Sarmila/GeoWiki-Features huggingface dataset:
There are two marked routes around Seefin: a shorter route to the west of the mountain via Windy Gap or a longer route to the east above Lough Caragh and overlooking Dingle Bay. The Way then climbs and follows the hills overlooking Dingle Bay until it reaches Drung Hill, where it turns inland to Foilmore. An linking spur provides a connection from Foilmore to Cahersiveen.

Geographic entities mentioned:
surface_form: Drung Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.026666666667
lon: -10.036388888889
Geography. Mount Bird was originally a separate island, which through volcanic activity has become a rounded peninsula on the northwestern tip of Ross Island. At its southernmost point, where it is connected with the rest of the island by a wide isthmus, a high pass, Bird Pass, separates the bulk of Mount Bird from the northern slopes of Mount Erebus.

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: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Named by New Zealand Geographic Board (NZGB), 2000. Bird Saddle. The feature is one of three prominent snow saddles on Ross Island, this one at about high between Mount Bird and Mount Erebus. Named in association with Mount Bird, which rises to high to the north of this saddle. Coastal features.

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: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
(Harry) Keys, New Zealand geochemist who worked several seasons during the 1970s and 1980s under the auspices of NZAP and United States Antarctic Research Program (USARP) on investigations as to the origin of salts in the McMurdo Sound area, the Mount Erebus volcano, and the quantity, shapes, and sizes of icebergs in the Antarctic marine environment. Harrison Bluff.

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
Cape Bird. Cape which marks the north extremity of Ross Island. Discovered in
1841 by a British expedition under Ross, and named by him for Lieutenant
Edward J. Bird of the ship Erebus. Beaufort Island. An island in the Ross Sea, the northernmost feature of the Ross Archipelago, lying north of Cape Bird.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
In association with the names of expedition ships grouped on this island, named after HMNZS Endeavour, tanker/supply ship which for at least 10 seasons, 1962-63 to 1971-72, transported bulk petroleum products and cargo to Scott Base and McMurdo Station on Ross Island. Takahe Nunatak. The northern of two similar nunataks that lie apart and north-northeast of Mount Bird in northwest Ross Island.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
Kakapo Nunatak. The southern of two similar nunataks that lie apart and north-northeast of Mount Bird in northwest Ross Island. It rises to about high and, like Takahe Nunatak close NE, appears to be part of an ice-covered crater rim. Kakapo Nunatak is one of several features near Mount Bird assigned the native name of a New Zealand mountain bird.

