Sarmila/GeoWiki-Features huggingface dataset:
The Sajur is also the only river in Syria that enters the Euphrates on its right bank; both the Balikh and the Khabur flow into the Euphrates on the left bank. Drainage basin. The Sajur drains a total area of. The Syrian part of the Sajur basin – the Manbij Plain – has been particularly well-studied. This area is bounded on the north by the Syro–Turkish border and extends as far south as Manbij.

Geographic entities mentioned:
surface_form: sajur
instance_of: Watercourse
countries: Turkey
Syria
coordinates: lat: 36.65972222
lon: 38.07055556
Economy. Both Turkey and Syria use water from the Sajur for irrigation purposes. Since the 19th century, occupation in and cultivation of the Sajur basin have steadily increased, especially in the western, more fertile part of the area. The introduction of motorized pumps has led to a considerable decrease of the groundwater table, with the effect that many wells have dried up.

Geographic entities mentioned:
surface_form: sajur
instance_of: Watercourse
countries: Turkey
Syria
coordinates: lat: 36.65972222
lon: 38.07055556
The introduction of motorized pumps has led to a considerable decrease of the groundwater table, with the effect that many wells have dried up. Turkey has built the Kayacık Dam on the Ayfinar Deresi, one of the two streams that join to form the Sajur. This high dam creates a reservoir with a surface area of. From this reservoir, an area of is irrigated.

Geographic entities mentioned:
surface_form: sajur
instance_of: Watercourse
countries: Turkey
Syria
coordinates: lat: 36.65972222
lon: 38.07055556
Turkey has built the Kayacık Dam on the Ayfinar Deresi, one of the two streams that join to form the Sajur. This high dam creates a reservoir with a surface area of. From this reservoir, an area of is irrigated. A dam with a planned reservoir capacity of is under construction on the Syrian part of the Sajour. The city of Aleppo disposes part of its wastewater into the Sajur drainage system.

Geographic entities mentioned:
surface_form: sajur
instance_of: Watercourse
countries: Turkey
Syria
coordinates: lat: 36.65972222
lon: 38.07055556
Turkey has built the Kayacık Dam on the Ayfinar Deresi, one of the two streams that join to form the Sajur. This high dam creates a reservoir with a surface area of. From this reservoir, an area of is irrigated. A dam with a planned reservoir capacity of is under construction on the Syrian part of the Sajour. The city of Aleppo disposes part of its wastewater into the Sajur drainage system.

Geographic entities mentioned:
surface_form: sajour
instance_of: Watercourse
countries: Turkey
Syria
coordinates: lat: 36.65972222
lon: 38.07055556
Moritz via Andermatt in the central Swiss Alps. The train provides a one-seat ride for an 8-hour end-to-end journey, and omits stops made by local trains. The Glacier Express has been called the 'slowest express train in the world'. As St. Moritz and Zermatt are home to two well-known mountains, the Glacier Express is also said to travel from Matterhorn to Piz Bernina.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: Piz Bernina
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.382388888889
lon: 9.9081111111111
As St. Moritz and Zermatt are home to two well-known mountains, the Glacier Express is also said to travel from Matterhorn to Piz Bernina. The journey from Zermatt starts at the dead end of an Alpine valley, the Mattertal, just below the Matterhorn at an elevation of before it descends to the huge valley of the Valais in Brig.

Geographic entities mentioned:
surface_form: Mattertal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.083333333333
lon: 7.8
One passenger was killed and 42 other passengers were injured. The accident was caused by the train traveling too fast as a result of human error. Albula line. Shortly after leaving St. Moritz station () in Graubünden, the train passes Samedan and Bever on the high Engadin plateau. There it continues in the &quot;Val Bever&quot; before entering the Albula Tunnel at under the Albula Pass.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Oberalp section. From Chur, the train follows back the course of the Rhine through the gorge of Ruinaulta and climbs slowly the valley toward Ilanz (), Mustér () and Sedrun (). From Sedrun the line becomes steeper to finally reach its summit, the Oberalp Pass at. From there the train enters the Canton of Uri in Central Switzerland and continues down to Andermatt (). Furka section.

Geographic entities mentioned:
surface_form: Ruinaulta
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.8081
lon: 9.31495
Furka section. From Andermatt, the train goes forward in the valley called Urseren passing the villages of Hospental () and Realp (). From there the train enters the Furka Base Tunnel, leaving the old railway line which climbs the Furka Pass (operated today by the Furka Cogwheel Steam Railway), to emerge in Oberwald () in the Goms Valley, in the Canton of Valais.

