round; therefore, travelers should contact the local Bureau of Land Management office in Burns or the Hart Mountain National Antelope Refuge headquarters before taking it. There is no gas available along the road until the traveler reaches Plush, west the refuge headquarters. Plush is east of Lakeview.

Geographic entities mentioned:
surface_form: the traveler
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countries: United States
coordinates: lat: 46.0728
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Catlow Valley. The Catlow Valley is a basin in Harney County, Oregon, United States. It is a remote valley at the northwestern corner of North America's Basin and Range Province. The valley is named after a pioneer rancher, John Catlow. The area was used by Native Americans for thousands of years before European explorers arrived in the 19th century.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
Today, cattle ranching is the main commercial activity in the valley. The public land in the Catlow Valley is administered by the Bureau of Land Management. This public land offers a number of recreational opportunities including hiking, hunting, fishing, bird watching, and wildlife viewing. Geography. Catlow Valley is located in Harney County in southeastern Oregon.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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This public land offers a number of recreational opportunities including hiking, hunting, fishing, bird watching, and wildlife viewing. Geography. Catlow Valley is located in Harney County in southeastern Oregon. The area is the northwestern corner of North America's continental basin and range country. The valley is approximately long and wide. It covers approximately of high desert range land.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
The summit of Warner Peak is above sea level. From the crest of the Hart Mountain, the land slopes gently down to the floor of the valley. Steens Mountain's western boundary is Catlow Rim. The rim runs along the east side of Catlow Valley from north to south. At the north end of the valley, the rim begins as gentle rolling hills. The rim gets steeper and high as it runs south.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
At the north end of the valley, the rim begins as gentle rolling hills. The rim gets steeper and high as it runs south. At the south end of the valley, Catlow Rim has a cliff face that rises more than a above the valley floor. Beatys Butte is a stand-alone peak southwest of Catlow Valley. Its summit is above sea level, which gives it a prominence above the valley floor. Geology.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
Its summit is above sea level, which gives it a prominence above the valley floor. Geology. The Catlow Valley is a tectonic depression called a graben. It is bounded on the east and west by high, uplifted fault-block mountains—Hart Mountain to the west and Steens Mountain to the east—with which it forms a horst and graben geological feature.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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The cave is wide at its mouth. It is high and deep. Roaring Springs Cave is another prominent cave located at the base of Catlow Rim. During the Pleistocene Epoch, the Catlow Valley was covered by a single large lake, approximately by length and width. In some spots, the lake was over deep. Today, the valley is a high-desert alluvial basin.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
However, evidence of the ancient lake can still be seen in the form of shoreline erosion marks, gravel bars, and wave-cut terraces around the edge of the valley, especially along the base of Catlow Rim. Climate. The climate in the Catlow Valley is typical of the high-desert country of southeastern Oregon. Summers in the valley are short, characterized by high temperatures and very little moisture.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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The valley gets an average of of precipitation per year, mostly as snowfall. The winters are cold. There is no official weather reporting station in the Catlow Valley. The P Ranch weather station is the nearest official National Oceanic and Atmospheric Administration (NOAA) reporting station to the valley. It is approximately northeast of the Catlow Valley in the neighboring Blitzen Valley.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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The P Ranch weather station is the nearest official National Oceanic and Atmospheric Administration (NOAA) reporting station to the valley. It is approximately northeast of the Catlow Valley in the neighboring Blitzen Valley. The elevation of the P Ranch weather station is above sea level, approximately lower than the average elevation of the Catlow Valley.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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It is approximately northeast of the Catlow Valley in the neighboring Blitzen Valley. The elevation of the P Ranch weather station is above sea level, approximately lower than the average elevation of the Catlow Valley. It reports daily weather data to NOAA's National Climatic Data Center. Flora. The Catlow Valley topography provides a number of wildlife habitats.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
It reports daily weather data to NOAA's National Climatic Data Center. Flora. The Catlow Valley topography provides a number of wildlife habitats. These include seasonal lakes, marshes, riparian areas, grasslands, sage steppe, dry juniper forests, and rimrock. The valley is predominantly high-desert grassland with gently rolling hills to the north, west, and south of the valley floor.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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In addition, greasewood, shadscale, spiny hopsage, winterfat, and basin wildrye can be found in parts of the valley. Fauna. The Catlow Valley's wildlife includes many high-desert animal species. Large mammals found in the valley include mule deer, pronghorn, bighorn sheep, coyotes, bobcats, and cougars. The valley is also home to a herd of wild horses.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
