Sarmila/GeoWiki-Features huggingface dataset:
Pine Valley Peak. Pine Valley Peak is a mountain located in Zion National Park in Washington County, Utah, United States. Description. Pine Valley Peak, a formation composed of white Navajo Sandstone, is situated in Pine Valley, north-northwest of Springdale, Utah. Its neighbors include North Guardian Angel, to the southeast, and South Guardian Angel, to the south-southeast.

Geographic entities mentioned:
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4175
lon: -113.687
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 37.1086606
lon: -90.9967926
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 40.5496714
lon: -111.1421159
surface_form: pine valley peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.33526
lon: -113.07717
Pine Valley Peak. Pine Valley Peak is a mountain located in Zion National Park in Washington County, Utah, United States. Description. Pine Valley Peak, a formation composed of white Navajo Sandstone, is situated in Pine Valley, north-northwest of Springdale, Utah. Its neighbors include North Guardian Angel, to the southeast, and South Guardian Angel, to the south-southeast.

Geographic entities mentioned:
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4175
lon: -113.687
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 37.1086606
lon: -90.9967926
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 40.5496714
lon: -111.1421159
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: pine valley peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.33526
lon: -113.07717
Pine Valley Peak. Pine Valley Peak is a mountain located in Zion National Park in Washington County, Utah, United States. Description. Pine Valley Peak, a formation composed of white Navajo Sandstone, is situated in Pine Valley, north-northwest of Springdale, Utah. Its neighbors include North Guardian Angel, to the southeast, and South Guardian Angel, to the south-southeast.

Geographic entities mentioned:
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4175
lon: -113.687
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4175
lon: -113.687
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 37.1086606
lon: -90.9967926
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 37.1086606
lon: -90.9967926
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 40.5496714
lon: -111.1421159
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 40.5496714
lon: -111.1421159
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
surface_form: pine valley peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.33526
lon: -113.07717
Climate. Spring and fall are the most favorable seasons to visit Pine Valley Peak. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer.

Geographic entities mentioned:
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 38.4175
lon: -113.687
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 37.1086606
lon: -90.9967926
surface_form: pine valley
instance_of: Valley
countries: United States
coordinates: lat: 40.5496714
lon: -111.1421159
surface_form: pine valley peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.33526
lon: -113.07717
Katase. Katase is a village in Alutaguse Parish, Ida-Viru County, in northeastern Estonia. It's located on the northern shore of Lake Peipus. Katase has a population of 49 (as of 2011). Katase was first mentioned in 1419.

Geographic entities mentioned:
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
These unregulated inflows had a destabilizing effect on the lake’s ecosystem, leading to extensive flooding, followed later by episodes of drying, which disrupted the lake's natural balance. In an attempt to mitigate further ecological impact, a weir was constructed in 1980 at the junction between Lake Tuzkan and Lake Aydar, intended to regulate water inflow into Tuzkan.

Geographic entities mentioned:
surface_form: Lake Aydar
instance_of: Lake
countries: Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 40.89
lon: 66.92
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
Tuzkan Lake. Lake Tuzkan (Uzbek: Tuzkon, Cyrillic: Тузкан) also known as Tuzkansee, former endorheic (drainless) lake located in southeastern Kyzylkum, Uzbekistan. It lies within the territory of Jizzakh Region (&quot;Viloyat Jizzax&quot;) and forms part of the, which collectively spans an area of approximately 4,000 km². Prehistory.

Geographic entities mentioned:
surface_form: tuzkan lake
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
Tuzkan Lake. Lake Tuzkan (Uzbek: Tuzkon, Cyrillic: Тузкан) also known as Tuzkansee, former endorheic (drainless) lake located in southeastern Kyzylkum, Uzbekistan. It lies within the territory of Jizzakh Region (&quot;Viloyat Jizzax&quot;) and forms part of the, which collectively spans an area of approximately 4,000 km². Prehistory.

Geographic entities mentioned:
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
surface_form: tuzkansee
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
Prehistory. Until the mid-20th century, Lake Tuzkan, which once reached a maximum recorded depth of 237 meters, was fed exclusively by the during the spring snowmelt. This seasonal inflow caused temporary water accumulation, but the lake would typically evaporate during the hot summer months.

