Sarmila/GeoWiki-Features huggingface dataset:
The peak is &quot;named after the Bulgarian scholar Chernorizets Hrabar (9th Century AD).&quot;
Location. The cliff is located at, which is 1.5 km east of Greaves Peak, 1.2 km west of Crutch Peaks, and 1.15 km south of Pavlikeni Point and 3.9 km north of Kerseblept Nunatak (Bulgarian topographic survey 05 and mapping in 2005 and 2009).

Geographic entities mentioned:
surface_form: Greaves Peak
instance_of: Mountain
coordinates: lat: -62.4542
lon: -59.9894
surface_form: Crutch Peaks
instance_of: Mountain
coordinates: lat: -62.4535
lon: -59.9375
surface_form: Kerseblept Nunatak
instance_of: Mountain
coordinates: lat: -62.487916666667
lon: -59.955
surface_form: crutch peaks
instance_of: Mountain
coordinates: lat: -62.4535
lon: -59.9375
surface_form: greaves peak
instance_of: Mountain
coordinates: lat: -62.4542
lon: -59.9894
surface_form: kerseblept nunatak
instance_of: Mountain
coordinates: lat: -62.487916666667
lon: -59.955
Hrabar Nunatak. Hrabar Nunatak (Nunatak Hrabar \'nu-na-tak 'hra-b&r\) is a 160m rocky peak on the north coast of Greenwich Island in the South Shetland Islands, Antarctica, and overlooking Yakoruda Glacier to the south. The peak is &quot;named after the Bulgarian scholar Chernorizets Hrabar (9th Century AD).&quot;
Location.

Geographic entities mentioned:
surface_form: nunatak hrabar
instance_of: Mountain
coordinates: lat: -62.452916666667
lon: -59.960555555556
surface_form: hrabar nunatak
instance_of: Mountain
coordinates: lat: -62.452916666667
lon: -59.960555555556
Hrabar Nunatak. Hrabar Nunatak (Nunatak Hrabar \'nu-na-tak 'hra-b&r\) is a 160m rocky peak on the north coast of Greenwich Island in the South Shetland Islands, Antarctica, and overlooking Yakoruda Glacier to the south. The peak is &quot;named after the Bulgarian scholar Chernorizets Hrabar (9th Century AD).&quot;
Location.

Geographic entities mentioned:
surface_form: hrabar nunatak
instance_of: Mountain
coordinates: lat: -62.452916666667
lon: -59.960555555556
It also fractured UPRONA, as his former lieutenants engaged in a power struggle to succeed him as the party's leader. Within Burundi, Rwagasore enjoys nearly universal acclaim, and his assassination is commemorated annually with large ceremonies. He remains relatively unknown internationally in comparison to other leaders of independence movements in the African Great Lakes region. Early life.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
He took virtual control over the movement, though his familial connection to the Mwami disqualified him from holding any party offices and he officially served UPRONA only as an advisor. UPRONA was able to secure the early financial support of the Swahili population in Bujumbura and Lake Tanganyika coastline.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Taylor Valley. Taylor Valley is an ice-free valley about long, once occupied by the receding Taylor Glacier. It lies north of the Kukri Hills between the Taylor Glacier and New Harbour in Victoria Land, Antarctica. Taylor Valley is the southernmost of the three large McMurdo Dry Valleys in the Transantarctic Mountains, located west of McMurdo Sound. Exploration and naming.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Location. Taylor Valley is one of the McMurdo Dry Valleys. Parts of the area were visited by British expeditions led by Captain Robert Falcon Scott (1901–04 and 1910–13), who referred to Taylor Valley, as well as Beacon Valley and Pyramid Trough (named later), as &quot;dry valleys.&quot;
It runs from the east end of Taylor Glacier to New Harbour in McMurdo Sound.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Location. Taylor Valley is one of the McMurdo Dry Valleys. Parts of the area were visited by British expeditions led by Captain Robert Falcon Scott (1901–04 and 1910–13), who referred to Taylor Valley, as well as Beacon Valley and Pyramid Trough (named later), as &quot;dry valleys.&quot;
It runs from the east end of Taylor Glacier to New Harbour in McMurdo Sound.

Geographic entities mentioned:
surface_form: Beacon Valley
instance_of: Valley
coordinates: lat: -77.8167
lon: 160.65
surface_form: Pyramid Trough
instance_of: Valley
coordinates: lat: -78.3
lon: 163.45
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
surface_form: pyramid
instance_of: Mountain
coordinates: lat: -78.35
lon: 163.5
Named after the Matterhorn by United States geologist T.L. Péwé, who visited the area in December 1957. Lacroix Glacier. Glacier between Suess and Matterhorn Glaciers, which flows southeast into Taylor Valley. Mapped by the BrAE under Scott, 1910–13, and named after Alfred Lacroix (see Mount Lacroix). Suess Glacier. Glacier between Canada and Lacroix Glaciers, flowing south into Taylor Valley.

