Sarmila/GeoWiki-Features huggingface dataset:
The Great Northern Railway enters the locality from the east (Pentland), passes through the town which is served by Torrens Creek railway station (), and exits to the west (Prairie). The creek of the same name arises in the Great Dividing Range, flowing southward to the Thomson River system to eventually run into Lake Eyre.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
Goadby Marwood. Goadby Marwood is a village and former civil parish, now in the parish of Eaton, in the Melton district, in the north of the English county of Leicestershire. It is about north of Melton Mowbray and a few miles from the Vale of Belvoir. In 1931 the parish had a population of 144. History.

Geographic entities mentioned:
surface_form: Vale of Belvoir
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.92
lon: -0.86
It is endemic to Alaska. Charles Paul Alexander first described the species in 1955 under the synonym &quot;Erioptera denali&quot;. The species holotype was collected near the Teklanika River in Denali National Park and Preserve. It is named after Denali. Description. The fly measures about 3.5 millimeters in length, with wings nearly 4 mm.

Geographic entities mentioned:
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
Ultima Thule Peak. Ultima Thule Peak is a glaciated mountain summit located in the Saint Elias Mountains of Wrangell-St. Elias National Park and Preserve, in the U.S. state of Alaska. The peak rises above the Hawkins Glacier to its east, Erickson Creek Glacier to the south, and the Canyon Creek Glacier to the northwest.

Geographic entities mentioned:
surface_form: ultima thule peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.29411
lon: -142.007799
Ultima Thule Peak. Ultima Thule Peak is a glaciated mountain summit located in the Saint Elias Mountains of Wrangell-St. Elias National Park and Preserve, in the U.S. state of Alaska. The peak rises above the Hawkins Glacier to its east, Erickson Creek Glacier to the south, and the Canyon Creek Glacier to the northwest.

Geographic entities mentioned:
surface_form: ultima thule peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.29411
lon: -142.007799
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
The first ascent of the then-unnamed peak was made in 1996 by Paul Claus, Ruedi Homberger, and Reto Reuesh via the south face. Paul Claus dubbed the peak “Ultima Thule Peak.” The second ascent was made April 20, 2013, by Kevin Ditzler and Jay Claus via the southwest ridge. Climate.

Geographic entities mentioned:
surface_form: ultima thule peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.29411
lon: -142.007799
Climate. Based on the Köppen climate classification, Ultima Thule Peak is located in a subarctic climate zone with long, cold, snowy winters, and cool summers. Winds coming off the Gulf of Alaska are forced upwards by the Saint Elias Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: ultima thule peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.29411
lon: -142.007799
Stóra-Björnsfell. Stóra-Björnsfell () is an elongated medium-sized tuya located in Iceland. It contains pillow lava, hyaloclastite and sheet lava. The volcano formed when a subglacial eruption occurred beneath an ice sheet during the last ice age. Stóra-Björnsfell's pillow lava appears originally to have erupted from a fissure.

Geographic entities mentioned:
surface_form: stóra-björnsfell
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.49666667
lon: -20.71138889
The entire journey usually takes 8 days. Most hikers walk the trail from north to south, which is the way the route is described in the most guidebooks. The hike starts in Niederdorf, goes through Monta Piana, where are numerous remnants from fights of First World War. From Monte Piana the hike continues around Monte Cristallo, then to Lake Sorapiss and across the Sorapiss mountain range.

Geographic entities mentioned:
surface_form: Monta Piana
instance_of: Mountain
countries: Italy
coordinates: lat: 46.61527778
lon: 12.23944444
The hike starts in Niederdorf, goes through Monta Piana, where are numerous remnants from fights of First World War. From Monte Piana the hike continues around Monte Cristallo, then to Lake Sorapiss and across the Sorapiss mountain range. After that it nearly touches Antelao mountain and continues through San Vito di Cadore toward Monte Pelmo.

Geographic entities mentioned:
surface_form: Lake Sorapiss
instance_of: Lake
countries: Italy
coordinates: lat: 46.5204
lon: 12.2236
From Monte Piana the hike continues around Monte Cristallo, then to Lake Sorapiss and across the Sorapiss mountain range. After that it nearly touches Antelao mountain and continues through San Vito di Cadore toward Monte Pelmo. From Monte Pelmo the hike continues to Longarone which is the terminus. Part of the hike is common with similar trails Alta Via 4 and Alta Via 5. Accommodation.