Geographic entities mentioned:
surface_form: Urseren
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.633333333333
lon: 8.5333333333333
Mattertal line. From Brig, () the train continues to Visp (), then enters the valley of Mattertal and goes up, passing the villages of Stalden (), St. Niklaus () and Randa (), where a spectacular debris avalanche completely disconnected the railway and road in 1991. Täsch () is an important station as it is the end of the open road, and therefore a terminal for motorists.

Geographic entities mentioned:
surface_form: Mattertal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.083333333333
lon: 7.8
After a high-profile case in Milan in 1384, there were a number of witch trials in Italy during the 15th-century. A number of mass witch trials with many executions took place in Cuneo 1477, Pavia 1479, Valtellina 1460, 1483 and 1485, in Canavese 1472 and 1475–76, in Peveragno in 1485 and 1489 and in Carignano in 1493–94. The Italian witch trials reached their peak during the Italian Wars.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
During the second Italian witch hunt of 1580–1660, the majority of witch trials were conducted by local secular courts, rather than the Inquisition. During the second wave, the largest mass witch trials were the one of Val di Fassa in 1573, 1627–31 and 1643–1644; the Val di Non in 1611–1615, Turino in 1619, Nogaredo in 1640-1647, and Valtellina of the 1670s.

Geographic entities mentioned:
surface_form: Valtellina
instance_of: Valley
countries: Italy
coordinates: lat: 46.166666666667
lon: 9.8666666666667
It is subtitled &quot;In search of the birdmen of Peru&quot; and is an account of two interlinked journeys. In the first Shah travels from Machu Picchu to Cusco, and then largely by public transport via Lake Titicaca and Nazca to Lima.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
To the east of the lake are the Mostoos Hills. Besides the aforementioned Martineau River and Cold Lake, the waters of Primrose Lake flow through multiple rivers and lakes en route to the Churchill River, including Cold River, Pierce Lake, Lepine Lake, Lac des Îles, Waterhen River, Waterhen Lake, Beaver River, and Lac Île-à-la-Crosse. Primrose Lake IBA.

Geographic entities mentioned:
surface_form: Lac Île-à-la-Crosse
instance_of: Lake
countries: Canada
coordinates: lat: 55.4444
lon: -107.849
surface_form: cold lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.55009
lon: -110.00084
surface_form: pierce lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.168
lon: -92.959
surface_form: waterhen lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.1033
lon: -99.5583
surface_form: lac des îles
instance_of: Lake
countries: Canada
coordinates: lat: 54.433425
lon: -109.417464
surface_form: waterhen lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.48804
lon: -108.458651
surface_form: primrose lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7875
lon: -110.0325
surface_form: lac des îles
instance_of: Lake
countries: Canada
coordinates: lat: 45.895833
lon: -70.84384
surface_form: pierce lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.500091
lon: -109.700818
surface_form: lac des îles
instance_of: Lake
countries: Canada
coordinates: lat: 47.08555555555556
lon: -72.45416666666667
It lies within muskeg and the boreal forest ecozone of Canada. There are several rivers and creeks that flow into the lake with Calder River on the northern shore being the primary inflow. Martineau River is the lake's outflow and it starts on the southern shore and flows in a south-westerly direction into Cold Lake in Alberta. To the east of the lake are the Mostoos Hills.

Geographic entities mentioned:
surface_form: cold lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.55009
lon: -110.00084
There are several islands in the lake that support colonial nesting birds with Backes Island () being the most prominent. Backes Island has been designated a provincial wildlife refuge. Birds found on the island and elsewhere in the IBA include the American white pelican, double-crested cormorant, common tern, California gull, great blue heron, ring-billed gull, and the herring gull. Launch Site.

Geographic entities mentioned:
surface_form: blue
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.1
lon: -119.283
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
The lake straddles the Saskatchewan / Alberta border, with most of the water surface in Saskatchewan with only the south-west corner of the lake in Alberta. On the Saskatchewan side of the lake is Backes Island Wildlife Refuge, which is a small protected island near the middle of the lake that is important to birds.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Most of the IBA is in Saskatchewan but the western boundary is in Alberta. The lake is surrounded by boreal forests and has a sub-arctic climate. There are several islands in the lake that support colonial nesting birds with Backes Island () being the most prominent. Backes Island has been designated a provincial wildlife refuge.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
There are several islands in the lake that support colonial nesting birds with Backes Island () being the most prominent. Backes Island has been designated a provincial wildlife refuge. Birds found on the island and elsewhere in the IBA include the American white pelican, double-crested cormorant, common tern, California gull, great blue heron, ring-billed gull, and the herring gull. Launch Site.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Primrose Lake. Primrose Lake is a large lake in the Canadian provinces of Saskatchewan and Alberta in the Churchill River drainage basin. The lake straddles the Saskatchewan / Alberta border, with most of the water surface in Saskatchewan with only the south-west corner of the lake in Alberta.