Geographic entities mentioned:
surface_form: Mount Lacroix
instance_of: Mountain
coordinates: lat: -65.05
lon: -63.9667
surface_form: mount lacroix
instance_of: Mountain
coordinates: lat: -65.05
lon: -63.9667
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -65.05
lon: -63.9667
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -65.05
lon: -63.9667
surface_form: alfred
instance_of: Mountain
coordinates: lat: -70.31133
lon: -69.23369
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -66.85
lon: 141.333
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -66.85
lon: 141.333
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
A large number of solitary fossil corals have been found here by NZARP/USARP teams in the course of joint geological studies of the area. The name was suggested by Donald P. Elston, USGS, a research team member who worked at the ridge in the 1979–80 and 1980–81 seasons. Northern glaciers and streams.

Geographic entities mentioned:
surface_form: donald
instance_of: Mountain
coordinates: lat: -65.0833
lon: -60.1
Mummy Pond. A pond between Suess and Lacroix Glaciers. So named by T.L. Péwé, United States geologist who visited the area in December 1957, because of the mummified seals found around the pond. Lake Chad. Small lake lying east of the mouth of Suess Glacier. Charted and named by the BrAE under Scott, 1910–13, after the African lake of the same name. Spaulding Pond.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
Suess Glacier. Glacier between Canada and Lacroix Glaciers, flowing south into Taylor Valley. Charted and named by the BrAE under Scott, 1910–13, for Professor Eduard Suess, noted Austrian geologist and paleontologist. Canada Glacier. Small glacier flowing southeast into the north side of Taylor Valley immediately west of Lake Fryxell. Charted and named by the BrAE, 1910–13, under Scott.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The name was suggested by hydrologist Diane McKnight, leader of USGS teams that made intensive studies of the hydrology of
streams of the Lake Fryxell basin, 1987–94. Named after William J. Green of Miami University, Oxford, Ohio, who conducted research on the geochemistry of the Onyx River, 1980–81, and Lake Fryxell, Lake Hoare, and their feeder streams, 1982–83. Canada Stream.

Geographic entities mentioned:
surface_form: hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
surface_form: lake hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
The name was suggested by Diane McKnight, leader of a USGS team which made extensive studies of the hydrology and geochemistry of streams and ponds in the Lake Fryxell basin, 1987–94. Named after hydrologist Edward Furlong, a member of the field team that established stream gaging stations on streams flowing into Lake Fryxell in the 1990–91 season. Delta Stream.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Parera Pond. A pond lying south of Andrews Ridge. Named by the New Zealand Geographic Board (NZGB) in 1998. &quot;Parera&quot; is the Maori word for wild duck. Mummy Pond. A pond between Suess and Lacroix Glaciers. So named by T.L. Péwé, United States geologist who visited the area in December 1957, because of the mummified seals found around the pond. Lake Chad.

Geographic entities mentioned:
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -65.05
lon: -63.9667
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -66.85
lon: 141.333
The name was suggested by Donald P. Elston, USGS, a research team member who worked at the ridge in the 1979–80 and 1980–81 seasons. Northern glaciers and streams. Glaciers and streams descending towards the valley floor from the Asgard Range include Matterhorn Glacier, Lacroix Glacier, Suess Glacier, Canada Glacier and Commonwealth Glacier. Matterhorn Glacier.

Geographic entities mentioned:
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -65.05
lon: -63.9667
surface_form: matterhorn
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
surface_form: matterhorn
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -66.85
lon: 141.333
Mapped by the BrAE under Scott, 1910–13, and named after Alfred Lacroix (see Mount Lacroix). Suess Glacier. Glacier between Canada and Lacroix Glaciers, flowing south into Taylor Valley. Charted and named by the BrAE under Scott, 1910–13, for Professor Eduard Suess, noted Austrian geologist and paleontologist. Canada Glacier.

Geographic entities mentioned:
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -65.05
lon: -63.9667
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: lacroix
instance_of: Mountain
coordinates: lat: -66.85
lon: 141.333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Throughout that period, Earth's southern continents were locked into the supercontinent Gondwana. The dark band of rock that divides the sandstone is dolerite (sometimes called diabase), a volcanic rock that forms underground. The distinctive dolerite intrusion—or sill—is a remnant of a massive volcanic plumbing system that produced major eruptions about 180 million years ago.