Geographic entities mentioned:
surface_form: Antelao
instance_of: Mountain
countries: Italy
coordinates: lat: 46.4525
lon: 12.260555555556
surface_form: Monte Pelmo
instance_of: Mountain
countries: Italy
coordinates: lat: 46.4202
lon: 12.1332
Chand Bibi was appointed regent for Bahadur by the nobles and administered the kingdom in his name. However, in spite of the accord, skirmishes and intermittent fighting continued between Ahmadnagar and the Mughals. In 1599, Akbar launched another invasion of the Deccan, sending his younger son Daniyal against Ahmadnagar.

Geographic entities mentioned:
surface_form: the Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
It usually hunts by hovering over the water to detect prey, before diving vertically bill-first to capture fish. When not foraging, it has a straight rapid flight and have been observed flying at speeds approaching 50 km/h. In Lake Victoria in East Africa, the introduction of the Nile perch reduced the availability of haplochromine cichlids which were formerly the preferred prey of these birds.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Sackpfeife. Sackpfeife is a mountain of Landkreis Waldeck-Frankenberg, Hesse, Germany.

Geographic entities mentioned:
surface_form: sackpfeife
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9554
lon: 8.53856
surface_form: sackpfeife
instance_of: Mountain
countries: Germany
coordinates: lat: 50.95
lon: 8.53333333
However, in 1954, the Free Territory was dissolved and its territory split between Italy and Yugoslavia. Trieste, Grado, Sistiana and Muggia remained part of Italy. Other. After the political closure of most of the Adriatic Coast in 1945 due to the Cold War, the State of Carinthia in Austria began to call its Wörthersee lake district the &quot;Austrian Riviera.&quot;

Geographic entities mentioned:
surface_form: Wörthersee
instance_of: Lake
countries: Austria
coordinates: lat: 46.625
lon: 14.15
Danilevsky was imprisoned for 100 days in the Peter and Paul Fortress and then was sent to live under police surveillance in Vologda, where he worked in provincial administration. In 1852, he was appointed to an expedition, led by Karl Ernst von Baer, to assess the condition of the fishing industry on the Volga and the Caspian Sea.

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
Calpella (Pomo: &quot;Kalpela&quot;, meaning &quot;Mussel bearer&quot;) is an unincorporated community and census-designated place (CDP) in Mendocino County, California, United States. It is located on the Russian River, north of Ukiah. It is situated within the Ukiah Valley, at the intersection of U.S. Route 101 and State Route 20. The population was 799 at the 2020 census, up from 679 in 2010.

Geographic entities mentioned:
surface_form: Ukiah Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.1867
lon: -123.2052
Sjenica Airport. Sjenica Airport (), also known as Dubinje Airport () is a military airport in Serbia, near the town of Sjenica on Pešter plateau. The airport is also near to the mountain resort Zlatar. History. The airport was built as a military one, and used by Yugoslav army air force. During the 1999 NATO bombing of FR Yugoslavia, it was damaged.

Geographic entities mentioned:
surface_form: Pešter
instance_of: Plateau
countries: Sandžak
coordinates: lat: 43.094167
lon: 20.116667
Geography. The region where Kyakhta stands is advantageous for Russo-Chinese trade. The Siberian River Routes connect the fur-bearing lands of Siberia to Lake Baikal. From there, the Selenga River valley is the natural route through the Selenga Highlands southeast of Lake Baikal out onto the plains of Mongolia. History.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Micajah Pond is a pond located in Plymouth, Massachusetts. The Micajah Heights neighborhood surrounds the southeastern portion of the pond and Little Micajah Pond. The maximum depth is. Shenandoah Estates borders the northern portion of the pond known as the lily pond and wraps around the pond bordered by Goldfinch Lane. Boat access is on the southeastern shore of the pond.

Geographic entities mentioned:
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Micajah Pond (Massachusetts). Micajah Pond is a pond located in Plymouth, Massachusetts. The Micajah Heights neighborhood surrounds the southeastern portion of the pond and Little Micajah Pond. The maximum depth is. Shenandoah Estates borders the northern portion of the pond known as the lily pond and wraps around the pond bordered by Goldfinch Lane.