Geographic entities mentioned:
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
This seasonal inflow caused temporary water accumulation, but the lake would typically evaporate during the hot summer months. Unlike other nearby lakes—many of which were artificially created or expanded through human activities such as drainage and irrigation infrastructure in the Mirzachoʻl steppe—Lake Tuzkan is of natural origin. Development in the modern era.

Geographic entities mentioned:
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
Between February 1969 and February 1970, nearly 60% of the Syr Darya’s average annual discharge—approximately 22 km³—was diverted into the Arnasay lowlands. This large-scale redirection of water reached Lake Tuzkan, dramatically increasing its surface area and volume.

Geographic entities mentioned:
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
A subsequent snowmelt in the spring of 1994 led to a further rise of three meters, bringing the lake’s depth to around 242 meters. As a result, the land bridge between Lake Tuzkan and Lake Aydar, along with the weir, was completely submerged. Since that event, Lake Tuzkan has effectively merged with Lake Aydar, and no clear boundary now exists between the two bodies of water.

Geographic entities mentioned:
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
As a result, the land bridge between Lake Tuzkan and Lake Aydar, along with the weir, was completely submerged. Since that event, Lake Tuzkan has effectively merged with Lake Aydar, and no clear boundary now exists between the two bodies of water. Geography and bathymetry.

Geographic entities mentioned:
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
The lake currently spans an area of approximately 705 km², with an average depth ranging between 20 and 40 metres. Following the submersion of the land bridge separating it from Lake Aydar, the water level of Lake Tuzkan has synchronized with that of Lake Aydar and fluctuates seasonally. The average water temperature is 0.2°C in January, 13.2°C in April, 27.5°C in July, and 16.4°C in October.

Geographic entities mentioned:
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
Nature conservation. In addition to the characteristic fauna of the Kyzylkum Desert, Lake Tuzkan serves as a vital habitat for a wide range of water birds, many of which began migrating to the area following the formation of Lake Aydar. The region is recognized as an Important Bird Area (IBA) and is listed under the Ramsar Convention on Wetlands of International Importance.

Geographic entities mentioned:
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
On 10 July 2018, both parties formalized an agreement to construct two nuclear power plant units, each with a capacity of 1,200 MW, for a total cost of USD 11 billion. Between August 2018 and March 2019, four potential sites were evaluated, and a location west of Lake Tuzkan, in the Forish district, was identified as the most suitable for the construction of the new Uzbek nuclear power plant.

Geographic entities mentioned:
surface_form: tuzkan
instance_of: Lake
countries: Uzbekistan
coordinates: lat: 40.6
lon: 67.483333333333
It is bordered by the River Dee to the north and east. Threave Castle stands on an island in the river. The River Dee is commonly known as the Black Water of Dee on the northern border, the name changes with the meeting of the Water of Ken to the north west and is then known as Loch Ken along the eastern border. Balmaghie parish borders Girthon to the west and Tongland and Twynholm to the south.

Geographic entities mentioned:
surface_form: Loch Ken
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.009
lon: -4.056
U'wa means &quot;intelligent people who can speak&quot;. The Betoye with 800 members constitutes the second-largest ethnic group in the department. They inhabit the banks of the Cravo Norte River and the municipality of Tame. The area of its territory is. Their language is considered part of the Chibcha language family.

Geographic entities mentioned:
surface_form: Cravo Norte River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 6.29382
lon: -70.19937
Geography. The area of what was Montogmeryshire was almost wholly mountainous, although there are some fertile valleys in the east. The highest point (county top) was Moel Sych at, whose summit lies at the triple county boundary point of Montgomeryshire, Denbighshire and Merionethshire in the Berwyn Mountains. The county top of Denbighshire, Cadair Berwyn at, was less than a kilometre away.

Geographic entities mentioned:
surface_form: Moel Sych
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.87608
lon: -3.38878
The highest point (county top) was Moel Sych at, whose summit lies at the triple county boundary point of Montgomeryshire, Denbighshire and Merionethshire in the Berwyn Mountains. The county top of Denbighshire, Cadair Berwyn at, was less than a kilometre away. Its main rivers were the River Severn (which flows east into Shropshire) and the River Dyfi (which flows west into the Irish Sea).

Geographic entities mentioned:
surface_form: Cadair Berwyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.8806
lon: -3.38099
French Valley. French Valley is a region located in southwestern Riverside County, near the cities and communities of Hemet, Winchester, Murrieta, and Temecula in the state of California, United States. It is part of the Plains of Leon, contiguous with the Perris Plain, that drains into the Temecula Basin by means of tributaries of the Santa Margarita River. History.