Geographic entities mentioned:
surface_form: primrose lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7875
lon: -110.0325
The entire lake plus surrounding land totalling is part of an Important Bird Area (IBA) of Canada. Description. Primrose Lake has a total surface area of, of which is in Alberta, and an elevation of. It lies within muskeg and the boreal forest ecozone of Canada. There are several rivers and creeks that flow into the lake with Calder River on the northern shore being the primary inflow.

Geographic entities mentioned:
surface_form: primrose lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7875
lon: -110.0325
To the east of the lake are the Mostoos Hills. Besides the aforementioned Martineau River and Cold Lake, the waters of Primrose Lake flow through multiple rivers and lakes en route to the Churchill River, including Cold River, Pierce Lake, Lepine Lake, Lac des Îles, Waterhen River, Waterhen Lake, Beaver River, and Lac Île-à-la-Crosse. Primrose Lake IBA.

Geographic entities mentioned:
surface_form: primrose lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7875
lon: -110.0325
Primrose Lake IBA. The Primrose Lake (SK 092) IBA encompasses the entire lake and much of the surrounding landscape. Most of the IBA is in Saskatchewan but the western boundary is in Alberta. The lake is surrounded by boreal forests and has a sub-arctic climate. There are several islands in the lake that support colonial nesting birds with Backes Island () being the most prominent.

Geographic entities mentioned:
surface_form: primrose lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7875
lon: -110.0325
Launch Site. The south-west corner of Primrose Lake () in Alberta was used as launch site for sounding rockets of the types super Loki and Arcas in Canada. The first launch was on 5 April 1968 and the last one was 11 September 1991. Fish species. The fish species include walleye, sauger, yellow perch, northern pike, lake trout, lake whitefish, cisco, white sucker, longnose sucker, and burbot.

Geographic entities mentioned:
surface_form: primrose lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7875
lon: -110.0325
In 1593, Pietro's &quot;particular experience and knowledge of the Roman court&quot; led him to continue advising Ferdinando on various matters, including encouraging him to pursue the reclamation of the Val di Chiana. After Lorenzo took over as First Secretary from Pietro, a sort of dynamic tension developed between the two brothers.

Geographic entities mentioned:
surface_form: Val di Chiana
instance_of: Valley
countries: Italy
coordinates: lat: 43.25
lon: 11.816666666667
Geography. The parish of Tux covers the higher and largest part of the Tuxertal, a side valley of the Zillertal that branches off at Mayrhofen. The territory of the parish extends to the glaciated peak of Olperer (3,476 m) and the 2,338 m high saddle of the Tuxer Joch, a crossing between the Zillertal and Wipptal valleys that was heavily used even in the protohistoric period.

Geographic entities mentioned:
surface_form: Tuxertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.1625
lon: 11.754166666667
surface_form: Zillertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.333333333333
lon: 11.866666666667
Geography. The parish of Tux covers the higher and largest part of the Tuxertal, a side valley of the Zillertal that branches off at Mayrhofen. The territory of the parish extends to the glaciated peak of Olperer (3,476 m) and the 2,338 m high saddle of the Tuxer Joch, a crossing between the Zillertal and Wipptal valleys that was heavily used even in the protohistoric period.

Geographic entities mentioned:
surface_form: Olperer
instance_of: Mountain
countries: Austria
coordinates: lat: 47.053055555556
lon: 11.658888888889
surface_form: Wipptal
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 47
lon: 11.5
The territory of the parish extends to the glaciated peak of Olperer (3,476 m) and the 2,338 m high saddle of the Tuxer Joch, a crossing between the Zillertal and Wipptal valleys that was heavily used even in the protohistoric period. Other prominent peaks within the municipality are the 3,288 m high Gefrorene Wand Spitze and the 3,231 m high Hoher Riffler.

Geographic entities mentioned:
surface_form: Gefrorene Wand Spitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.065277777778
lon: 11.679166666667
The 2,292 m high hamlet of Geiseljoch lies on the way into the Inn valley that was once a busy trading route to the markets in Hall in Tirol and Innsbruck. From Vorderlanersbach there is a single-cable gondola lift to the Rastkogel skiing area, which in turn is linked to the nearby skiing areas of Penken and Eggalm.