Geographic entities mentioned:
surface_form: band
instance_of: Mountain
coordinates: lat: -78.05
lon: 163.967
Charted and named by the BrAE under Scott, 1910–13, after the African lake of the same name. Spaulding Pond. A pond northeast of the terminal ice cliff of Howard Glacier. The name was suggested by Diane McKnight, leader of United States Geological Survey (USGS) field teams which studied the hydrology and geochemistry of streams and ponds in the Lake Fryxell basin, Taylor Valley, 1987–94.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
The pond is part of the Aiken Creek system and receives drainage from several glaciers including Commonwealth Glacier, Wales Glacier and the unnamed glacier next westward. The name was suggested by USGS hydrologist Diane McKnight, leader of USGS field teams that studied the hydrology of streams entering Lake Fryxell, Taylor Valley, 1987–94. Coral Ridge.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
The name was suggested by hydrologist Diane McKnight, leader of a USGS team which made extensive studies of the hydrology and geochemistry of streams and ponds in the Lake Fryxell basin, 1987–94. Named after USGS hydrologist Edmund Andrews, a member of the field team who studied glacier hydrology during the 1987–88 and 1991–92 summer seasons. Huey Creek.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Huey Creek. A glacial meltwater stream, long, flowing south from an ice field west of Mount Falconer to the north-central shore of Lake Fryxell. The name was suggested by hydrologist Diane McKnight, leader of a USGS team that made extensive hydrological studies in the Lake Fryxell basin, 1987–94.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
The name was suggested by hydrologist Diane McKnight, leader of a USGS team that made extensive hydrological studies in the Lake Fryxell basin, 1987–94. The name acknowledges support received by the USGS field team in Taylor Valley from United States Navy Squadron VXE-6 and its twin engine UH-1N &quot;Huey&quot; helicopters. Commonwealth Glacier.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Named by the US-ACAN after Diane McKnight, research hydrologist, USGS, leader of USGS field teams over several years (1987–94) that made extensive studies of the hydrology and geochemistry of streams flowing into Lake Fryxell. Lost Seal Stream. A glacial meltwater stream, long, draining from the west margin of Commonwealth Glacier into the northeast end of Lake Fryxell.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Mount J. J. Thomson. A prominent hump-shaped peak along the north wall of Taylor Valley, standing above Lake Bonney, between Rhone Glacier and Matterhorn Glacier. So named by the Western Journey Party, led by Taylor, of the BrAE, 1910–13. The initials have been retained to distinguish the name from Mount Allan Thomson (also named by BrAE, 1910–13) near Mackay Glacier. Lake Bonney.

Geographic entities mentioned:
surface_form: matterhorn
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
surface_form: lake bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
Northern glaciers and streams. Glaciers and streams descending towards the valley floor from the Asgard Range include Matterhorn Glacier, Lacroix Glacier, Suess Glacier, Canada Glacier and Commonwealth Glacier. Matterhorn Glacier. Small alpine glacier on the edge of the north wall of Taylor Valley, just west of the Matterhorn. Named after the Matterhorn by United States geologist T.L.

Geographic entities mentioned:
surface_form: matterhorn
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
surface_form: matterhorn
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Named after the Matterhorn by United States geologist T.L. Péwé, who visited the area in December 1957. Lacroix Glacier. Glacier between Suess and Matterhorn Glaciers, which flows southeast into Taylor Valley. Mapped by the BrAE under Scott, 1910–13, and named after Alfred Lacroix (see Mount Lacroix). Suess Glacier. Glacier between Canada and Lacroix Glaciers, flowing south into Taylor Valley.