Geographic entities mentioned:
surface_form: french valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
It is part of the Plains of Leon, contiguous with the Perris Plain, that drains into the Temecula Basin by means of tributaries of the Santa Margarita River. History. Since the late 1800s, the French Valley was home to French grain farmers and sheepherders. After the Franco-Prussian War and the Alsace becoming German, many French-speaking residents fled to America.

Geographic entities mentioned:
surface_form: french valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
After the Franco-Prussian War and the Alsace becoming German, many French-speaking residents fled to America. Among the early settlers of the French Valley were Auguste Giagnaire, Jean Labrucherie and Alexandre, Auguste and Calixte Vial, the Pourroys and the Nicolases. The train network eventually reached Temecula and Murrieta, but not the area inhabited by the French.

Geographic entities mentioned:
surface_form: french valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
Among the early settlers of the French Valley were Auguste Giagnaire, Jean Labrucherie and Alexandre, Auguste and Calixte Vial, the Pourroys and the Nicolases. The train network eventually reached Temecula and Murrieta, but not the area inhabited by the French. The first use of the name &quot;French Valley&quot; occurred in 1913 in a California Conservation Commission report.

Geographic entities mentioned:
surface_form: french valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
A traditional lifestyle was maintained until 1964 when the Metropolitan Water District of Southern California acquired 6,000 acres of land to build the Skinner Reservoir that started operating in 1976. Many ranches were immersed in the new lake. In 1989, the French Valley Airport was inaugurated. It was built on the land of the Borel family.

Geographic entities mentioned:
surface_form: french valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
Many ranches were immersed in the new lake. In 1989, the French Valley Airport was inaugurated. It was built on the land of the Borel family. In 1993, a jail opened, and later became the Southwest Justice Center. In 2007, 702 acres of the French Valley were designated as a wildlife area by the California Department of Fish and Wildlife. Geography. According to the U.S.

Geographic entities mentioned:
surface_form: french valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
Other places nearby include the Skinner Reservoir in the Lake Skinner Park, and Diamond Valley Lake. French Valley is located within 10 minutes of nearby cities Temecula and Murrieta as well as the 15 and 215 freeways. French Valley is also less than 15 minutes from the Temecula Valley Wine Country and Old Town Temecula. The nearby French Valley Airport is named after the valley.

Geographic entities mentioned:
surface_form: french valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
French Valley is located within 10 minutes of nearby cities Temecula and Murrieta as well as the 15 and 215 freeways. French Valley is also less than 15 minutes from the Temecula Valley Wine Country and Old Town Temecula. The nearby French Valley Airport is named after the valley. French Valley is considered to be in the greater Inland Empire region of Southern California.

Geographic entities mentioned:
surface_form: french valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
surface_form: french valley
instance_of: Valley
countries: United States
coordinates: lat: 33.5959
lon: -117.125
The airport was permanently closed by FAA NOTAM on June 3, 2019. The airport's location was within 5 miles of three visitor attractions: the, the, and Mount Snow ski area. Facilities and aircraft. The property covers an area of 35 acres (14 ha) at an elevation of 1,953 feet (595 m) above mean sea level.

Geographic entities mentioned:
surface_form: Mount Snow
instance_of: Mountain
countries: United States
coordinates: lat: 42.95897
lon: -72.92371
History. Caspar René Gregory dated the manuscript to the 10th century. Currently the manuscript is dated by the INTF to the 10th century. The manuscript was added to the list of New Testament manuscripts by C. R. Gregory (1078e). Gregory saw it in 1886. Currently the manuscript is housed at the Great Lavra (A' 16), in Athos.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Abriachan. Abriachan (; Gaelic: &quot;Obar Itheachan&quot;), is a village in the Highland council area of Scotland. It is situated high above the western shore of Loch Ness, 15 km to the south-west of the city of Inverness. The village has a population of approximately 120.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
Brigit's Garden. Brigit's Garden is a garden in County Galway, Ireland, located to the west of Lough Corrib. It is open to the public and is dedicated to the goddess Brigid and the Celtic calendar. The founders describe it as &quot;place of connection with nature, beauty and Celtic heritage&quot;.