Among the common reptiles are Great Basin fence lizards, sagebrush lizards, desert horned lizards, western skinks, gopher snakes, and western rattlesnakes. In the sage steppes and grasslands of the Catlow Valley, resident birds include horned larks, Brewer's sparrows, vesper sparrows, sage thrashers, sagebrush sparrows, black-throated sparrows, common ravens, and greater sage grouse.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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The larger birds include great horned owls, long-eared owls, prairie falcons, American kestrels, red-tailed hawks, and golden eagles. All five of the year-round creeks that flow into the Catlow Valley (Rock Creek, Guano Creek, Home Creek, Skull Creek, and Threemile Creek) support fish populations. The native fish are tui chub, Lahontan cutthroat trout, and Great Basin redband trout.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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The redband populations in Guano, Skull, and Threemile creeks are limited. In addition, degraded parts of the Threemile Creek habitat include Threemile Reservoir. Early history. Native Americans used the Catlow Valley for thousands of years before the first European explorers arrived. The valley has a number of petroglyph sites. Some of these petroglyphs may be up to 12,000 years old.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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Cressman identified four rock fire pits and other housekeeping features within Catlow Cave. Later excavations found stone tools, baskets, woven mats, sandals, rope, and fragments of leather. The Skull Creek dunes are another archaeological site that provides evidence of early Native American habitation in the Catlow Valley. That site documents at least 8,000 years of occupation.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
The Skull Creek dunes are another archaeological site that provides evidence of early Native American habitation in the Catlow Valley. That site documents at least 8,000 years of occupation. Prior to the arrival of white settlers, the Catlow Valley area was occupied by the Northern Paiute people. 19th century.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 42.56349
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In 1864, Lieutenant Colonel Charles S. Drew of the 1st Oregon Cavalry passed just south of the Catlow Valley while on a long-range reconnaissance patrol for the United States Army. Drew named Beatys Butte in honor of Sergeant A. M. Beaty, one of the noncommissioned officers in his party.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 42.56349
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However, the road was little more than a trail, and it was rarely used. Cattle ranchers began using the Catlow Valley in the latter part of the 19th century. The first to arrive was Peter French in 1872, locating one of his five ranches in the valley. Another cattle rancher, John Catlow, followed in 1874. Catlow never owned land in the valley, but he grazed cattle there in the mid-1870s.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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While a jury decided it was self-defense, the Shirk brothers moved their main ranch to a location south of Beatys Butte to minimize future conflict with French and his employees. 20th century. In the early 1900s, a surge of dry-land farmers arrived in the Catlow Valley. They were drawn by the prospect of free land offered by the federal government's Homestead Act.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
They were drawn by the prospect of free land offered by the federal government's Homestead Act. People's interest in the area was increased by newspaper articles promising that a railroad would soon be built through the valley. By 1916, there were over 700 settlers living in the Catlow Valley. To support these settlers, small unincorporated communities were established across the valley.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
Sageview was located on the west side of the valley. A post office was the only building at the site. The post office was opened in 1916 and closed in 1918. The Tiara post office was open from May 1916 to January 1917. The largest and oldest community in the Catlow Valley was Blitzen. Its post office was opened in 1916. However, there were only three families left in Blitzen in 1924.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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Today, there is no evidence of habitation at any of these sites except at the ghost town of Blitzen, where there are still a few deteriorated buildings at the town site. Human activity. Today, there are no incorporated towns or unincorporated communities in the Catlow Valley, but only a few scattered ranches. Agriculture is the primary source of income for those living in the valley.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
Wells provide groundwater for large irrigation circles and pipe irrigation systems in the valley. Because of the short growing season, the valley's principal crops are wild hay and alfalfa. The largest ranch in the Catlow Valley is the Roaring Springs Ranch. It includes of deeded property plus grazing rights on an additional of public land.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
The ghost town of Blitzen is located on property owned by the ranch. In 2007, the Roaring Springs Ranch won the Environmental Stewardship Award sponsored by the National Cattlemen's Beef Association and the United States Department of Agriculture. All of the public land in the Catlow Valley is administered by the Bureau of Land Management (BLM).