Geographic entities mentioned:
surface_form: micajah pond (massachusetts)
instance_of: Lake
countries: United States
coordinates: lat: 41.9203
lon: -70.6983
Micajah Pond (Massachusetts). Micajah Pond is a pond located in Plymouth, Massachusetts. The Micajah Heights neighborhood surrounds the southeastern portion of the pond and Little Micajah Pond. The maximum depth is. Shenandoah Estates borders the northern portion of the pond known as the lily pond and wraps around the pond bordered by Goldfinch Lane.

Geographic entities mentioned:
surface_form: micajah pond
instance_of: Lake
countries: United States
coordinates: lat: 41.9203
lon: -70.6983
Kilnsey. Kilnsey is a small village in Wharfedale, North Yorkshire, England. It lies on the B6160 road, between the villages of Grassington and Kettlewell, near Arncliffe and just across the River Wharfe from Conistone. The village is north of Skipton and south of Kettlewell. History. The village is mentioned in the Domesday Book of 1086 as &quot;Chilsie&quot; when it was described as waste.

Geographic entities mentioned:
surface_form: Wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
It was established in late summer 1943 as a subcamp of Buchenwald concentration camp, supplying slave labour from many Eastern countries occupied by Germany (including evacuated survivors of eastern extermination camps), for extending the nearby tunnels in the Kohnstein and for manufacturing the V-2 rocket and the V-1 flying bomb.

Geographic entities mentioned:
surface_form: Kohnstein
instance_of: Mountain
countries: Germany
coordinates: lat: 51.54044444
lon: 10.73505556
Led Zeppelin's next album, &quot;Houses of the Holy&quot;, was released in March 1973. It featured further experimentation by the band, who expanded their use of synthesisers and mellotron orchestration. The predominantly orange album cover, designed by the London-based design group Hipgnosis, depicts images of nude children climbing the Giant's Causeway in Northern Ireland.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
The Valley is about long and wide with a general northeast to southwest orientation. The Valley is defined on the east by North Fork Mountain and on the west by the River Knobs. Motorized traffic may gain access to the valley from the west by either Riverton Gap (via the town of Riverton) or Hinkle Gap, through which Root Run and Mill Creek, respectively, drain it.

Geographic entities mentioned:
surface_form: North Fork Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
Route 33 just west of Franklin, West Virginia. Seneca Rocks rise near the northern end of the Valley. Many of the named features in or near the Valley reflect old family names of the original settlers: Judy Gap, Bennett Gap, Teter Gap, and Harper Gap; also Bland Hills, Dolly Ridge, Harman Knob, Harper Knob, Mallow Knob, and Ketterman Knob. 18th century.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
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
They were also attracted by the fertile limestone soils and gently rolling bottomland. They were soon joined by the Teters and by Pennsylvania Dutch families, some having migrated southwest following the ridges and through the &quot;Valley of Virginia&quot; from Pennsylvania's Lebanon and Lancaster counties. A few German families also moved west from Spotsylvania County, Virginia.

Geographic entities mentioned:
surface_form: Valley of Virginia
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
The farms remained largely self-sufficient because the poor roads and absence of turnpikes made it difficult to reach larger markets in adjacent areas. In June 1781, after a difficult passage over North Fork Mountain, the Valley was evangelized by Bishop Francis Asbury. Asbury was one of the two original Methodist missionaries in the United States.

Geographic entities mentioned:
surface_form: North Fork Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
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
Small sash and circular saw mills, however, were present. Geology. Germany Valley is characterized by Ordovician limestones at the culmination of the Wills Mountain anticline. The Valley is formed within the eastern and western limbs of this eroded anticline (fold), which are represented by North Fork Mountain and the River Knobs, respectively.

Geographic entities mentioned:
surface_form: Wills Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.845555555556
lon: -78.681666666667
Small sash and circular saw mills, however, were present. Geology. Germany Valley is characterized by Ordovician limestones at the culmination of the Wills Mountain anticline. The Valley is formed within the eastern and western limbs of this eroded anticline (fold), which are represented by North Fork Mountain and the River Knobs, respectively.