Geographic entities mentioned:
surface_form: Lough Corrib
instance_of: Lake
countries: Ireland
coordinates: lat: 53.466666666667
lon: -9.2833333333333
Mount Terror (Antarctica). Mount Terror is an extinct volcano about high on Ross Island, Antarctica, about eastward of Mount Erebus. Mount Terror was named in 1841 by polar explorer Sir James Clark Ross for his second ship, HMS &quot;Terror&quot;. Geology. Mount Terror is a shield volcano that forms the eastern part of Ross Island, Antarctica.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Geography. The rocks at the summit have not been studied, but rocks from the lower areas range from 0.82 to 1.75 million years old, and Mount Terror shows no signs of more recent volcanic activity. The first ascent of Mount Terror was made by a New Zealand party in 1959. The mountain is to the west of Cape Crozier, and east of Mount Terra Nova and Mount Erebus. Kienle Nunataks.

Geographic entities mentioned:
surface_form: Mount Terra Nova
instance_of: Mountain
coordinates: lat: -77.5167
lon: 167.95
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount terra nova
instance_of: Mountain
coordinates: lat: -77.5167
lon: 167.95
surface_form: terra nova
instance_of: Mountain
coordinates: lat: -77.5167
lon: 167.95
At the suggestion of P.R. Kyle, named by Advisory Committee on Antarctic Names (US-ACAN) after Juergen Kienle (d.), Geophysical Institute, University of Alaska, Fairbanks, a United States Antarctic Project (USAP) team leader for the investigation of volcanic activity and seismicity on Mount Erebus in six field seasons, 1980-81 through 1985-86. Mount Sutherland.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
The peak is west-southwest of the summit of Mount Terror and south of Mount Sutherland. At the suggestion of P.R. Kyle, named by Advisory Committee on Antarctic Names (US-ACAN) (2000) after James A. Moore, a member of the New Mexico Institute of Mining and Technology team on Mount Erebus in the 1983–84 and 1985-86 field seasons. He completed his M.S. thesis on the geology of Mount Erebus.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
At the suggestion of P.R. Kyle, named by Advisory Committee on Antarctic Names (US-ACAN) (2000) after James A. Moore, a member of the New Mexico Institute of Mining and Technology team on Mount Erebus in the 1983–84 and 1985-86 field seasons. He completed his M.S. thesis on the geology of Mount Erebus. Ohau Peak. A sharp rock peak northeast of the summit of Mount Terror on Ross Island.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
Kyle, named by Advisory Committee on Antarctic Names (US-ACAN) (2000) after Werner F. Giggenbach, Chemistry Division, DSIR, who worked in the NZAP at Mount Erebus in four field seasons during the 1970s. He rappelled into the Inner Crater of Mount Erebus in 1978, but had to be pulled out when an eruption showered him and colleagues on the crater rim with volcanic bombs.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Giggenbach, Chemistry Division, DSIR, who worked in the NZAP at Mount Erebus in four field seasons during the 1970s. He rappelled into the Inner Crater of Mount Erebus in 1978, but had to be pulled out when an eruption showered him and colleagues on the crater rim with volcanic bombs. He was one of the leading volcanic gas geochemists of the period. Chuan Peak.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
Chuan who, as a scientist with the Brunswick Corporation, Costa Mesa, CA, undertook many airborne surveys of volcanic aerosols from Mount Erebus and also did sampling at the crater rim, 1983–84 and 1986–87; investigator (with Julie Palais) on a project which examined aerosols between Mount Erebus and the South Pole. Manahan Peak. A prominent peak east of Giggenbach Ridge in northeast Ross Island.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
Palmer and Laurence M. Gould. Rohnke Crests. Two rock ridges, about high, that are parallel and rise above the general ice mantle on the southeast slopes of Mount Terror. This feature is east of the head of Eastwind Glacier and northeast of Conical Hill. Names in association with Eastwind Glacier after Captain (later Rear Admiral) Oscar C.

Geographic entities mentioned:
surface_form: the general
instance_of: Mountain
coordinates: lat: 44.483387
lon: -114.802816
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Mount Terror (Antarctica). Mount Terror is an extinct volcano about high on Ross Island, Antarctica, about eastward of Mount Erebus. Mount Terror was named in 1841 by polar explorer Sir James Clark Ross for his second ship, HMS &quot;Terror&quot;. Geology. Mount Terror is a shield volcano that forms the eastern part of Ross Island, Antarctica.