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
The availability of potable water is a limiting factor for both day-use visitors and campers. High Desert Discovery Scenic Byway. The nearest town to the Catlow Valley is Burns, Oregon, the county seat of Harney County. Burns is approximately north of the valley. To reach the Catlow Valley from Burns, follow the High Desert Discovery Scenic Byway south. The drive takes several hours.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
High Desert Discovery Scenic Byway. The nearest town to the Catlow Valley is Burns, Oregon, the county seat of Harney County. Burns is approximately north of the valley. To reach the Catlow Valley from Burns, follow the High Desert Discovery Scenic Byway south. The drive takes several hours. From Burns, travel east on Oregon Route 78 for, then turn south on Oregon Route 205 toward Frenchglen.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
This highway crosses the Harney Basin, passing over &quot;The Narrows&quot; between Harney and Malheur lakes, and traverses the length of the Malheur National Wildlife Refuge to Frenchglen. Continue on Route 205 through the small unincorporated community of Frenchglen and over a low pass approximately into the northeast corner of the Catlow Valley.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
Continue on Route 205 through the small unincorporated community of Frenchglen and over a low pass approximately into the northeast corner of the Catlow Valley. Oregon Route 205 is the only paved road in the Catlow Valley. It follows Catlow Rim approximately before turning east towards Fields, located on the far side of Steens Mountain. The High Desert Discovery Scenic Byway ends at Fields.

Geographic entities mentioned:
surface_form: catlow valley
instance_of: Valley
countries: United States
coordinates: lat: 42.56349
lon: -119.05825
There is no gas available along the road until the traveler reaches Plush, west the refuge headquarters. Plush is east of Lakeview. Lakeview is the nearest incorporated city west of the Catlow Valley.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 42.56349
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He first experimented with this new medium during a trip to Switzerland in the autumn of 1908 where, working outdoors, he produced a radiant series of pastels exhibited in February of the following year at the Galerie Georges Petit in Paris.19 The French government immediately acquired &quot;Lac Léman&quot; (&quot;Lake Geneva&quot;), a majestic and iconic scene depicted in a number of different versions, all concentrating on the shimmering expanse of water.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Konstamonitou Monastery. The Kastamonitou Monastery (), officially called Konstamonitou Monastery (Μονή Κωνσταμονίτου), is an Orthodox Christian monastery in the monastic state of Mount Athos in Greece. It stands on the southeastern side of the Athos peninsula. The monastery ranks twentieth and last in the hierarchy of the Athonite monasteries.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
On April 23, 1945, Solaro was promoted to Regional Inspector of the Black Brigades, while Mario Pavia replaced him as federal secretary of the PFR. The collapse of the Italian Social Republic was however imminent, and the city's military leaders, headed by General Enrico Adami Rossi, decided to leave Turin and retreat towards the Valtellina, while Solaro tried in vain to persuade them to stay.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
Edgbaston Reserve. Edgbaston Reserve, formerly Edgbaston Station, is a nature reserve in central Queensland, Australia, north-east of Longreach. It lies in the upper catchment of Pelican Creek, which flows into the Thomson River and, ultimately, into Lake Eyre. It lies within the Great Artesian Basin and is notable for its many artesian springs and their plants and animals.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
Tatta District of the Sakha Republic was named after the river. The R504 Kolyma Highway crosses the Tatta roughly in the middle of its course. Course. The Tatta originates in the eastern slopes of the Lena Plateau and is the 7th longest tributary of the Aldan. It flows roughly northwards across a wide, flat valley marked by permafrost and thermokarst zones.