Geographic entities mentioned:
surface_form: takahe
instance_of: Mountain
coordinates: lat: -76.3
lon: -112.1
Mount Bird. Mount Bird () is a high shield volcano standing about south of Cape Bird, the northern extremity of Ross Island. It was mapped by the British National Antarctic Expedition, 1901–04, under Robert Falcon Scott, and apparently named by them after Cape Bird. Geography.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Geography. Mount Bird was originally a separate island, which through volcanic activity has become a rounded peninsula on the northwestern tip of Ross Island. At its southernmost point, where it is connected with the rest of the island by a wide isthmus, a high pass, Bird Pass, separates the bulk of Mount Bird from the northern slopes of Mount Erebus.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
The peninsula is flanked to the west and east by two large and frequently ice-bound bays, Wohlschlag Bay in the west and Lewis Bay in the east. Geology. Mount Bird is a basaltic shield volcano that was active from 4.6 to 3.8 million years ago. On the flanks of the volcano there are poorly exposed basalt scoria cones, and phonolite domes and flows.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Glaciers and streams. Several glaciers or meltwater streams flow from the mountain to the sea. Fitzgerald Stream. A stream between Fitzgerald Hill and Inclusion Hill on the lower ice-free west slopes of Mount Bird, flowing to McMurdo Sound across McDonald Beach. Explored by the NZGSAE, 1958-59, and named by the NZ-APC for E.B. Fitzgerald, deputy leader of the expedition. Shell Glacier.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Explored by the NZGSAE, 1958-59, and named by the NZ-APC for E.B. Fitzgerald, deputy leader of the expedition. Shell Glacier. A western lobe of the Mount Bird icecap. It descends steeply in the valley north of Trachyte Hill and Harrison Bluff in the center of the ice-free area on the lower western slopes of Mount Bird.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Shell Glacier. A western lobe of the Mount Bird icecap. It descends steeply in the valley north of Trachyte Hill and Harrison Bluff in the center of the ice-free area on the lower western slopes of Mount Bird. Mapped and so named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1958–59, because of the marine shell content of the moraines. Harrison Stream.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Harrison, mountaineer-assistant with the expedition. Wilson Stream. A meltwater stream which flows from the ice-free lower west slopes of Mount Bird, to the south of Alexander Hill, and over steep sea cliffs into Wohlschlag Bay. Mapped by the NZGSAE, 1958-59, and named by the NZ-APC for J. Wilson, mountaineer assistant with the expedition. Quaternary Icefall.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Wilson, mountaineer assistant with the expedition. Quaternary Icefall. A western lobe of the Mount Bird icecap, descending steeply into Wohlschlag Bay south of Cinder Hill. Mapped and so named by the NZGSAE, 1958-59, because of the Quaternary glacial period marine shells carried by the glacier and deposited in terminal moraines. Endeavour Piedmont Glacier.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Endeavour Piedmont Glacier. A piedmont glacier, long and wide, between the southwest part of Mount Bird and Micou Point. In association with the names of expedition ships grouped on this island, named after HMNZS Endeavour, tanker/supply ship which for at least 10 seasons, 1962-63 to 1971-72, transported bulk petroleum products and cargo to Scott Base and McMurdo Station on Ross Island.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Takahe Nunatak. The northern of two similar nunataks that lie apart and north-northeast of Mount Bird in northwest Ross Island. It rises to about high and, like Kakapo Nunatak is one of several features near Mount Bird assigned the native name of a New Zealand mountain bird. Named by New Zealand Geographic Board (NZGB), 2000. Kakapo Nunatak.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Named by New Zealand Geographic Board (NZGB), 2000. Kakapo Nunatak. The southern of two similar nunataks that lie apart and north-northeast of Mount Bird in northwest Ross Island. It rises to about high and, like Takahe Nunatak close NE, appears to be part of an ice-covered crater rim.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
The southern of two similar nunataks that lie apart and north-northeast of Mount Bird in northwest Ross Island. It rises to about high and, like Takahe Nunatak close NE, appears to be part of an ice-covered crater rim. Kakapo Nunatak is one of several features near Mount Bird assigned the native name of a New Zealand mountain bird. Named by New Zealand Geographic Board (NZGB), 2000. Norman Crag.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Kakapo Nunatak is one of several features near Mount Bird assigned the native name of a New Zealand mountain bird. Named by New Zealand Geographic Board (NZGB), 2000. Norman Crag. A rugged nunatak north of the summit of Mount Bird. The feature has a divided summit area and rises to over. Named by New Zealand Geographic Board (NZGB) (2000) after Bob Norman. Ruru Crests.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
The feature has a divided summit area and rises to over. Named by New Zealand Geographic Board (NZGB) (2000) after Bob Norman. Ruru Crests. Two parallel rock ridges northwest of the summit of Mount Bird. The feature rises to about. It is one of several landmarks near Mount Bird assigned the native name of a New Zealand mountain bird. Named by New Zealand Geographic Board (NZGB), 2000. Nash Peak.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Ruru Crests. Two parallel rock ridges northwest of the summit of Mount Bird. The feature rises to about. It is one of several landmarks near Mount Bird assigned the native name of a New Zealand mountain bird. Named by New Zealand Geographic Board (NZGB), 2000. Nash Peak. A prominent peak north of the Mount Bird summit in northwest Ross Island.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Named by New Zealand Geographic Board (NZGB), 2000. Nash Peak. A prominent peak north of the Mount Bird summit in northwest Ross Island. Named by the New Zealand Geographic Board (NZGB) (2000) after Sir Walter Nash, who was deeply involved in promoting New Zealand's role in Antarctica and who signed the Antarctic Treaty for New Zealand as Prime Minister. Wong Peak.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Named by the New Zealand Geographic Board (NZGB) (2000) after Sir Walter Nash, who was deeply involved in promoting New Zealand's role in Antarctica and who signed the Antarctic Treaty for New Zealand as Prime Minister. Wong Peak. A peak northeast of the summit of Mount Bird in northwest Ross Island. Named by New Zealand Geographic Board (NZGB) (2000) after Frank Wong. Beeby Peak.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Wong Peak. A peak northeast of the summit of Mount Bird in northwest Ross Island. Named by New Zealand Geographic Board (NZGB) (2000) after Frank Wong. Beeby Peak. A peak east-northeast of the summit of Mount Bird in northwest Ross Island. The feature rises to about. Named by New Zealand Geographic Board (NZGB) (2000) after Chris Beeby. Western Features.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