Geographic entities mentioned:
surface_form: North Fork Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
The Valley is defined on the east by North Fork Mountain and on the west by the River Knobs. Motorized traffic may gain access to the valley from the west by either Riverton Gap (via the town of Riverton) or Hinkle Gap, through which Root Run and Mill Creek, respectively, drain it. The southernmost Valley is also slightly entered, via Judy Gap, where a popular overlook is located along U.S.

Geographic entities mentioned:
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 44.4599675
lon: -89.6412311
surface_form: mill creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.871442
lon: -90.093448
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
Germany Valley. Germany Valley is a scenic upland valley high in the Allegheny Mountains of eastern West Virginia originally settled by German (including Pennsylvania Dutch) farmers in the mid-18th century. It is today a part of the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest, although much ownership of the valley remains in private hands.

Geographic entities mentioned:
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
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
surface_form: seneca rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
These settlers brought the familiar custom of placing hex signs on their barns (perhaps the only section of West Virginia where these signs were once found.)
Indians were by no means absent from the region, however, as the famous Seneca Trail (or Great Indian Warpath) passed near the Valley and the nearby British positions at Fort Seybert and Fort Upper Tract had been destroyed (1758) in Indian uprisings led by Killbuck, a Delaware chieftain.

Geographic entities mentioned:
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
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
19th century. At the time of the American Civil War, the communities of the upper North Fork, including Germany Valley, and Franklin, were strongly Confederate in their sympathies, although nearby Seneca Rocks and the lower South Branch Valley were generally northern in persuasion. Pendleton County was a border area like many unprotected by either Federal troops or the Confederates.

Geographic entities mentioned:
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: germany valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
surface_form: seneca rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
Germany Valley. Germany Valley is a scenic upland valley high in the Allegheny Mountains of eastern West Virginia originally settled by German (including Pennsylvania Dutch) farmers in the mid-18th century. It is today a part of the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest, although much ownership of the valley remains in private hands.

Geographic entities mentioned:
surface_form: germany valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
The Valley is noted for its extensive karst and cave development, with dozens of caves and cave systems having been formally documented and mapped. The area was made a National Natural Landmark, the Germany Valley Karst Area, in 1973 by the National Park Service.

Geographic entities mentioned:
surface_form: germany valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
(This is along the valley road leading east from Riverton). These traditional farming families long retained their language and &quot;old country&quot; customs and so the Valley became known as &quot;German Settlement&quot; or &quot;Germany Valley&quot;. At about the same time, many Scotch-Irish families also migrated from the north and bought land in Pendleton County, including Germany Valley.

Geographic entities mentioned:
surface_form: germany valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
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
(This is along the valley road leading east from Riverton). These traditional farming families long retained their language and &quot;old country&quot; customs and so the Valley became known as &quot;German Settlement&quot; or &quot;Germany Valley&quot;. At about the same time, many Scotch-Irish families also migrated from the north and bought land in Pendleton County, including Germany Valley.

Geographic entities mentioned:
surface_form: germany valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
The Valley is formed within the eastern and western limbs of this eroded anticline (fold), which are represented by North Fork Mountain and the River Knobs, respectively. Both North Fork Mountain and the River Knobs are classed as homoclinal ridges and Germany Valley itself as a homoclinal valley. Cave and karst features.

Geographic entities mentioned:
surface_form: germany valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
In 2002—after prolonged negotiations with Greer—the USFWS, West Virginia Department of Natural Resources (WV DNR), WV DEP, caving organizations and local landowners, the Germany Valley Karst Survey (GVKS) was formally contracted to survey the extent of the Hellhole cave system.

Geographic entities mentioned:
surface_form: germany valley
instance_of: Valley
countries: United States
coordinates: lat: 38.765
lon: -79.39
It is today a part of the Spruce Knob–Seneca Rocks National Recreation Area of the Monongahela National Forest, although much ownership of the valley remains in private hands. The Valley is noted for its extensive karst and cave development, with dozens of caves and cave systems having been formally documented and mapped.

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
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Germany Valley is situated in the upper reaches of the North Fork South Branch Potomac River in northeastern Pendleton County, West Virginia. The Valley floor is at an elevation of approximately with the surrounding mountaintops about higher. The Valley is about long and wide with a general northeast to southwest orientation.