Geographic entities mentioned:
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Mount Terror (Antarctica). Mount Terror is an extinct volcano about high on Ross Island, Antarctica, about eastward of Mount Erebus. Mount Terror was named in 1841 by polar explorer Sir James Clark Ross for his second ship, HMS &quot;Terror&quot;. Geology. Mount Terror is a shield volcano that forms the eastern part of Ross Island, Antarctica.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
It is the second-largest of the four volcanoes that make up Ross Island. Geography. The rocks at the summit have not been studied, but rocks from the lower areas range from 0.82 to 1.75 million years old, and Mount Terror shows no signs of more recent volcanic activity. The first ascent of Mount Terror was made by a New Zealand party in 1959.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Geography. The rocks at the summit have not been studied, but rocks from the lower areas range from 0.82 to 1.75 million years old, and Mount Terror shows no signs of more recent volcanic activity. The first ascent of Mount Terror was made by a New Zealand party in 1959. The mountain is to the west of Cape Crozier, and east of Mount Terra Nova and Mount Erebus. Kienle Nunataks.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
The first ascent of Mount Terror was made by a New Zealand party in 1959. The mountain is to the west of Cape Crozier, and east of Mount Terra Nova and Mount Erebus. Kienle Nunataks. Three aligned nunataks to the north of Mount Terror in northeast Ross Island. The nunataks trend east-west for and rise to about. The central nunatak is north-northeast of the Mount Terror summit.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
The mountain is to the west of Cape Crozier, and east of Mount Terra Nova and Mount Erebus. Kienle Nunataks. Three aligned nunataks to the north of Mount Terror in northeast Ross Island. The nunataks trend east-west for and rise to about. The central nunatak is north-northeast of the Mount Terror summit. At the suggestion of P.R.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Mount Sutherland. A peak west-northwest of the summit of Mount Terror on Ross Island. The feature rises to about. Named by Advisory Committee on Antarctic Names (US-ACAN) (2000) after Alexander L.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Rohnke, USCG, who commanded United States Coast Guard Cutter (USCGC) Eastwind in Ross Sea during United States Navy (United States Navy) Operation Deep Freeze (OpDFrz) I, 1955-56. Moore Peak. A peak rising to high on the west slope of Mount Terror, Ross Island. The peak is west-southwest of the summit of Mount Terror and south of Mount Sutherland. At the suggestion of P.R.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Moore Peak. A peak rising to high on the west slope of Mount Terror, Ross Island. The peak is west-southwest of the summit of Mount Terror and south of Mount Sutherland. At the suggestion of P.R. Kyle, named by Advisory Committee on Antarctic Names (US-ACAN) (2000) after James A.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
He completed his M.S. thesis on the geology of Mount Erebus. Ohau Peak. A sharp rock peak northeast of the summit of Mount Terror on Ross Island. The feature rises to about high and is central in three aligned summits north of Mount McIntosh. Named by New Zealand Geographic Board (NZGB) (2000) after a peak near the locality of Tekapo (see Tekapo Ridge), New Zealand. Giggenbach Ridge.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Named by New Zealand Geographic Board (NZGB) (2000) after a peak near the locality of Tekapo (see Tekapo Ridge), New Zealand. Giggenbach Ridge. A north-south chain of summits, long, located to the west and northwest of Mount Terror. The ridge rises to about west of Mount Terror, but descends to at the north end. Named at the suggestion of P.R.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Giggenbach Ridge. A north-south chain of summits, long, located to the west and northwest of Mount Terror. The ridge rises to about west of Mount Terror, but descends to at the north end. Named at the suggestion of P.R. Kyle, named by Advisory Committee on Antarctic Names (US-ACAN) (2000) after Werner F.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Manahan Peak. A prominent peak east of Giggenbach Ridge in northeast Ross Island. The peak rises to over high northwest of the summit of Mount Terror. Named by the Advisory Committee on Antarctic Names (US-ACAN) (2000) after biologist Donal T.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Barker Peak. A peak west-northwest of Mount Terror on Ross Island. The feature rises to about high and is the western of two peaks near the south end of Giggenbach Ridge. Name by New Zealand Geographic Board (NZGB) (2000) after Major James R. M. Barker, officer in command at Scott Base, 1970–71; a NZAP manager, 1970-86. Joyce Peak.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Tent Peak. A tent-shaped peak rising to about high midway between Mount Terror and Cape Crozier. It was descriptively named by a party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1958–59, which occupied the peak as an astronomical control station, January 5, 1959, and erected a tent below the peak. The Tooth.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
The Tooth. A distinctive rock outcrop on the eastern slopes of Mount Terror at an elevation of about. The feature lies south-southeast of Tent Peak and is reported to resemble a fossilized shark's tooth. Descriptively named by a party of the NZGSAE, 1958–59, working in eastern Ross Island. Slattery Peak.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
Descriptively named by a party of the NZGSAE, 1958–59, working in eastern Ross Island. Slattery Peak. A somewhat isolated rock peak, about high, that rises above the ice mantle southeast of Mount Terror. The peak position is additionally defined as southwest of The Knoll and east-northeast of Rohnke Crests.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
The name Ponui (meaning south wind) is one of several Maori wind names applied by New Zealand Geographic Board (NZGB) in this vicinity. Conical Hill. A small but distinctive rock hill, high, on the south slopes of Mount Terror, above Cape MacKay. Given this descriptive name by the British Antarctic Expedition, 1910–13, under Scott.