The feature rises to about. Named by New Zealand Geographic Board (NZGB) (2000) after Chris Beeby. Western Features. Features near the coast to the west of Mount Bird include, from north to south,
Inclusion Hill. A prominent steeply conical hill, high, between McDonald Beach and the Mount Bird icecap. It is a trachyte plug, in parts containing numerous inclusions of basalt.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Western Features. Features near the coast to the west of Mount Bird include, from north to south,
Inclusion Hill. A prominent steeply conical hill, high, between McDonald Beach and the Mount Bird icecap. It is a trachyte plug, in parts containing numerous inclusions of basalt. Explored and descriptively named by the NZGSAE, 1958-59. Fitzgerald Hill.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
It is a trachyte plug, in parts containing numerous inclusions of basalt. Explored and descriptively named by the NZGSAE, 1958-59. Fitzgerald Hill. A hill, high, standing west of Mount Bird between Fitzgerald Stream and Shell Glacier. Mapped by the NZGSAE, 1958-59, and named by the NZ-APC for E.B. Fitzgerald, deputy leader of the expedition. Cinder Hill.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Fitzgerald, deputy leader of the expedition. Cinder Hill. A prominent dissected volcano, high, consisting of layers of red basalt scoria and cinders and abundant olivine nodules, standing between Harrison Stream and Wilson Stream on the ice-free lower west slopes of Mount Bird. Mapped and descriptively named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1958-59.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Mapped and descriptively named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1958-59. Alexander Hill. A hill, high, with a prominent seaward cliff face, lying south of Harrison Stream and Cinder Hill on the lower ice-free west slopes of Mount Bird. Mapped by the NZGSAE, 1958-59, and named by the NZ-APC for B.N. Alexander, a surveyor with the expedition. Trachyte Hill.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Mapped by the NZGSAE, 1958-59, and named by the NZ-APC for B.N. Alexander, a surveyor with the expedition. Trachyte Hill. A prominent hill, high, just south of Shell Glacier in the center of the ice-free area on the lower west slopes of Mount Bird. Mapped and so named by the NZGSAE, 1958-59, because of the rock type composing the hill. Keys Hill.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Mapped and so named by the NZGSAE, 1958-59, because of the rock type composing the hill. Keys Hill. A hill, high, located at the head of Shearwater Glacier, west-southwest of the summit of Mount Bird in northwest Ross Island. Named by New Zealand Geographic Board (NZGB) (2000) after Gordon Keys, leader of long term NZAP atmospheric research, 1985-95. Palais Bluff.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
student at Ohio State University, collected snow samples and short ice core on Ross Island to examine the volcanic record. She has made many trips to Antarctica. Kea Nunataks. A line of several nunataks southeast of the summit of Mount Bird. The feature trends NW-SE and is long. Kea Nunataks is one of several features near Mount Bird assigned the native name of a New Zealand mountain bird.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Kea Nunataks. A line of several nunataks southeast of the summit of Mount Bird. The feature trends NW-SE and is long. Kea Nunataks is one of several features near Mount Bird assigned the native name of a New Zealand mountain bird. Named by New Zealand Geographic Board (NZGB), 2000. Kaka Nunatak. The most prominent of the Kea Nunataks, rising to about high near the center of the group.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Named by New Zealand Geographic Board (NZGB), 2000. Kaka Nunatak. The most prominent of the Kea Nunataks, rising to about high near the center of the group. It stands southeast of the summit of Mount Bird in northwest Ross Island. Kaka Nunatak is one of several features near Mount Bird assigned the native name of a New Zealand mountain bird. Named by New Zealand Geographic Board (NZGB), 2000.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Kaka Nunatak. The most prominent of the Kea Nunataks, rising to about high near the center of the group. It stands southeast of the summit of Mount Bird in northwest Ross Island. Kaka Nunatak is one of several features near Mount Bird assigned the native name of a New Zealand mountain bird. Named by New Zealand Geographic Board (NZGB), 2000. Bird Saddle.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Bird Saddle. The feature is one of three prominent snow saddles on Ross Island, this one at about high between Mount Bird and Mount Erebus. Named in association with Mount Bird, which rises to high to the north of this saddle. Coastal features. Coastal features around Mount Bird include Romanes Beach, McDonald Beach, Caughley Beach, Cape Bird Hut and Cape Bird. Romanes Beach.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Named in association with Mount Bird, which rises to high to the north of this saddle. Coastal features. Coastal features around Mount Bird include Romanes Beach, McDonald Beach, Caughley Beach, Cape Bird Hut and Cape Bird. Romanes Beach. Beach on the north shore of Wohlschlag Bay just south of Harrison Bluff. Mapped by a party of the NZGSAE, 1958-59, landed there by the USS Arneb.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
Harrison Bluff. A pale-colored trachyte headland forming the seaward termination of Trachyte Hill and marking the southern end of McDonald Beach on the western side of Mount Bird. Many skuas nest on the bluff. A survey station marked by a rock cairn was placed on the top of the northwest corner of the bluff by E.B. Fitzgerald of the Cape Bird Party of the NZGSAE, 1958-59.