Geographic entities mentioned:
surface_form: matterhorn
instance_of: Mountain
coordinates: lat: -71.855
lon: 8.3297222222222
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
It was named after the Taylor Glacier. Geology. In the oblique aerial photo at right, the tan bands are sandstone layers from the Beacon Supergroup, a series of sedimentary rock layers formed at the bottom of a shallow sea between 250 million and 400 million years ago. Throughout that period, Earth's southern continents were locked into the supercontinent Gondwana.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Taylor Valley. Taylor Valley is an ice-free valley about long, once occupied by the receding Taylor Glacier. It lies north of the Kukri Hills between the Taylor Glacier and New Harbour in Victoria Land, Antarctica. Taylor Valley is the southernmost of the three large McMurdo Dry Valleys in the Transantarctic Mountains, located west of McMurdo Sound. Exploration and naming.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Taylor Valley. Taylor Valley is an ice-free valley about long, once occupied by the receding Taylor Glacier. It lies north of the Kukri Hills between the Taylor Glacier and New Harbour in Victoria Land, Antarctica. Taylor Valley is the southernmost of the three large McMurdo Dry Valleys in the Transantarctic Mountains, located west of McMurdo Sound. Exploration and naming.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Taylor Valley. Taylor Valley is an ice-free valley about long, once occupied by the receding Taylor Glacier. It lies north of the Kukri Hills between the Taylor Glacier and New Harbour in Victoria Land, Antarctica. Taylor Valley is the southernmost of the three large McMurdo Dry Valleys in the Transantarctic Mountains, located west of McMurdo Sound. Exploration and naming.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
Taylor Valley is the southernmost of the three large McMurdo Dry Valleys in the Transantarctic Mountains, located west of McMurdo Sound. Exploration and naming. The Taylor Valley was discovered by the British National Antarctic Expedition (BrNAE, 1901–04). It was more fully explored by the British Antarctic Expedition, 1907–09 (BrAE) and the British Antarctic Expedition, 1910–13.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Exploration and naming. The Taylor Valley was discovered by the British National Antarctic Expedition (BrNAE, 1901–04). It was more fully explored by the British Antarctic Expedition, 1907–09 (BrAE) and the British Antarctic Expedition, 1910–13. It was named after the Taylor Glacier. Geology.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
J. Thomson, Lake Bonney, Nussbaum Reigel, Mummy Pond, Lake Chad, Andrews Ridge and Lake Frysell, which is fed by the Delta Stream from the south. Bonney Riegel. A riegel, or rock bar extending north from the Kukri Hills across Taylor Valley to Lake Bonney. Named in association with Lake Bonney by the Western Journey Party, led by Griffith Taylor, of the BrAE, 1910–13. Mount J. J. Thomson.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
surface_form: lake bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
J. Thomson, Lake Bonney, Nussbaum Reigel, Mummy Pond, Lake Chad, Andrews Ridge and Lake Frysell, which is fed by the Delta Stream from the south. Bonney Riegel. A riegel, or rock bar extending north from the Kukri Hills across Taylor Valley to Lake Bonney. Named in association with Lake Bonney by the Western Journey Party, led by Griffith Taylor, of the BrAE, 1910–13. Mount J. J. Thomson.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
surface_form: lake bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
Mount J. J. Thomson. A prominent hump-shaped peak along the north wall of Taylor Valley, standing above Lake Bonney, between Rhone Glacier and Matterhorn Glacier. So named by the Western Journey Party, led by Taylor, of the BrAE, 1910–13. The initials have been retained to distinguish the name from Mount Allan Thomson (also named by BrAE, 1910–13) near Mackay Glacier. Lake Bonney.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
So named by the Western Journey Party, led by Taylor, of the BrAE, 1910–13. The initials have been retained to distinguish the name from Mount Allan Thomson (also named by BrAE, 1910–13) near Mackay Glacier. Lake Bonney. Lake lying at the mouth of Taylor Glacier. Named by the BrAE under Scott, 1910–13, for T. Bonney, professor of geology at Cambridge University, England. Ventifact Knobs.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
The knobs are covered by ventifacts, suggesting the name, and are located just east of Lake Bonney. Named by United States geologist Troy L. Péwé who was first to study and describe the knobs in December 1957. Nussbaum Riegel. A riegel or rock-bar across Taylor Valley, extending from the vicinity of Sollas Glacier toward Lake Chad. Charted and named by the BrAE under Scott, 1910–13. The Defile.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
surface_form: lake chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