Geographic entities mentioned:
surface_form: Lena Plateau
instance_of: Plateau
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.75
lon: 125
Formation and rocks. Volcanism in the Eifel began about 600,000 years ago and led to the formation of numerous volcanic landforms. What was probably the last eruption, which led to the formation of the Ulmener Maar, was about 11,000 years ago. Within those timeframes the Boos maars belong to the youngest formations in the Volcanic Eifel.

Geographic entities mentioned:
surface_form: Ulmener Maar
instance_of: Lake
countries: Germany
coordinates: lat: 50.21
lon: 6.98306
It is part of the Chaudière-Appalaches region and the population was 6,185 as of the Canada 2021 Census. Beauceville's new constitution dates from 1998, when it amalgamated with Saint-François-Ouest and Saint-François-de-Beauce. The previous city was also the creation of a merging between Beauceville and Beauceville-Est, distinction made because each shared a bank of the Chaudière River.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
In 1998 Beauceville gained significant territories, when it annexed the neighbouring municipalities of Saint-François-de-Beauce (the municipality from which Beauceville had originally split) and Saint-François-Ouest. Throughout its history, Beauceville has suffered from spring floods of the Chaudière River, and many streets of the municipality have been repeatedly inundated, causing great damage.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
The municipality has more than 25 manufacturing companies and its industrial park is expanding and welcoming many new companies. Geography. Covering an area of 164.56 km2, Beauceville extends on both banks of the Chaudière River, 85 km south of Quebec City, 55 km from the border of the US state of Maine and 150 km from Sherbrooke. Demographics.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
In addition to her broadcast work, Meacock hosts various business awards and conferences events, and also mentors new broadcasters, actors and public speakers. Her charity work has involved climbing Snowdon, cycling from Manchester to Chester and from Chester to Liverpool, sleeping out for the homeless and abseiling down Liverpool's Radio City Tower.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Gettysburg. The 3rd Alabama mainly fought on the 1st day of battle on July 1, 1863, at the area of the battlefield known as Oak Ridge, specifically the Oak Hill portion of the ridge. There is a monument located on Oak Hill under the name O'Neal's Brigade, which honors the 3rd as well as the 5th, 6th, 12th and 26th infantry regiments. Total strength and casualties.

Geographic entities mentioned:
surface_form: Oak Ridge
instance_of: Landform
countries: United States
coordinates: lat: 39.8867
lon: -77.2342
This region has no sharply defined boundary with the Lüneburg Heath. Lüneburg Heath lies between the rivers Elbe to the north, the Drawehn to the east, the Aller to the south and southwest, the middle course of the Wümme to the west and the Harburg Hills (&quot;Harburger Berge&quot;) to the northwest.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The eastern boundary to the Wendland is formed by the Göhrde-Drawehn Hills (the Ostheide natural region). Parts of Lüneburg Heath are in the &quot;Südheide Nature Park&quot;, others in the Lüneburg Heath Nature Park. Hills and elevations. The highest elevation on Lüneburg Heath is the Wilseder Berg () above NN).

Geographic entities mentioned:
surface_form: Wilseder Berg
instance_of: Mountain
countries: Germany
coordinates: lat: 53.1677
lon: 9.9392
Other hills over high are: Falkenberg (), near Bergen, Ahrberg (), Hakenberg (), Hoher Mechtin (), Pampower Berg (), Lüßberg (), Brunsberg, near Sprötze (), Goldbockenberg (), Hingstberg (), Staffelberg (), Hengstberg (), Höpenberg near Schneverdingen (), Haußelberg (), Breithorn (), Mützenberg (), Tellmer Berg (), Wümmeberg (), Schiffberg (), Hummelsberg and Wulfsberg (each), Drullberg and Thonhopsberg (each), Kruckberg and Wietzer Berg (each) and Höllenberg ().