Geographic entities mentioned:
surface_form: mount bird
instance_of: Mountain
coordinates: lat: -77.266666666667
lon: 166.75
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Mapped and so named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1958–59, because of the marine shell content of the moraines. Harrison Stream. A small stream flowing west between Trachyte and Cinder Hills to the north end of Romanes Beach. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for J. Harrison, mountaineer-assistant with the expedition.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
While visiting Imatra, he painted The Tower&quot;’ (NAMU) and ‘&quot;A Castle in Finland’&quot; (collection of K.Grygoryshyn), both depicting the famous architectural marvel of Grand Hotel de Cascade (now Valtionhotelli). The hotel was built in the form of a castle in Art Nouveau style and is reminiscent of Olavinlinna fortress situated on the other side of Lake Saimaa.

Geographic entities mentioned:
surface_form: Saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
The trip yielded a number of romantic, &quot;White Night&quot; drawings and watercolours of scenic highlights near Vyborg – including Monrepos Park, the three-towered Olavinlinna Castle in Savonlinna, and the island-dotted Lake Saimaa, whose ‘fairy-tale beauty’ had been extolled by numerous artists and poets.

Geographic entities mentioned:
surface_form: Saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
Sunol Valley. Sunol Valley () is located in Alameda County, California, United States. The small town of Sunol lies in the valley. It is largely rural, but is in proximity to the highly populated Bay Area suburbs of Fremont, Pleasanton, and Livermore. Description. Interstate 680 runs through the valley. The historic Sunol Water Temple is situated in the Sunol Valley.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
It is largely rural, but is in proximity to the highly populated Bay Area suburbs of Fremont, Pleasanton, and Livermore. Description. Interstate 680 runs through the valley. The historic Sunol Water Temple is situated in the Sunol Valley. Historically steelhead have run as high as the Sunol Valley via Alameda Creek, and restoration plans are underway to restore such anadromous fish runs.

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
Sunol Valley. Sunol Valley () is located in Alameda County, California, United States. The small town of Sunol lies in the valley. It is largely rural, but is in proximity to the highly populated Bay Area suburbs of Fremont, Pleasanton, and Livermore. Description. Interstate 680 runs through the valley. The historic Sunol Water Temple is situated in the Sunol Valley.

Geographic entities mentioned:
surface_form: sunol valley
instance_of: Valley
countries: United States
coordinates: lat: 37.5948
lon: -121.887
It is largely rural, but is in proximity to the highly populated Bay Area suburbs of Fremont, Pleasanton, and Livermore. Description. Interstate 680 runs through the valley. The historic Sunol Water Temple is situated in the Sunol Valley. Historically steelhead have run as high as the Sunol Valley via Alameda Creek, and restoration plans are underway to restore such anadromous fish runs.

Geographic entities mentioned:
surface_form: sunol valley
instance_of: Valley
countries: United States
coordinates: lat: 37.5948
lon: -121.887
Historically steelhead have run as high as the Sunol Valley via Alameda Creek, and restoration plans are underway to restore such anadromous fish runs. These restoration plans by the San Francisco Public Utilities Commission include the planned modification of a Pacific Gas and Electric pipeline that has blocked fish migration in Alameda Creek. Sunol Valley Quarry.

Geographic entities mentioned:
surface_form: sunol valley
instance_of: Valley
countries: United States
coordinates: lat: 37.5948
lon: -121.887
Sunol Valley Quarry. The Sunol Valley Rock Quarry is located within the Sunol Valley; this facility has been used as the source for fill material in a considerable amount of the land development for neighboring communities. In the course of excavating this quarry for such fill, chemical analysis has been conducted to ascertain the safety of such soils.

Geographic entities mentioned:
surface_form: sunol valley
instance_of: Valley
countries: United States
coordinates: lat: 37.5948
lon: -121.887
surface_form: sunol valley
instance_of: Valley
countries: United States
coordinates: lat: 37.5948
lon: -121.887
On the first day of the festival, images of Vishvaksena and Hanuman are paraded to the shrine of Ranganayaki, the presiding consort goddess of the temple. Soil from a holy bael tree and from the banks of the Kaveri river are brought by priests, as though collected by the deities and seeds are sown in this soil as part of the &quot;Ankurarpanam&quot; (sprouting the seeds) ritual.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Collection records for the cylindrical lioplax exist from the Alabama River (Dallas County, Alabama), Black Warrior River (Jefferson County, Alabama) and tributaries (Prairie Creek, Marengo County, Alabama; Valley Creek, Jefferson County, Alabama); Coosa River (Shelby, Elmore counties, Alabama) and tributaries (Oothcalooga Creek, Bartow County, Georgia; CoahuIla Creek, Whitfield County, Georgia; Annuchee Creek, Floyd County, Georgia; Little Wills Creek, Etowah County, Alabama; Choccolocco Creek, Talladega County, Alabama; Yellowleaf Creek, Shelby County, Alabama); and the Cahaba River (Bibb, Shelby counties, Alabama) and its tributary, Little Cahaba River (Jefferson County, Alabama).