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
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Valley floor is at an elevation of approximately with the surrounding mountaintops about higher. The Valley is about long and wide with a general northeast to southwest orientation. The Valley is defined on the east by North Fork Mountain and on the west by the River Knobs.

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
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Route 33 just west of Franklin, West Virginia. Seneca Rocks rise near the northern end of the Valley. Many of the named features in or near the Valley reflect old family names of the original settlers: Judy Gap, Bennett Gap, Teter Gap, and Harper Gap; also Bland Hills, Dolly Ridge, Harman Knob, Harper Knob, Mallow Knob, and Ketterman Knob. 18th century.

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
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Clashes between these units were frequent and bitter, with members of the same families often contending against one another. Raids by Union army units and Union partisans such as the Swamps occurred several times in the Valley during the war years. Originally, the coves and moist slopes of the Valley were covered with fine timber stands, notably including black walnut.

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
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
After crossing the Colorado to avoid the impassable Algodones Dunes west of Yuma, Arizona, they followed the river about south (to about the Arizona's southwest corner on the Colorado River) before turning northwest to about today's Mexicali, Mexico and then turning north through today's Imperial Valley and then northwest again before reaching Mission San Gabriel Arcángel near the future city of Los Angeles, California.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
The majority of the group remained in Montreal until late July, when they given directives to withdraw to New York City. A canoe provided transportation for the trip up the Richelieu River and Lake Champlain. At Whitehall additional men that were employed by McKay joined the southbound party, among them Ovide de Montigny.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Hunt's party continued southwest through the modern state of Wyoming and the hunting party rejoined on the 18th of August, having killed 8 Bison. While at the base of Cloud Peak on 30 August, a scouting party of Apsáalooke visited the camp. The following day a delegation of Apsáalooke on horseback invited them to visit their nearby village.

Geographic entities mentioned:
surface_form: Cloud Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.382138888889
lon: -107.17391388889
New establishments would be created to challenge the NWC across the region in addition to pursuing trading expeditions among various Indigenous nations. A total of almost 60 men were directed to locations from the Willamette Valley of Oregon to the Bitterroot Valley of Montana and the vicinity of modern Kamloops in British Columbia.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
surface_form: Bitterroot Valley
instance_of: Valley
countries: United States
coordinates: lat: 46.247
lon: -114.16
Audubon/Downriver lies within the Okanagan dry forests ecoregion, part of the broader temperate coniferous forest biome. The Okanagan dry forests extend from just south of Spokane northwest through the Okanagan to the Thompson Plateau in British Columbia.

Geographic entities mentioned:
surface_form: Thompson Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.25
lon: -120.5
It is a comparatively compact range located between Garmisch-Partenkirchen, Mittenwald, Seefeld in Tirol and Ehrwald along the border between Germany (Bavaria) and Austria (Tyrol). Zugspitze, the highest peak is at the same time the highest mountain in Germany. The Wetterstein mountains are an ideal region for mountaineers and climbers.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
To the east the Isar forms the boundary from Mittenwald to Scharnitz. South of Scharnitz it continues along the Drahnbach stream to Seestadeln. To the south the boundary extends from Ehrwald along the Gaisbach stream and over the Ehrwalder Alm to the Gaistal valley (Leutascher Ache) and continues via Leutasch-Oberweidach and past the Simmelberg to the north to the Drahnbach.

Geographic entities mentioned:
surface_form: Leutascher Ache
instance_of: Watercourse
countries: Germany
Austria
coordinates: lat: 47.4312
lon: 11.2584
The saddle near the Ehrwalder Alm is the link between the Wetterstein and Mieming Chain. Peaks. The Zugspitze is very frequently climbed using various routes and the Alpspitze summit, too, is a popular destination that can be reached on several different routes. The ridge of Jubiläumsgrat is a high alpine climbing route that links these two summits.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
surface_form: Alpspitze
instance_of: Mountain
countries: Germany
coordinates: lat: 47.429444444444
lon: 11.0475
WBNR. WLNA (1260 AM) is a commercial radio station licensed to Beacon, New York, and serving the Hudson Valley. The station is owned by Pamal Broadcasting and calls itself &quot;The Beacon.&quot; It simulcasts a conservative talk radio format with sister stations WLNA 1460 AM in Peekskill and WGHQ 920 AM in Kingston. The studios are on New York State Route 52 in Beacon.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
There are also the remains of temples to Apollo and Jupiter. During the civil war between Octavian and Antony, Agrippa tried to turn the lake into a military port, the Portus Julius. A waterway was dug from Lake Lucrino to Avernus to this end. The port's remains may still be seen under the lake's surface. Avernus was also regarded as a divine being.