Geographic entities mentioned:
surface_form: Hoher Mechtin
instance_of: Mountain
countries: Germany
coordinates: lat: 53.0442
lon: 10.9094
surface_form: Haußelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.85722222
lon: 10.1875
surface_form: Wietzer Berg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.8703
lon: 10.0814
Rivers in the area, beside the numerous small heathland streams, include the Wümme, which rises on the western slopes of the Wilseder Berg, in the south the Lachte with its tributary the Lutter, and the Aller, the Vissel, the Böhme, the Grindau, the Meiße and the Örtze. They all belong to the Weser river system. Those flowing into the Elbe are the Aue, the Ilmenau, the Luhe and the Seeve. Geology.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Nature parks and nature reserves. In the northwestern part of Lüneburg Heath is the Lüneburg Heath Nature Park which covers an area of. At its heart, around the Wilseder Berg, is the Lüneburg Heath Nature Reserve (&quot;Naturschutzgebiet&quot; or NSG) founded as long ago as 1921 with of land which is roughly 58% woods and 20% heathland.

Geographic entities mentioned:
surface_form: Wilseder Berg
instance_of: Mountain
countries: Germany
coordinates: lat: 53.1677
lon: 9.9392
The amount required, even in the heyday of production, could have been continuously supplied by an area of woodland about 50 km2 in area, yet the heath covers over 7000 km2. In any case the wood certainly did not come from the heath, but via the waterways, especially from Mecklenburg up the Elbe and from the area of the Schaalsee.

Geographic entities mentioned:
surface_form: Schaalsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.590277777778
lon: 10.914444444444
Mount Cornwell (Antarctica). Mount Cornwell () is a mountain, high, standing south of Mount Washburn in Gromshin Heights along the northeast side of Newcomer Glacier in the northern part of the Sentinel Range. It surmounts lower Vicha Glacier to the east and Newcomer Glacier to the west. The mountain was named by the Advisory Committee on Antarctic Names for Lieutenant James W. Cornwell of U.S.

Geographic entities mentioned:
surface_form: mount cornwell (antarctica)
instance_of: Mountain
coordinates: lat: -77.666694444444
lon: -86.15
surface_form: cornwell
instance_of: Mountain
coordinates: lat: -77.666694444444
lon: -86.15
Mount Cornwell (Antarctica). Mount Cornwell () is a mountain, high, standing south of Mount Washburn in Gromshin Heights along the northeast side of Newcomer Glacier in the northern part of the Sentinel Range. It surmounts lower Vicha Glacier to the east and Newcomer Glacier to the west. The mountain was named by the Advisory Committee on Antarctic Names for Lieutenant James W. Cornwell of U.S.

Geographic entities mentioned:
surface_form: mount cornwell
instance_of: Mountain
coordinates: lat: -77.666694444444
lon: -86.15
surface_form: cornwell
instance_of: Mountain
coordinates: lat: -77.666694444444
lon: -86.15
It surmounts lower Vicha Glacier to the east and Newcomer Glacier to the west. The mountain was named by the Advisory Committee on Antarctic Names for Lieutenant James W. Cornwell of U.S. Navy Squadron VX-6, who was co-pilot on photographic flights over the range on 14–15 December 1959.

Geographic entities mentioned:
surface_form: cornwell
instance_of: Mountain
coordinates: lat: -77.666694444444
lon: -86.15
Lake McLarty. Lake McLarty is a freshwater lake and associated nature reserve on the Swan Coastal Plain of Western Australia. The lake is named after a prominent pioneering family which settled in the district in the early 1860s. It lies about south of Perth on the eastern side of the Harvey Estuary and forms part of the Peel-Yalgorup System Ramsar site.