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
Lake Sandoval. Lake Sandoval is an oxbow lake in the Amazon basin. It's located in the Department of Madre de Dios in southeastern Peru, about from the city of Puerto Maldonado. It is a part of the Tambopata Candamo Reserved Zone. Lake Sandoval is one of the largest oxbow lakes in southeastern Peru, with a surface area of about.

Geographic entities mentioned:
surface_form: lake sandoval
instance_of: Lake
countries: Peru
coordinates: lat: -12.605547222222
lon: -69.041886111111
It is a part of the Tambopata Candamo Reserved Zone. Lake Sandoval is one of the largest oxbow lakes in southeastern Peru, with a surface area of about. It is one of the most popular tourist destinations in the Madre de Dios region, particularly for ecotourism, and it is also a popular site for research purposes. There is a touristic hike from the river Madre de Dios to the lake.

Geographic entities mentioned:
surface_form: lake sandoval
instance_of: Lake
countries: Peru
coordinates: lat: -12.605547222222
lon: -69.041886111111
An aquaculture facility near the lake cultivated arapaima (&quot;Arapaima gigas&quot;) and other species in the 1970s. In 1979, flooding of the Madre de Dios River led to the escape of about 1,000 arapaima fry into Lake Sandoval, and the larger Madre de Dios River watershed, when rising waters reached the aquaculture ponds they were contained in.

Geographic entities mentioned:
surface_form: lake sandoval
instance_of: Lake
countries: Peru
coordinates: lat: -12.605547222222
lon: -69.041886111111
In 1998, in light of negative impacts caused by increasing human activity near the lake, the National Institute for Natural Resources (INRENA) requested assistance from the IUCN's Giant Otter Project in the development of a giant otter tourism management plan for Lake Sandoval and the larger Tambopata Candamo Reserved Zone.

Geographic entities mentioned:
surface_form: lake sandoval
instance_of: Lake
countries: Peru
coordinates: lat: -12.605547222222
lon: -69.041886111111
Gold rush. The discovery of gold in 1851 at Yreka (and throughout Siskiyou and Trinity counties) brought the California Gold Rush-era prospectors up the rivers of the region in search of gold, leading to the first non-Native American settlements in the area, including at Old Shasta, Portuguese Flat, Upper Soda Springs, Weaverville, and Yreka itself. Geography.

Geographic entities mentioned:
surface_form: Upper Soda Springs
instance_of: Landform
countries: United States
coordinates: lat: 41.2219
lon: -122.277
Numerous parks and recreation opportunities fill the area including Shasta Lake, Lake Siskiyou, Castle Crags State Park, a new park at Upper Soda Springs, the Trinity Alps, Lava Beds National Monument, Clair Engle Lake, Castle Lake, Lassen Volcanic National Park, Caribou Wilderness, Thousand Lakes Wilderness, and climbing Mount Shasta. Metropolitan areas.

Geographic entities mentioned:
surface_form: Upper Soda Springs
instance_of: Landform
countries: United States
coordinates: lat: 41.2219
lon: -122.277
Whiteside Mountain has the highest cliffs in Eastern North America. It also has a feature called Devil's Courthouse (distinct from the Devil's Courthouse 20 miles away in Transylvania County, NC). Since the 1980s, the forest service has tried to restrict access to the Courthouse and has allowed the foot trail to it to grow over because of dangers such as strong winds.

Geographic entities mentioned:
surface_form: Devil's Courthouse
instance_of: Mountain
countries: United States
coordinates: lat: 35.3025
lon: -82.8956
surface_form: devil's courthouse
instance_of: Mountain
countries: United States
coordinates: lat: 35.3025
lon: -82.8956
Whiteside Mountain. Whiteside Mountain or Sanigilâ'gĭ  in Cherokee is a mountain in Jackson County, North Carolina between Cashiers, Highlands, North Carolina, and the Georgia border. Whiteside Mountain has the highest cliffs in Eastern North America. It also has a feature called Devil's Courthouse (distinct from the Devil's Courthouse 20 miles away in Transylvania County, NC).

Geographic entities mentioned:
surface_form: whiteside mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.0809
lon: -83.1382
Whiteside Mountain. Whiteside Mountain or Sanigilâ'gĭ  in Cherokee is a mountain in Jackson County, North Carolina between Cashiers, Highlands, North Carolina, and the Georgia border. Whiteside Mountain has the highest cliffs in Eastern North America. It also has a feature called Devil's Courthouse (distinct from the Devil's Courthouse 20 miles away in Transylvania County, NC).