Geographic entities mentioned:
surface_form: terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
surface_form: mount terror
instance_of: Mountain
coordinates: lat: -77.516666666667
lon: 168.53333333333
A peak west-northwest of Mount Terror on Ross Island. The feature rises to about high and is the western of two peaks near the south end of Giggenbach Ridge. Name by New Zealand Geographic Board (NZGB) (2000) after Major James R. M. Barker, officer in command at Scott Base, 1970–71; a NZAP manager, 1970-86. Joyce Peak. A peak rising to over high in the north-central part of Ross Island.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
It stands west of the main summits of Giggenbach Ridge and south-southeast of Wyandot Point. Named by Advisory Committee on Antarctic Names (US-ACAN) (2000) after Karen Joyce, a long-term ASA employee, who from 1990 made 10 deployments to McMurdo Station, including a winter-over; assisted with computers in the Crary Science and Engineering Center. Kristin Peak.

Geographic entities mentioned:
surface_form: joyce
instance_of: Body of water
Lake
coordinates: lat: -77.7167
lon: 161.633
The peak position is additionally defined as southwest of The Knoll and east-northeast of Rohnke Crests. Named after Leo Slattery, who wintered at Scott Base three times, twice as Officer in Charge; Post Clerk on Ross Island, summer 1973-74; Postmaster on Ross Island, summers 1979-80, 1981–82, and 1983–84. Pönui Nunatak. A nunatak located southeast of Slattery Peak and southwest of The Knoll.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The name Ponui (meaning south wind) is one of several Maori wind names applied by New Zealand Geographic Board (NZGB) in this vicinity. Conical Hill. A small but distinctive rock hill, high, on the south slopes of Mount Terror, above Cape MacKay. Given this descriptive name by the British Antarctic Expedition, 1910–13, under Scott.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Tent Peak. A tent-shaped peak rising to about high midway between Mount Terror and Cape Crozier. It was descriptively named by a party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1958–59, which occupied the peak as an astronomical control station, January 5, 1959, and erected a tent below the peak. The Tooth.

Geographic entities mentioned:
surface_form: tent
instance_of: Mountain
coordinates: lat: -67.6
lon: -65.35
The Tooth. A distinctive rock outcrop on the eastern slopes of Mount Terror at an elevation of about. The feature lies south-southeast of Tent Peak and is reported to resemble a fossilized shark's tooth. Descriptively named by a party of the NZGSAE, 1958–59, working in eastern Ross Island. Slattery Peak.

Geographic entities mentioned:
surface_form: tent
instance_of: Mountain
coordinates: lat: -67.6
lon: -65.35
The feature rises to about. Named by Advisory Committee on Antarctic Names (US-ACAN) (2000) after Alexander L. Sutherland, Jr., Ocean Projects Manager, OPP, NSF, with responsibility for directing operations and logistics for United States Antarctic Project (USAP) research vessels from 1989; responsible for acquisition of the Research Vessel/Ice Breakers Nathaniel B. Palmer and Laurence M. Gould.