Nussbaum Riegel. A riegel or rock-bar across Taylor Valley, extending from the vicinity of Sollas Glacier toward Lake Chad. Charted and named by the BrAE under Scott, 1910–13. The Defile. Narrow ice-free passageway between the terminus of Suess Glacier and the talus-covered slope of Nussbaum Riegel in Taylor Valley. Charted and descriptively named by the BrAE under Scott, 1910–13. Andrews Ridge.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Charted and descriptively named by the BrAE under Scott, 1910–13. Andrews Ridge. A gentle ridge, the northern arm of Nussbaum Riegel, which trends eastward to the south of Suess Glacier and Lake Chad in Taylor Valley. Named by Griffith Taylor, leader of the Western Journey Party of the BrAE, 1910–13. Parera Pond. A pond lying south of Andrews Ridge.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
surface_form: lake chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
Charted and descriptively named by the BrAE under Scott, 1910–13. Andrews Ridge. A gentle ridge, the northern arm of Nussbaum Riegel, which trends eastward to the south of Suess Glacier and Lake Chad in Taylor Valley. Named by Griffith Taylor, leader of the Western Journey Party of the BrAE, 1910–13. Parera Pond. A pond lying south of Andrews Ridge.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
Lake Hoare. A lake about long between Lake Chad and Canada Glacier. Named by the 8th Victoria University of Wellington Antarctic Expedition (VUWAE), 1963–64, for physicist R.A. Hoare, a member of VUWAE that examined lakes in Taylor, Wright, and Victoria Valleys. Lake Fryxell. Lake long, between Canada and Commonwealth Glaciers at the lower end of Taylor Valley.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
Named by the 8th Victoria University of Wellington Antarctic Expedition (VUWAE), 1963–64, for physicist R.A. Hoare, a member of VUWAE that examined lakes in Taylor, Wright, and Victoria Valleys. Lake Fryxell. Lake long, between Canada and Commonwealth Glaciers at the lower end of Taylor Valley. Mapped by the BrAE under Scott, 1910–13. The lake was visited by Professor T.L.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Fryxell, glacial geologist of Augustana College, Illinois. Many Glaciers Pond. A pond, long, located south of the snout of Commonwealth Glacier in Taylor Valley. The pond is part of the Aiken Creek system and receives drainage from several glaciers including Commonwealth Glacier, Wales Glacier and the unnamed glacier next westward.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
Coral Ridge. A ridge trending north–south, transverse to the axis of Taylor Valley, forming a divide above sea level between Lake Fryxell and Explorers Cove, McMurdo Sound. A large number of solitary fossil corals have been found here by NZARP/USARP teams in the course of joint geological studies of the area. The name was suggested by Donald P.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Glacier between Canada and Lacroix Glaciers, flowing south into Taylor Valley. Charted and named by the BrAE under Scott, 1910–13, for Professor Eduard Suess, noted Austrian geologist and paleontologist. Canada Glacier. Small glacier flowing southeast into the north side of Taylor Valley immediately west of Lake Fryxell. Charted and named by the BrAE, 1910–13, under Scott. Charles S.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Green Creek. A glacial meltwater stream, long, flowing northeast from the extremity of Canada Glacier into the southwest end of Lake Fryxell, close east of Bowles Creek, in Taylor Valley. The name was suggested by hydrologist Diane McKnight, leader of USGS teams that made intensive studies of the hydrology of
streams of the Lake Fryxell basin, 1987–94. Named after William J.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: bowles
instance_of: Mountain
coordinates: lat: -61.283333333333
lon: -54.133333333333
surface_form: bowles
instance_of: Mountain
coordinates: lat: -62.616666666667
lon: -60.202222222222
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Canada Stream. A small meltwater stream flowing east-southeast from the front of Canada Glacier into Lake Fryxell, in Taylor Valley. Named in association with Canada Glacier by the New Zealand Antarctic Place-Names Committee (NZ-APC) in 1983. Andrews Creek. A glacial meltwater stream which flows south along the east margin of Canada Glacier into the west end of Lake Fryxell.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
The name acknowledges support received by the USGS field team in Taylor Valley from United States Navy Squadron VXE-6 and its twin engine UH-1N &quot;Huey&quot; helicopters. Commonwealth Glacier. Glacier which flows in a southeast direction and enters the north side of Taylor Valley immediately west of Mount Coleman. Charted and named by the BrAE under Scott, 1910–13.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
Southern glaciers and streams. Glaciers descending towards the valley floor from the Kukri Hills include, from west to east, Glaciers in the Kukri Hills that flow towards the Taylor Valley floor include, from west to east, Calkin Glacier, Hughes Glacier, Sollas Glacier, Marr Glacier, Moa Glacier, Goldman Glacier, Howard Glacier, Crescent Glacier, Von Guerard Glacier.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: taylor valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: marr
instance_of: Mountain
coordinates: lat: -66.4
lon: 52.1167
Mount J. J. Thomson. A prominent hump-shaped peak along the north wall of Taylor Valley, standing above Lake Bonney, between Rhone Glacier and Matterhorn Glacier. So named by the Western Journey Party, led by Taylor, of the BrAE, 1910–13. The initials have been retained to distinguish the name from Mount Allan Thomson (also named by BrAE, 1910–13) near Mackay Glacier. Lake Bonney.