Geographic entities mentioned:
surface_form: whiteside mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.0809
lon: -83.1382
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
There is also an overhang, a small platform less than 7 feet in diameter, connected to Whiteside as if it were a cantilever. Similar overhangs can be found on the Appalachian Trail. History. The Cherokee name for Whiteside mountain is Sanigilâ'gĭ. Legend of Spear Finger. Cherokee myth says that Spear-finger, the powerful woman monster, built a bridge from the Hiwassee River to Whiteside Mountain.

Geographic entities mentioned:
surface_form: whiteside mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.0809
lon: -83.1382
Similar overhangs can be found on the Appalachian Trail. History. The Cherokee name for Whiteside mountain is Sanigilâ'gĭ. Legend of Spear Finger. Cherokee myth says that Spear-finger, the powerful woman monster, built a bridge from the Hiwassee River to Whiteside Mountain. Legend of De Soto.

Geographic entities mentioned:
surface_form: whiteside mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.0809
lon: -83.1382
Since the terrain is too rough for men and horses to get through, for De Soto to have come through here at a time when there were no roads or pathways is unlikely. De Soto's route most likely took him through the Cumberland Gap from South Carolina. Inscription Update - Nov. 18, 2021 The inscription actually reads, &quot;T.T.&quot; Un luego Santa a la memoria&quot; In 1946, Rev.

Geographic entities mentioned:
surface_form: cumberland
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
state of Alaska. Description. The mountain is situated 13 miles north of Sukakpak Mountain, 100 miles north of the Arctic Circle, and 200 miles north-northwest of Fairbanks. The peak lies along the east side of the Dietrich River valley, and can be seen from the Dalton Highway which traverses the valley. Topographic relief is significant as the summit rises above the river in two miles.

Geographic entities mentioned:
surface_form: Sukakpak Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 67.60417
lon: -149.74194
Snowden Mountain. Snowden Mountain is a mountain summit located in the Brooks Range, in the U.S. state of Alaska. Description. The mountain is situated 13 miles north of Sukakpak Mountain, 100 miles north of the Arctic Circle, and 200 miles north-northwest of Fairbanks.

Geographic entities mentioned:
surface_form: snowden mountain
instance_of: Mountain
countries: United States
coordinates: lat: 67.79806
lon: -149.69389
Topographic relief is significant as the summit rises above the river in two miles. The peak is set in the Snowden Mountain Area of Critical Environmental Concern, which is managed by the Bureau of Land Management. This ACEC is extremely rugged and was established to protect Dall sheep habitat on the southern slope of the Brooks Range.

Geographic entities mentioned:
surface_form: snowden mountain
instance_of: Mountain
countries: United States
coordinates: lat: 67.79806
lon: -149.69389
The name has been officially adopted by the U.S. Board on Geographic Names. Climate. Based on the Köppen climate classification, Snowden Mountain is located in a subarctic climate zone with long, cold, winters, and short, cool summers. Winter temperatures can drop below −30 °F with wind chill factors below −50 °F. Precipitation runoff from the mountain drains west into the Dietrich River.

Geographic entities mentioned:
surface_form: snowden mountain
instance_of: Mountain
countries: United States
coordinates: lat: 67.79806
lon: -149.69389
Early in its career the CAWIU involved itself primarily in spontaneous agricultural strikes, including the Santa Clara Valley cannery workers strike in July 1931 and the California pea pickers strike in May 1932. However, the union focused little on recruiting and organizing a large group of permanent members.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
It has a length of, and a catchment area of, with water supplied by melting snow. In the summer the water is brackish. Course. The river originates in lake Karachinsky and flows northwards along the Turgay Depression. In the upper reaches it flows through lake Kushmurun. The river empties into the right bank of the Tobol from its mouth. History.

Geographic entities mentioned:
surface_form: Turgay Depression
instance_of: Valley
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 52
lon: 64.5
It has a length of, and a catchment area of, with water supplied by melting snow. In the summer the water is brackish. Course. The river originates in lake Karachinsky and flows northwards along the Turgay Depression. In the upper reaches it flows through lake Kushmurun. The river empties into the right bank of the Tobol from its mouth. History.

Geographic entities mentioned:
surface_form: Kushmurun
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.683333333333
lon: 64.8
Causes of the disaster. Bangladesh's annual monsoon for 2007 started with unusually heavy rain, intensified by a storm from the Bay of Bengal on 9–10 June 2007. By 11 June, more than one-third of the southeastern coastal city of Chittagong was under water, reported the Australian Broadcasting Corporation.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Derryloughan, County Tyrone. Derryloughan is a townland in County Tyrone, Northern Ireland. It lies on the southwest corner of Lough Neagh, 4 miles from Coalisland. It is situated in the historic barony of Dungannon Middle and the civil parish of Clonoe and covers an area of 1751 acres. The name derives from the Irish: &quot;Doire Lochain&quot; (Oak wood of the little lough). Geography.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
Garabogazköl. Garabogazköl (also spelled Kara-Bogaz-Gol; &quot;Black Strait Lake&quot;), or Garabogazköl Aylagy (&quot;Black Strait Lake Bay&quot;), is a shallow, highly saline lagoon off the Caspian Sea in northwestern Turkmenistan. The lagoon has a variable surface area typically about. It is very shallow, with an average depth of 10 meters.