Geographic entities mentioned:
surface_form: Lake Lucrino
instance_of: Lake
countries: Italy
coordinates: lat: 40.829444444444
lon: 14.080277777778
A waterway was dug from Lake Lucrino to Avernus to this end. The port's remains may still be seen under the lake's surface. Avernus was also regarded as a divine being. The 4th-5th century writer Servius the Grammarian described a statue of Avernus, which perspired during the storm after the union of Lake Avernus and Lucrinus Lacus, and to which expiatory sacrifices were offered. '.

Geographic entities mentioned:
surface_form: Lucrinus Lacus
instance_of: Lake
countries: Italy
coordinates: lat: 40.829444444444
lon: 14.080277777778
The valley is narrow and the valley bottom is poorly sorted fluvial and colluvial sands, gravels, and cobbles. In 1883, the Gustavus Blin Wright syndicate was awarded a contract (in return for a land grant) to build a wide and long wagon road from Sicamous on Shuswap Lake, via the four lakes, to Big Eddy on the Columbia River. Begun immediately, the work was completed in October 1884.

Geographic entities mentioned:
surface_form: Shuswap Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.000693
lon: -119.01263
The Permian and Triassic sandstone aquifer in the Otter Valley is one of Devon's largest groundwater sources, supplying drinking water to 200,000 people. Topography. The river's source is north of Otterford, where a stream feeds the Otterhead Lakes: and then through Churchstanton before entering Devon. The river flows through a predominantly rural area, with small cattle, sheep and dairy farms.

Geographic entities mentioned:
surface_form: Otterhead Lakes
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 50.9189
lon: -3.10444
Swithinbank Slope. Swithinbank Slope is a semi-circular ice slope, about 25 nautical miles (46 km) long, between Mount Hallgren and Newmayer Cliffs in the Kirwan Escarpment of Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and air photos by the Norwegian expedition (1958–59). Named for Charles W.

Geographic entities mentioned:
surface_form: Mount Hallgren
instance_of: Mountain
coordinates: lat: -73.383333333333
lon: -3.3666666666667
surface_form: Kirwan Escarpment
instance_of: Landform
coordinates: lat: -73.4167
lon: -3.5
surface_form: swithinbank slope
instance_of: Landform
coordinates: lat: -73.4667
lon: -2.2
Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and air photos by the Norwegian expedition (1958–59). Named for Charles W. Swithinbank, glaciologist with NBSAE.

Geographic entities mentioned:
surface_form: charles
instance_of: Mountain
coordinates: lat: -67.38333
lon: 50
Swithinbank Slope. Swithinbank Slope is a semi-circular ice slope, about 25 nautical miles (46 km) long, between Mount Hallgren and Newmayer Cliffs in the Kirwan Escarpment of Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and air photos by the Norwegian expedition (1958–59). Named for Charles W.

Geographic entities mentioned:
surface_form: swithinbank slope
instance_of: Landform
coordinates: lat: -73.4667
lon: -2.2
Two abortive rounds of talks took place across Victoria Falls in August 1975 and Geneva, Switzerland between October and December 1976. While the latter conference was going on, the RLI played a key role in one of the security forces' biggest victories in the war thus far, at &quot;Hill 31&quot; in the Honde Valley on 15 November 1976.

Geographic entities mentioned:
surface_form: Honde Valley
instance_of: Valley
countries: Zimbabwe
coordinates: lat: -18.49677778
lon: 32.8532
The Battle of &quot;Hill 31&quot;. Call sign 81A of K Company, Rhodesia Regiment (RR), patrolling the Mutasa North Tribal Trust Lands on Operation Thrasher, spotted a group of insurgents about 30 to 40 strong at 04:45 on 15 November 1976, just south of a kraal in the Honde Valley, about north of Umtali and from the Mozambique border.