Geographic entities mentioned:
surface_form: freshwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.6453
lon: -60.3967
Pas de Morgins. Pas de Morgins (el. 1369 m.) is a high mountain pass in the Alps between the canton of Valais in Switzerland and France. It is located at the top of the Val de Morgins, which turns off the Val d'Illiez at Troistorrents. The road through the Val de Morgins is marked by a series of hairpin curves. It connects Monthey and Abondance. Tour de France.

Geographic entities mentioned:
surface_form: Val d'Illiez
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.2409
lon: 6.8922
Though it breeds only in Madagascar, it spends the non-breeding season in a number of countries in the African Great Lakes region and the Indian Ocean islands: Burundi, Democratic Republic of the Congo, Madagascar, Malawi, Rwanda, South Africa, Uganda and Zambia. Description. The Madagascar cuckoo is a small, slim cuckoo, measuring in length.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
No local programming originates here as the station broadcasts complete wall-to-wall syndication. KYDO is considered a &quot;move in&quot; station, because it started in Brawley in California's Imperial Valley before moving closer to San Diego. KSIQ in Brawley, California (1981–2009).

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
&quot;SI&quot; stood for the Spanish-language word for &quot;yes.&quot; This was meant to attract the large Hispanic audience in the Imperial Valley and to have them interpret the name as &quot;Yes-96.&quot; The station would later rebrand as &quot;Q96&quot;, using the last letter of its callsign.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
Lac de Chavoley. Lac de Chavoley is a lake at Ceyzérieu in the Ain department, France. It is located 300 m east of Lac de Morgnieu.

Geographic entities mentioned:
surface_form: Lac de Morgnieu
instance_of: Lake
countries: France
coordinates: lat: 45.823611111111
lon: 5.6869444444444
Lac de Chavoley. Lac de Chavoley is a lake at Ceyzérieu in the Ain department, France. It is located 300 m east of Lac de Morgnieu.

Geographic entities mentioned:
surface_form: lac de chavoley
instance_of: Lake
countries: France
coordinates: lat: 45.824444444444
lon: 5.6963888888889
The area was visited by early 19th century sealers. The feature is named after the Siren nymphs of Greek mythology. Location. Siren Lake is centred at, which is 1.8 km east of Devils Point, 800 m east-southeast of Lucifer Crags, 1 km southwest of Wasp Hill and 680 m north of Sevar Point. Detailed Spanish mapping in 1992, and Bulgarian mapping in 2009 and 2017.

Geographic entities mentioned:
surface_form: Wasp Hill
instance_of: Mountain
coordinates: lat: -62.6644
lon: -61.1311
surface_form: siren lake
instance_of: Lake
coordinates: lat: -62.66888888888889
lon: -61.14805555555556
Siren Lake. Siren Lake (,) is the oval-shaped 250 m long in southeast-northwest direction and 140 m wide lake near the west extremity of South Beaches on Byers Peninsula, Livingston Island in the South Shetland Islands, Antarctica. It has a surface area of 2.7 ha and is separated from Raskuporis Cove waters by a 55 to 70 m wide strip of land. The area was visited by early 19th century sealers.

Geographic entities mentioned:
surface_form: siren lake
instance_of: Lake
coordinates: lat: -62.66888888888889
lon: -61.14805555555556
Flatiron Valley. Flatiron Valley is a north-south valley including a sub-glacial lake, located in the south part of the Ganymede Heights, marginal to Jupiter Glacier, situated in eastern Alexander Island, Antarctica. The name derives from field work in 1978–79 by the Department of Geography, University of Aberdeen, Scotland, with British Antarctic Survey support.