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
Ciste Dhubh. Ciste Dhubh is a mountain in the Scottish Highlands, between Glen Shiel and Glen Affric. With a height of, it is classed as a Munro. It is almost surrounded by glens: Fionngleann (north), An Caorann Mòr (east) and Allt Cam-bàn (west), with the Bealach a' Chòinich pass (south) linking it to the mountain of Sgùrr an Fhuarail.

Geographic entities mentioned:
surface_form: Glen Shiel
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.2103
lon: -5.4239
surface_form: Glen Affric
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.283333333333
lon: -4.9333333333333
surface_form: ciste dhubh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.199243
lon: -5.209016
The mountain also has ridges to the north west and north which descend to upper Glen Affric. There are two small corries on either side of the northern ridge. Ciste Dhubh falls to deep glens on all sides except to the south where the mountain is connected to the adjoining Munro of Aonach Meadhoin by a col with a height of 591 metres called the Bealach a’ Choinich (Pass of the Bog).

Geographic entities mentioned:
surface_form: Aonach Meadhoin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.173026
lon: -5.229182
surface_form: aonach meadhoin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.173026
lon: -5.229182
The mountains north, east and west flanks fall into deep valleys which contain the streams which form the head waters of the River Affric and takes water away north east to the Beauly Firth. Drainage from the southern slopes of the mountain goes south to Loch Cluanie and then east via the River Moriston and Loch Ness to the Moray Firth. Climbing.

Geographic entities mentioned:
surface_form: Loch Cluanie
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.13961
lon: -5.088876
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: loch cluanie
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.13961
lon: -5.088876
surface_form: ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: loch ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
The return to Loch Cluanie can include the adjoining Munro of Aonach Meadhoin, which is a ascent from the Bealach a’ Choinich. The view from the top of Ciste Dhubh is good: the mountain is surrounded by higher peaks but none of them are too close (Ciste Dhubh has a prominence of) and the nearby mountains of Mullach Fraoch-choire, A' Chràlaig and Sgurr nan Ceathreamhnan are well seen in detail.

Geographic entities mentioned:
surface_form: A' Chràlaig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.184186
lon: -5.154837
surface_form: sgurr nan ceathreamhnan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.255
lon: -5.2236111111111
surface_form: ciste dhubh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.199243
lon: -5.209016
surface_form: ciste dhubh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.199243
lon: -5.209016
surface_form: mullach fraoch-choire
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.205379
lon: -5.155652
surface_form: a' chràlaig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.184186
lon: -5.154837
Climbing. The most common ascent of Ciste Dhubh starts on the A87 road just east of the Cluanie Inn on the shores of Loch Cluanie at grid reference. From there it is a walk up the valley of the Allt a’ Chaorainn Bhig to reach the Bealach a’ Choinich; an alternative way of reaching this bealach is by climbing the Corbett of Am Bathach which stands to the east of the valley.

Geographic entities mentioned:
surface_form: loch cluanie
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.13961
lon: -5.088876
surface_form: ciste dhubh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.199243
lon: -5.209016
From the bealach it is a steep ascent up grassy slopes until the southern ridge is reached which is followed to Ciste Dhubh’s rocky summit. It is possible to ascend the mountain from the Alltbeithe youth hostel in upper Glen Affric by climbing the northern ridge. The return to Loch Cluanie can include the adjoining Munro of Aonach Meadhoin, which is a ascent from the Bealach a’ Choinich.

Geographic entities mentioned:
surface_form: glen affric
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.283333333333
lon: -4.9333333333333
The summit is precipitous and rocky, and the southern ridge is steep and in places quite narrow, it offers few dangers for walkers but care is needed in high winds or under winter conditions. The mountain also has ridges to the north west and north which descend to upper Glen Affric. There are two small corries on either side of the northern ridge.

Geographic entities mentioned:
surface_form: glen affric
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.283333333333
lon: -4.9333333333333
With a height of, it is classed as a Munro. It is almost surrounded by glens: Fionngleann (north), An Caorann Mòr (east) and Allt Cam-bàn (west), with the Bealach a' Chòinich pass (south) linking it to the mountain of Sgùrr an Fhuarail. Its name comes from Scottish Gaelic &quot;A' Chiste Dhubh&quot;, &quot;the black chest&quot;, possibly referring to the dark rocky summit. Landscape.