Geographic entities mentioned:
surface_form: Honde Valley
instance_of: Valley
countries: Zimbabwe
coordinates: lat: -18.49677778
lon: 32.8532
The blasting revealed a variety of fossil footprints. In 1882 paleontologists from the National Academy of Sciences identified the tracks as belonging to Pleistocene creatures like birds, horses, lions, mastodons, giant sloths, and wolves. Early in 1900 a new Nevada fossil site was discovered in the Virgin Valley. The site bore three fossil rich horizons.

Geographic entities mentioned:
surface_form: Virgin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -114.082
Harrington later returned to the site and uncovered more of the sloth's bones. In 1933, the Tule Springs Expedition, led by Fenley Hunter, was the first major effort to explore the archaeological importance of the area surrounding Tule Springs. The Tule Springs Archaeological Site contains ground sloths, mammoths, prehistoric horses and American camels and the first giant condors in Nevada.

Geographic entities mentioned:
surface_form: Tule Springs
instance_of: Landform
countries: United States
coordinates: lat: 36.3239
lon: -115.266
Lägh da Cavloc. Lägh da Cavloc (Italian: &quot;Lago di Cavloccio&quot;) is a lake near Maloja Pass in the Val Forno, Grisons, Switzerland. While the northern shore is rocky and lined with pine trees, there is a beach on the shallow southern shore that is a popular swimming spot despite the cold water temperature.

Geographic entities mentioned:
surface_form: Val Forno
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.367111111111114
lon: 9.713277777777778
surface_form: val forno
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.367111111111114
lon: 9.713277777777778
surface_form: lägh da cavloc
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.38
lon: 9.7047222222222
surface_form: lago di cavloccio
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.38
lon: 9.7047222222222
Lägh da Cavloc. Lägh da Cavloc (Italian: &quot;Lago di Cavloccio&quot;) is a lake near Maloja Pass in the Val Forno, Grisons, Switzerland. While the northern shore is rocky and lined with pine trees, there is a beach on the shallow southern shore that is a popular swimming spot despite the cold water temperature.