Geographic entities mentioned:
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Slievemore. Slievemore () is the second highest peak on Achill Island after Croaghaun, in County Mayo, Ireland. Its elevation is 671 m (2,201 ft). Archaeology. In 1991, the Achill Archaeological Field School was opened. That year, the Deserted Village Project was created to perform archaeology excavations in Slievemore.

Geographic entities mentioned:
surface_form: Croaghaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.981
lon: -10.204
surface_form: slievemore
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.00905
lon: -10.059938888889
surface_form: croaghaun
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.6636
lon: -6.7675
Slievemore. Slievemore () is the second highest peak on Achill Island after Croaghaun, in County Mayo, Ireland. Its elevation is 671 m (2,201 ft). Archaeology. In 1991, the Achill Archaeological Field School was opened. That year, the Deserted Village Project was created to perform archaeology excavations in Slievemore.

Geographic entities mentioned:
surface_form: slievemore
instance_of: Mountain
countries: Ireland
coordinates: lat: 54.00905
lon: -10.059938888889
It was built of fieldstone in a Colonial Revival style in 1941. Architects in the Hudson Valley, and particularly Dutchess County, took inspiration from then-President Franklin D. Roosevelt's efforts to revive its use in the region, following the example of the early Dutch settlers of the area, who built many stone houses for themselves.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
It later evolved into Yazidism. Origins. The Adawiyya order was founded by Sheikh Adi ibn Musafir. Adi ibn Musafir was of an Arab descent from the Umayyad dynasty, born around 1075 in a village known as Bait Far, near Baalbek in the Beqaa Valley in Lebanon. From his remote village, he travelled to Baghdad to study Sufism.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Board Branch. Board Branch is a stream in Shelby County in the U.S. state of Missouri. It is a tributary of Tiger Fork. Board Branch was so named for the board trees near its course which supplied sawmills.

Geographic entities mentioned:
surface_form: tiger fork
instance_of: Watercourse
countries: United States
coordinates: lat: 39.848097
lon: -91.861
Board Branch. Board Branch is a stream in Shelby County in the U.S. state of Missouri. It is a tributary of Tiger Fork. Board Branch was so named for the board trees near its course which supplied sawmills.

Geographic entities mentioned:
surface_form: board branch
instance_of: Watercourse
countries: United States
coordinates: lat: 39.9086522
lon: -91.9390594
Campuses of the University of Hong Kong. The University of Hong Kong's main campus covers of land on Pok Fu Lam Road and Bonham Road in Lung Fu Shan of Central and Western District, Hong Kong Island. The university also has a few buildings in Sandy Bay Gap. HKU buildings are some of the few remaining examples of British colonial architecture in Hong Kong.

Geographic entities mentioned:
surface_form: Lung Fu Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.27993333
lon: 114.13504167
The university also has a few buildings in Sandy Bay Gap. HKU buildings are some of the few remaining examples of British colonial architecture in Hong Kong. The university lends its name to HKU station, the main public transport access to the campus (and the Lung Fu Shan and Shek Tong Tsui neighbourhoods), opened on 28 December 2014.

Geographic entities mentioned:
surface_form: Lung Fu Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.27993333
lon: 114.13504167
Mylochromis anaphyrmus. &quot;Mylochromis anaphyrmus&quot; is a species of cichlid endemic to Lake Malawi where it can be found at depths of around in waters with sandy substrates. This species can reach a length of TL. This species can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Lago Fagnano. Lago Fagnano (named after the Salesian monk José Fagnano), also known as Cami Lake, the southernmost lake of its size outside Antarctica, is the largest lake in Tierra del Fuego and flows southward along the eastern slope of the Andean Cordillera of Patagonia into the Magellan Strait through the Azopardo River.

Geographic entities mentioned:
surface_form: Lago Fagnano
instance_of: Lake
countries: Chile
Argentina
coordinates: lat: -54.543333333333
lon: -67.983333333333
After Baosi entered the royal palace, King You deposed Queen Shen (申后) and her son Crown Prince Yijiu, replacing them with Baosi and Bofu. King You and Bofu were both killed in 771 BCE by Quanrong nomads at Mount Li near Xi'an in present-day Shaanxi. Another source says that Bofu lived and contended for the throne with Queen Shen's son, King Ping of Zhou.