Geographic entities mentioned:
surface_form: mount allan
instance_of: Mountain
coordinates: lat: -69.9833
lon: -67.75
von Guerard, a member of the field team in three seasons, 1990–94, who assisted in establishing stream gaging stations on streams flowing into Lake Fryxell in the 1990–91 season. Maria Creek. A glacial meltwater stream, long, which flows from the snout of Canada Glacier. It drains NE, close to the glacier, entering the west end of Lake Fryxell to the west of Bowles Creek and Green Creek.

Geographic entities mentioned:
surface_form: bowles
instance_of: Mountain
coordinates: lat: -61.283333333333
lon: -54.133333333333
surface_form: bowles
instance_of: Mountain
coordinates: lat: -62.616666666667
lon: -60.202222222222
It drains NE, close to the glacier, entering the west end of Lake Fryxell to the west of Bowles Creek and Green Creek. The name was suggested by Diane McKnight, USGS hydrologist working in the Lake Fryxell basin, 1987–94, and alludes to the many aeolian deposits of fine sands along the creek, indicative of strong winds blowing around the south end of Canada Glacier during the winter.

Geographic entities mentioned:
surface_form: strong
instance_of: Mountain
coordinates: lat: -70.583333333333
lon: -62.75
Features. Features of the valley include, from west to east, Bonney Riegel below Mount J. J. Thomson, Lake Bonney, Nussbaum Reigel, Mummy Pond, Lake Chad, Andrews Ridge and Lake Frysell, which is fed by the Delta Stream from the south. Bonney Riegel. A riegel, or rock bar extending north from the Kukri Hills across Taylor Valley to Lake Bonney.

Geographic entities mentioned:
surface_form: chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
surface_form: lake chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
Named after USGS hydrologist Sarah Ann Spauiding, a member of the team during two seasons, 1988–89 and 1991–92, who studied the pond. Lake Hoare. A lake about long between Lake Chad and Canada Glacier. Named by the 8th Victoria University of Wellington Antarctic Expedition (VUWAE), 1963–64, for physicist R.A. Hoare, a member of VUWAE that examined lakes in Taylor, Wright, and Victoria Valleys.

Geographic entities mentioned:
surface_form: chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
surface_form: lake chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
Andrews Ridge. A gentle ridge, the northern arm of Nussbaum Riegel, which trends eastward to the south of Suess Glacier and Lake Chad in Taylor Valley. Named by Griffith Taylor, leader of the Western Journey Party of the BrAE, 1910–13. Parera Pond. A pond lying south of Andrews Ridge. Named by the New Zealand Geographic Board (NZGB) in 1998. &quot;Parera&quot; is the Maori word for wild duck.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
So named by T.L. Péwé, United States geologist who visited the area in December 1957, because of the mummified seals found around the pond. Lake Chad. Small lake lying east of the mouth of Suess Glacier. Charted and named by the BrAE under Scott, 1910–13, after the African lake of the same name. Spaulding Pond. A pond northeast of the terminal ice cliff of Howard Glacier.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The name was suggested by Diane McKnight, leader of United States Geological Survey (USGS) field teams which studied the hydrology and geochemistry of streams and ponds in the Lake Fryxell basin, Taylor Valley, 1987–94. Named after USGS hydrologist Sarah Ann Spauiding, a member of the team during two seasons, 1988–89 and 1991–92, who studied the pond. Lake Hoare.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
Mapped by the BrAE under Scott, 1910–13. The lake was visited by Professor T.L. Péwé during United States Navy Operation Deep Freeze, 1957–58, and was named by him for Doctor Fritiof M. Fryxell, glacial geologist of Augustana College, Illinois. Many Glaciers Pond. A pond, long, located south of the snout of Commonwealth Glacier in Taylor Valley.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
Bowles, a member of the field team in the 1987–88 summer season, who conducted a study of organic geochemistry of streams flowing into Lake Fryxell. Aiken Creek. A glacial meltwater stream in Taylor Valley, which flows north from the unnamed glacier west of Wales Glacier to Many Glaciers Pond, then west to Lake Fryxell. The feature is long and receives some tributary flow from Wales Glacier.