Geographic entities mentioned:
surface_form: a' chiste dhubh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.199243
lon: -5.209016
Ciste Dhubh. Ciste Dhubh is a mountain in the Scottish Highlands, between Glen Shiel and Glen Affric. With a height of, it is classed as a Munro. It is almost surrounded by glens: Fionngleann (north), An Caorann Mòr (east) and Allt Cam-bàn (west), with the Bealach a' Chòinich pass (south) linking it to the mountain of Sgùrr an Fhuarail.

Geographic entities mentioned:
surface_form: ciste dhubh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.199243
lon: -5.209016
This pass, which lives up to its translated name, is strategically important as it also connects to the adjacent Corbett of Am Bathach and is vital to the walker who wants to climb the mountain with either or both of these adjoining hills. All drainage from Ciste Dhubh finds its way to the east coast of Scotland over away.

Geographic entities mentioned:
surface_form: am bathach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.1788
lon: -5.189
From there it is a walk up the valley of the Allt a’ Chaorainn Bhig to reach the Bealach a’ Choinich; an alternative way of reaching this bealach is by climbing the Corbett of Am Bathach which stands to the east of the valley. From the bealach it is a steep ascent up grassy slopes until the southern ridge is reached which is followed to Ciste Dhubh’s rocky summit.

Geographic entities mentioned:
surface_form: ciste dhubh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.199243
lon: -5.209016
From the bealach it is a steep ascent up grassy slopes until the southern ridge is reached which is followed to Ciste Dhubh’s rocky summit. It is possible to ascend the mountain from the Alltbeithe youth hostel in upper Glen Affric by climbing the northern ridge. The return to Loch Cluanie can include the adjoining Munro of Aonach Meadhoin, which is a ascent from the Bealach a’ Choinich.

Geographic entities mentioned:
surface_form: aonach meadhoin
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.173026
lon: -5.229182
Climbing. The most common ascent of Ciste Dhubh starts on the A87 road just east of the Cluanie Inn on the shores of Loch Cluanie at grid reference. From there it is a walk up the valley of the Allt a’ Chaorainn Bhig to reach the Bealach a’ Choinich; an alternative way of reaching this bealach is by climbing the Corbett of Am Bathach which stands to the east of the valley.

Geographic entities mentioned:
surface_form: am bathach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.1788
lon: -5.189
In addition, he often painted figures, especially biblical and mythological, with a naive touch. Svalastoga probably had two working winters in Numedal, first 1801-1802 and then 1806–07. A major work is the living room interior at Nordigard Berdal in Vinje from 1802. In 1803, he also painted the altarpiece of the new church in Rauland (&quot;Rauland kyrkje&quot;).

Geographic entities mentioned:
surface_form: Numedal
instance_of: Valley
countries: Norway
coordinates: lat: 60
lon: 9.2
Nile minnow. The Nile minnow (&quot;Leptocypris niloticus&quot;) is a species of freshwater ray-finned fish belonging to the family Danionidae. This fish is found in the Nile, Omo, Niger, Bénoué, Volta, and Senegal Rivers, and the Lake Chad basin. It was described by Léon-Daniel de Joannis in 1835.

Geographic entities mentioned:
surface_form: Bénoué
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
Canto Alto. Canto Alto is a mountain of Lombardy, Italy. It is located within the Bergamo Alps.

Geographic entities mentioned:
surface_form: canto alto
instance_of: Mountain
countries: Italy
coordinates: lat: 45.77
lon: 9.67
Taxonomy. &quot;Sebastes rastrelliger&quot; was first formally described as &quot;Sebastichthys rastrelliger&quot; in 1880 by the American ichthyologists David Starr Jordan and Charles Henry Gilbert with the type locality given as Point Conception to Santa Catalina Island in California. Some authorities place this species in the subgenus &quot;Pteropodus&quot;.

Geographic entities mentioned:
surface_form: Point Conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
Plums, pears, and strawberries are also grown in Michigan. These fruits are mainly grown in West Michigan due to the moderating effect of Lake Michigan on the climate. There is also significant fruit production, especially cherries, but also grapes, apples, and other fruits, in Northwest Michigan along Lake Michigan. Michigan produces wines, beers and a multitude of processed food products.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
His first work was in southern India with H.F.Blanford. He then worked in central India and surveyed western Chota Nagpur and took over the position of director at Calcutta, succeeding Medlicott in 1887. He was given six extensions from the normal age of retirement at 54 thus retiring at the age of 60 on 16 July 1894 after 37 years of service.

Geographic entities mentioned:
surface_form: Chota Nagpur
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85