Geographic entities mentioned:
surface_form: Ganymede Heights
instance_of: Mountain
coordinates: lat: -70.8667
lon: -68.4333
surface_form: flatiron valley
instance_of: Landform
coordinates: lat: -70.9
lon: -68.4833
Flatiron Valley. Flatiron Valley is a north-south valley including a sub-glacial lake, located in the south part of the Ganymede Heights, marginal to Jupiter Glacier, situated in eastern Alexander Island, Antarctica. The name derives from field work in 1978–79 by the Department of Geography, University of Aberdeen, Scotland, with British Antarctic Survey support.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Flatiron Valley. Flatiron Valley is a north-south valley including a sub-glacial lake, located in the south part of the Ganymede Heights, marginal to Jupiter Glacier, situated in eastern Alexander Island, Antarctica. The name derives from field work in 1978–79 by the Department of Geography, University of Aberdeen, Scotland, with British Antarctic Survey support.

Geographic entities mentioned:
surface_form: flatiron valley
instance_of: Landform
coordinates: lat: -70.9
lon: -68.4833
The event is not authorised by the Shore estate or the tournament. Born Frances Rose Shore, in 1916, she lived in the Coachella Valley and is credited for having founded in Palm Springs the Colgate-Dinah Shore Winner's Circle women's golf tournament, now known as the LPGA's Chevron Championship in Texas, The Dinah initially coincided with the tournament, which took place the same weekend.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
In a cyst on the fish they undergo metamorphosis to become juvenile mussels and then drop to the substrate to develop further. This mussel is threatened by a number of processes. The rivers it inhabits have been impounded by dams at a number of locations, forming lakes and reservoirs including Lake Ouachita, Lake Hamilton and Lake Catherine. The rivers have been channelized and dredged.

Geographic entities mentioned:
surface_form: Lake Ouachita
instance_of: Lake
countries: United States
coordinates: lat: 34.6
lon: -93.3333
Hawaiian tropical high shrublands. The Hawaiian tropical high shrublands are a tropical savanna ecoregion in the Hawaiian Islands. Geography. The high shrublands ecoregion covers an area of on the upper slopes of the volcanoes Mauna Kea, Mauna Loa, Hualālai, and Haleakalā. Flora. The plant communities include open shrublands, grasslands, and deserts.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
According to the United States Census Bureau, the city has a total area of, of which is land and, or 1.04%, is water. Villa Rica sits on the ridgeline that separates the Chattahoochee and the Tallapoosa river basins. Slightly more than half of Villa Rica lies within Carroll County, and the remainder lies within Douglas County. Climate.

Geographic entities mentioned:
surface_form: Chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
At 12:10 pm on Sunday &quot;Lusitania&quot; was again under way and passing the Daunt Rock Lightship. In the first 24 hours she achieved, with further daily totals of 575, 570, 593 and before arriving at Sandy Hook at 9:05 am Friday 13 September, taking in total 5 days and 54 minutes, 30 minutes outside the record time held by &quot;Kaiser Wilhelm II&quot; of the North German Lloyd line.

Geographic entities mentioned:
surface_form: Sandy Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.452891
lon: -73.995237
__TOC__
&quot;Highlander&quot;. The Kurgan was born in what is now Russia on the coast of the Caspian Sea. His tribe, part of the Kurgan culture, were infamous for their cruelty, known to &quot;toss children into pits full of starved dogs, and watch them fight for [the] meat&quot; for amusement.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Nakajima G10N. The Nakajima G10N &quot;Fugaku&quot; (Japanese: 富岳 or 富嶽, &quot;Mount Fuji&quot;) was a planned Japanese ultra-long-range heavy bomber designed during World War II.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
In 1269 his brother Raimondo, bishop of Como, was captured by Conrad Venosta von Matsch (a minor vassal of Valchiavenna); Napo intervened and freed him in 1273. In the same year, after the election of Rudolph of Habsburg as Holy Roman Emperor, Napo switched to the imperial party in order to counter the dominance of Charles of Anjou. His reward was the title of imperial vicar in Lombardy (1274).

Geographic entities mentioned:
surface_form: Valchiavenna
instance_of: Valley
countries: Italy
coordinates: lat: 46.25
lon: 9.4