Geographic entities mentioned:
surface_form: Mount Li
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 34.358686111111
lon: 109.21048611111
Kirigalpoththa. Kirigalpoththa is the second-tallest mountain in Sri Lanka at above mean sea level, and is also the highest mountain in the country whose summit is accessible to the general public (the highest point, Pidurutalagala, is occupied by a military base and off-limits to the public). The peak is situated near the city of Nuwara Eliya, within the Nuwara Eliya District.

Geographic entities mentioned:
surface_form: Pidurutalagala
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 7.0008333333333335
lon: 80.77388888888889
surface_form: kirigalpoththa
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.79916667
lon: 80.76666667
Kirigalpoththa. Kirigalpoththa is the second-tallest mountain in Sri Lanka at above mean sea level, and is also the highest mountain in the country whose summit is accessible to the general public (the highest point, Pidurutalagala, is occupied by a military base and off-limits to the public). The peak is situated near the city of Nuwara Eliya, within the Nuwara Eliya District.

Geographic entities mentioned:
surface_form: kirigalpoththa
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.79916667
lon: 80.76666667
The duties of a Renaissance architect included consideration of engineering concerns, so Ligorio engaged in these renovations during his time as the Architect of the Vatican. He is particularly remembered for his role in the restoration of the Acqua Vergine, an ancient Roman aqueduct. Its malfunction was forcing Roman citizens to use the unsanitary water of the Tiber River.

Geographic entities mentioned:
surface_form: Acqua Vergine
instance_of: Watercourse
countries: Italy
John Salong. John Dahmasing Salong (born 1966) is a member of the Parliament of Vanuatu from Ambrym as a member of the Land and Justice Party. He became Minister of Climate Change Adaptation, Meteorology and Geo-Hazards, Energy, Environment and Disaster Management in August 2024. He was Minister of Finance and Economic Management from November 2022 to August 2024.

Geographic entities mentioned:
surface_form: Ambrym
instance_of: Mountain
countries: Vanuatu
coordinates: lat: -16.333333333333
lon: 168.33333333333
Lake Babati. Lake Babati is a lake in Tanzania known for its population of hippos. Recent droughts have led to a drop in the number of sightings of hippos, causing concern for local hoteliers. The lake is located near Babati town, in the Babati Urban District of Manyara Region.

Geographic entities mentioned:
surface_form: manyara
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.5833333333333
lon: 35.833333333333
Lake Babati. Lake Babati is a lake in Tanzania known for its population of hippos. Recent droughts have led to a drop in the number of sightings of hippos, causing concern for local hoteliers. The lake is located near Babati town, in the Babati Urban District of Manyara Region.

Geographic entities mentioned:
surface_form: lake babati
instance_of: Lake
countries: Tanzania
coordinates: lat: -4.25
lon: 35.73333333
Lesser Slave Lake Provincial Park is a provincial park and birdwatching area located in north-central Alberta, Canada. The park is located on the northeastern shore of the Lesser Slave Lake (while Hilliard's Bay Provincial Park, &quot;Lesser Slave Lake Wildland&quot; and &quot;Grouard Trail Park Reserve&quot; stand on the northwestern shore), north from the town of Slave Lake on Highway 88.

Geographic entities mentioned:
surface_form: Lesser Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.440556
lon: -115.488611
For convenience, storms are included that affected the Yemeni island of Socotra. Most of the tropical cyclones originated in the Arabian Sea, the portion of the Indian Ocean north of the equator and west of India. The remainder formed in the Bay of Bengal off India's east coast. Collectively, the 64 storms have caused at least US$8.3 billion in damage and 1,693 deaths.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
He was the first chancellor of the University of California, Berkeley, and twelfth president of the University of California. Early life and education. Kerr was born in Stony Creek, Pennsylvania, to Samuel William and Caroline (Clark) Kerr. He was raised on rural farms outside of Reading, Pennsylvania, first in the Stony Creek area and then in the Oley Valley after age 10.

Geographic entities mentioned:
surface_form: Oley Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.383
lon: -75.776
Allen Academy is an independent co-educational day school located in Bryan, Texas that was founded in 1886 by John H. and Rivers O. Allen. The campus is located northeast of Texas A&M University and enrolls about 340 students from throughout the Brazos Valley. The school is the oldest private school in the state of Texas and is a non-denominational pre-kindergarten through grade 12 school.

Geographic entities mentioned:
surface_form: Brazos Valley
instance_of: Valley
countries: United States
coordinates: lat: 30.66
lon: -96.3