Geographic entities mentioned:
surface_form: lägh da cavloc
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.38
lon: 9.7047222222222
Description. The Payson ophiolite crops out south and west of the town of Payson, Arizona, in the Arizona transition zone between the Colorado Plateau and the Basin and Range. It consists of a well-developed sheeted dyke complex that grades below into gabbroic rock and above into submarine volcanic rock. The whole sequence dips gently (by about 15 degrees) to the southwest.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Duxbury Beach. Duxbury Beach is a barrier beach in the town of Duxbury, Massachusetts. It is six miles long and is accessed by the Powder Point Bridge from Duxbury, or Gurnet Road from Marshfield.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
Duxbury Beach is a barrier beach in the town of Duxbury, Massachusetts. It is six miles long and is accessed by the Powder Point Bridge from Duxbury, or Gurnet Road from Marshfield. Since 1975, approximately 4.5 miles of the beach is owned by Duxbury Beach Reservation, Inc, which annually leases a substantial portion of the beach—excepting the Duxbury Beach Park area—to the town of Duxbury.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
History. An early trans-Atlantic cable came ashore at Rouse's Hummock on July 23, 1869, connecting France with the United States. Among those on the first call were Napoleon III and President James Garfield. George and Georgianna Wright purchased most of the land of Duxbury Beach in 1885 and constructed cottages on the beach at that time.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
George and Georgianna Wright purchased most of the land of Duxbury Beach in 1885 and constructed cottages on the beach at that time. In 1892, George Wright led the construction of what was known as &quot;Long Bridge&quot; and &quot;Gurnet Bridge,&quot; which in its refurbished form remains the only access road from Duxbury to Duxbury Beach. The original bridge was built with oak and pine lumber.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
The original bridge was built with oak and pine lumber. In 1919, George Wright's estate sold their land holdings on Duxbury Beach to the Duxbury Beach Association, a common law trust consisting of Duxbury residents. Duxbury Beach remained the property of the Duxbury Beach Association from 1919 until 1975.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
The original bridge was built with oak and pine lumber. In 1919, George Wright's estate sold their land holdings on Duxbury Beach to the Duxbury Beach Association, a common law trust consisting of Duxbury residents. Duxbury Beach remained the property of the Duxbury Beach Association from 1919 until 1975.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
Regular attempts were made during this time period by the Massachusetts State Legislature and the Massachusetts Governor's Office to acquire the beach. Beginning in 1973, the Duxbury Beach Association leased annually the beach to the Town of Duxbury. Ownership of the beach was transferred in 1975 from the Duxbury Beach Association to Duxbury Beach Reservation, Inc., a non-profit organization.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
Regular attempts were made during this time period by the Massachusetts State Legislature and the Massachusetts Governor's Office to acquire the beach. Beginning in 1973, the Duxbury Beach Association leased annually the beach to the Town of Duxbury. Ownership of the beach was transferred in 1975 from the Duxbury Beach Association to Duxbury Beach Reservation, Inc., a non-profit organization.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
According to Envision Duxbury's Comprehensive Master Plan, released in 2019 and the result of a coordinated planning effort by the Town of Duxbury and the Metropolitan Area Planning Council, 83% of Duxbury residents reported that Duxbury Beach is the town of Duxbury's greatest asset. Wildlife and ecosystems.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
Fauna. Piping plovers nest on the beach, and their habitats are protected by the Town of Duxbury's conservation officers and Duxbury Beach Reservation, Inc.'s staff.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
Piping plovers are threatened or endangered depending on the location in North America, but due in part to protected nesting sites like Duxbury Beach, Massachusetts piping plovers have seen a 500% increase in breeding pairs between 1986 and 2023, resulting in 50% of piping plovers on the Atlantic Coast nesting in Massachusetts.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
Brant, sanderlings, semipalmated plovers, sandpipers, sea ducks, loons, roseate terns, grebes, cormorants, mergansers, swallows, and various gulls are all present in their proper seasons. Powder Point Bridge. The Powder Point Bridge is the only access road by which the town of Duxbury is joined to Duxbury Beach. The current bridge's construction was completed on August 29, 1987.

Geographic entities mentioned:
surface_form: duxbury beach
instance_of: Landform
countries: United States
coordinates: lat: 42.04176944
lon: -70.63559167
Watson Bluff. Watson Bluff () is a dark bluff 225 m, at the east end of David Island. Discovered by the Australasian Antarctic Expedition, 1911–14, under Mawson, and named for Andrew D. Watson, geologist with the expedition.

Geographic entities mentioned:
surface_form: watson bluff
instance_of: Landform
coordinates: lat: -66.4167
lon: 98.95
The Noyyal River runs through Coimbatore and forms the southern boundary of the old city limits. The city sits amidst Noyyal's basin area and has an extensive tank system fed by the river and rainwater. The eight major tanks/wetland areas of Coimbatore are Singanallur, Kallimadai, Valankulam, Ukkadam Periyakulam, Selvampathy, Narasampathi, Krishnampathi, Selvachinthamani, and Kumaraswami tanks.

Geographic entities mentioned:
surface_form: Singanallur
instance_of: Lake
countries: India
coordinates: lat: 10.98905278
lon: 77.02274444
surface_form: Valankulam
instance_of: Lake
countries: India
coordinates: lat: 10.9917
lon: 76.9722
The breed designation was established at the All-Union Cynological Congress in 1947, using dogs from the Lake Baikal region, Irkutsk Oblast, Evenki Autonomous Okrug, as well as the Amur River basin and coastal regions. In 1949, standards for the East Siberian laika was approved, however systematic breeding would not begin until the 1970s in government kennels at Irkutsk and in Leningrad.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Watkins returned to the Los Angeles area, where, at a San Fernando Valley street corner, he was recognized and picked up in a hollowed-out school bus that was painted black, driven by the same two Manson girls, who had greeted him at the door of the Topanga Canyon house.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
It was July 4, 1968. Watkins remained with the Family and became Manson's chief lieutenant. On October 31, he set out with the others in the group's school bus to Goler Wash, near Death Valley. There, over the next few days, Manson set up additional Family bases at two unused (or little-used) ranches, Myers and Barker. Helter Skelter involvement.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556