Geographic entities mentioned:
surface_form: pond
instance_of: Mountain
coordinates: lat: -62.95
lon: -60.55
The initials have been retained to distinguish the name from Mount Allan Thomson (also named by BrAE, 1910–13) near Mackay Glacier. Lake Bonney. Lake lying at the mouth of Taylor Glacier. Named by the BrAE under Scott, 1910–13, for T. Bonney, professor of geology at Cambridge University, England. Ventifact Knobs. Minor knobs, high, composed of lake clay covered by glacial drift.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Péwé who was first to study and describe the knobs in December 1957. Nussbaum Riegel. A riegel or rock-bar across Taylor Valley, extending from the vicinity of Sollas Glacier toward Lake Chad. Charted and named by the BrAE under Scott, 1910–13. The Defile. Narrow ice-free passageway between the terminus of Suess Glacier and the talus-covered slope of Nussbaum Riegel in Taylor Valley.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The Defile. Narrow ice-free passageway between the terminus of Suess Glacier and the talus-covered slope of Nussbaum Riegel in Taylor Valley. Charted and descriptively named by the BrAE under Scott, 1910–13. Andrews Ridge. A gentle ridge, the northern arm of Nussbaum Riegel, which trends eastward to the south of Suess Glacier and Lake Chad in Taylor Valley.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Hoare, a member of VUWAE that examined lakes in Taylor, Wright, and Victoria Valleys. Lake Fryxell. Lake long, between Canada and Commonwealth Glaciers at the lower end of Taylor Valley. Mapped by the BrAE under Scott, 1910–13. The lake was visited by Professor T.L. Péwé during United States Navy Operation Deep Freeze, 1957–58, and was named by him for Doctor Fritiof M.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Charted and named by the BrAE under Scott, 1910–13, for Professor Eduard Suess, noted Austrian geologist and paleontologist. Canada Glacier. Small glacier flowing southeast into the north side of Taylor Valley immediately west of Lake Fryxell. Charted and named by the BrAE, 1910–13, under Scott. Charles S. Wright, a Canadian physicist, was a member of the party that explored this area.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Commonwealth Glacier. Glacier which flows in a southeast direction and enters the north side of Taylor Valley immediately west of Mount Coleman. Charted and named by the BrAE under Scott, 1910–13. Named for the Commonwealth of Australia, which made a financial grant to the BrAE and contributed two members to the Western Geological Party which explored this area. McKnight Creek.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
It separates the Kukri Hills to the south from the Asgard Range to the north. Features. Features of the valley include, from west to east, Bonney Riegel below Mount J. J. Thomson, Lake Bonney, Nussbaum Reigel, Mummy Pond, Lake Chad, Andrews Ridge and Lake Frysell, which is fed by the Delta Stream from the south. Bonney Riegel.

Geographic entities mentioned:
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
Ventifact Knobs. Minor knobs, high, composed of lake clay covered by glacial drift. The glacial drift has cobbles that are well polished by the wind and cut into ventifacts. The knobs are covered by ventifacts, suggesting the name, and are located just east of Lake Bonney. Named by United States geologist Troy L. Péwé who was first to study and describe the knobs in December 1957. Nussbaum Riegel.

Geographic entities mentioned:
surface_form: bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
surface_form: lake bonney
instance_of: Lake
coordinates: lat: -77.71667
lon: 162.41667
Moss Vale is the junction of the Unanderra – Moss Vale railway line to Wollongong, opened in 1932, but now only used by freight trains. Television. Television is delivered from the Illawarra region with a transmitter based on Mount Gibraltar.

Geographic entities mentioned:
surface_form: Mount Gibraltar
instance_of: Mountain
countries: Australia
coordinates: lat: -34.465333333333
lon: 150.42826666667
Masha is entrusted with guarding him. Tensions arise between both: the officer is a well-educated aristocrat who is both amused and impressed by the crude attempts of Masha, a fisherman's orphan daughter, to compose Agitprop poetry. When their camels are stolen, their commander decides to send his captive on a boat to their headquarters in Kazalinsk via the Aral Sea.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Mount Abuna Yosef. Abuna Yosef (Amharic: አቡነ ዮሴፍ) is a prominent mountain in the Lasta massif of the Ethiopian Highlands. At it is the 6th tallest mountain in Ethiopia and the 19th highest of Africa. It is located in the Semien Wollo Zone of the Amhara Region. Afro-alpine environment.

Geographic entities mentioned:
surface_form: mount abuna yosef
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.140833333333
lon: 39.181666666667
surface_form: abuna yosef
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.140833333333
lon: 39.181666666667
Mount Abuna Yosef. Abuna Yosef (Amharic: አቡነ ዮሴፍ) is a prominent mountain in the Lasta massif of the Ethiopian Highlands. At it is the 6th tallest mountain in Ethiopia and the 19th highest of Africa. It is located in the Semien Wollo Zone of the Amhara Region. Afro-alpine environment.

Geographic entities mentioned:
surface_form: abuna yosef
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.140833333333
lon: 39.181666666667
At it is the 6th tallest mountain in Ethiopia and the 19th highest of Africa. It is located in the Semien Wollo Zone of the Amhara Region. Afro-alpine environment. The Abuna Yosef massif is home to Ethiopian wolves, Gelada baboons, Erica arborea, Lobelia and other afro-alpine vegetation. The Abuna Yosef Community Conservation Area covers about 70 km of the Abuna Yosef massif. Major towns.

Geographic entities mentioned:
surface_form: abuna yosef
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.140833333333
lon: 39.181666666667
At it is the 6th tallest mountain in Ethiopia and the 19th highest of Africa. It is located in the Semien Wollo Zone of the Amhara Region. Afro-alpine environment. The Abuna Yosef massif is home to Ethiopian wolves, Gelada baboons, Erica arborea, Lobelia and other afro-alpine vegetation. The Abuna Yosef Community Conservation Area covers about 70 km of the Abuna Yosef massif. Major towns.

Geographic entities mentioned:
surface_form: abuna yosef
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.140833333333
lon: 39.181666666667
surface_form: abuna yosef
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.140833333333
lon: 39.181666666667
The Abuna Yosef Community Conservation Area covers about 70 km of the Abuna Yosef massif. Major towns. At the eastern part of the mountain range, the town of Wandatch (on the Kobo - Lalibela road) is the main entry point to the Abuna Yosef afro-alpine massif. At 3500 m above sea level, it is one of the most elevated towns in Ethiopia.

Geographic entities mentioned:
surface_form: abuna yosef
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.140833333333
lon: 39.181666666667
When the expanding flank finally gives it releases a flow of magma. More explosive lateral eruptions are referred to as lateral blasts. Some of the most notable examples of a lateral eruption include Mount St. Helens, Mount Pelée, and Mount Etna. Creation of a lateral eruption. Most eruptions are caused by the immediate decompression of a magma chamber near the flanks of the volcano.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Pyroclastic flows and lahars can affect areas originating from the volcano roughly in the shape of a cone that can span hundreds of square kilometers. Examples. Mount St. Helens is a stratovolcano located in Washington, USA. Volcanic activity beginning in March 1980 saw magma accumulating underneath the mountain's north flank.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
On May 18, 1980, an earthquake triggered the collapse of the flank and a lateral eruption which killed 57 people. It was the deadliest volcanic event in US history. Bezymianny is a stratovolcano located on the Kamchatka peninsula in Russia. On March 30, 1956, it erupted laterally after a flank collapse similar to that experienced by Mount St. Helens.

Geographic entities mentioned:
surface_form: Bezymianny
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.966666666667
lon: 160.6
Helens. No fatalities resulted from this eruption due to the remote location of the volcano. Subsequent lava dome growth has since filled the 1956 caldera with a new cone. Mount Pelée is a volcano located on Martinique, in the Caribbean. It underwent a lateral eruption on May 8, 1902, killing 28,000 people in the deadliest volcanic event of the 20th century.

Geographic entities mentioned:
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
San Francisco Peaks in Arizona are the remnants of a single taller volcano that may have had a lateral eruption around 200,000 years ago. Nevado de Toluca is a stratovolcano to the west of Toluca, Mexico. About 25,000 years ago, Nevado de Toluca experienced a large, lateral blast to the east which reduced the elevation by about 3000ft.

Geographic entities mentioned:
surface_form: Nevado de Toluca
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.101666666667
lon: -99.7675
Frances River (Yukon). The Frances River is a left tributary of the Liard River in southern Yukon. The Frances River forms the drain of Frances Lake. Flowing south, it passes Tuchitua, where the Nahanni Range Road branches off from the Yukon Highway 4 (Robert Campbell Highway).

Geographic entities mentioned:
surface_form: Frances Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.3478
lon: -129.572
Bronnlinde became Woglinde, probably to avoid confusion with Brünnhilde. Wagner may also have been influenced by the Rhine River-based German legend of Lorelei, the lovelorn young maiden who drowns herself in the river and becomes a siren, luring fishermen onto the rocks by her singing. Further possible sources lie in Greek mythology and literature.

Geographic entities mentioned:
surface_form: Lorelei
instance_of: Mountain
countries: Germany
coordinates: lat: 50.139444444444
lon: 7.7288888888889
The city is built on the two sides of a shallow valley, into which flow two streams from the west, the Trunkfield Brook and the Leamonsley Brook, and out of which the Curborough Brook runs to the north-east, eventually flowing into the River Trent. The two streams have been dammed south of the cathedral on Dam Street to form Minster Pool and near St Chad's Road to form Stowe Pool. Suburbs.

Geographic entities mentioned:
surface_form: Minster Pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.684293
lon: -1.829972
surface_form: Stowe Pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.688384
lon: -1.822799