Geographic entities mentioned:
surface_form: Penken
instance_of: Mountain
countries: Austria
coordinates: lat: 47.1689
lon: 11.7997
The Tuxer valley was discovered in prehistoric times as evinced by various finds from the middle Stone Age. The first settlers in the valley were probably Breuni, who came from the Raeti tribe and settled in the Wipptal. Shepherds and miners also settled the valley, migrating over the Tuxer Joch from the Schmirn valley and cultivating it by clearing forests.

Geographic entities mentioned:
surface_form: Wipptal
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 47
lon: 11.5
Negeri Sembilan has diverse tropical rainforests and an equatorial climate. The state's mountain ranges belong to the Titiwangsa Mountains, a southern subrange of the Tenasserim Hills that span throughout southern Myanmar, southern Thailand and Peninsular Malaysia, with Mount Besar Hantu as the highest point. The Titiwangsa also ends here, at Mount Tampin, located south of the state.

Geographic entities mentioned:
surface_form: Mount Besar Hantu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.2269876
lon: 102.0125621
The state's mountain ranges belong to the Titiwangsa Mountains, a southern subrange of the Tenasserim Hills that span throughout southern Myanmar, southern Thailand and Peninsular Malaysia, with Mount Besar Hantu as the highest point. The Titiwangsa also ends here, at Mount Tampin, located south of the state. The capital of Negeri Sembilan is Seremban.

Geographic entities mentioned:
surface_form: Mount Tampin
instance_of: Mountain
countries: Malaysia
coordinates: lat: 2.508611111111111
lon: 102.21166666666667
Its rainforests form part of the Titiwangsa Forest Complex, a component of the Central Forest Spine conservation area that covers much of the heavily forested and mountainous interior of Peninsular Malaysia. Highest point. Mount Besar Hantu, at 1,462 m (4,797 ft), located in Jelebu District and close to the border with Pahang, is the highest point in Negeri Sembilan.

Geographic entities mentioned:
surface_form: Mount Besar Hantu
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.2269876
lon: 102.0125621
The nearby Mount Nuang, which is 31 metres taller, marks the tripoint with Selangor and Pahang at its northernmost point, of which it is the third tallest in the former; while in the south, Mount Ledang, an isolated mountain, marks the tripoint with Malacca and Johor, where it is the highest point of the latter at 1,276 m (4,186.3 ft). Traditional districts.

Geographic entities mentioned:
surface_form: Mount Nuang
instance_of: Mountain
countries: Malaysia
coordinates: lat: 3.26667
lon: 101.9
surface_form: Mount Ledang
instance_of: Mountain
countries: Malaysia
coordinates: lat: 2.3741666666667
lon: 102.60777777778
This area is also used as a wildlife refuge. The reservoir is bridged by State Route 127. Only a few miles below Elk River Dam is the beginning of slack water (Tims Ford Lake) caused by the Tims Ford Dam of the Tennessee Valley Authority. The slack water extends upstream to the vicinity of Estill Springs. It is then bridged by U.S. Route 41A.

Geographic entities mentioned:
surface_form: Tims Ford Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.196944444444
lon: -86.278611111111
Recreation. In Limestone County, Alabama there is a Canoe and Kayak Trail. The trail begins at the Alabama-Tennessee state line and goes to Elk River Mills. Outside of Winchester, TN Tims Ford Lake was created by damming the Elk River which allows for boating and water based activities.

Geographic entities mentioned:
surface_form: Tims Ford Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.196944444444
lon: -86.278611111111
In the 2021 census, Shipston-on-Stour had a population of 5,849. This area is sometimes termed the Vale of Red Horse, close to the Oxfordshire and Gloucestershire borders. Etymology linked to sheep and wool trade. In the 8th century, the toponym was &quot;Scepwaeisctune&quot;, Old English for Sheep-wash-Town. It had a sheep marketplace for many centuries.

Geographic entities mentioned:
surface_form: Vale of Red Horse
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.117
lon: -1.472
On Lord Howe Island, the species is generally uncommon, but is locally abundant in the moist forests of the southern parts of the island, where it forms an association with &quot;Piper&quot; species on the north-western slopes of Mount Lidgbird.

Geographic entities mentioned:
surface_form: Mount Lidgbird
instance_of: Mountain
countries: Australia
coordinates: lat: -31.566666666667
lon: 159.08333333333
Mit'u. Mit'u (Quechua for mud, hispanicized spelling &quot;Mito&quot;) is a mountain in the Andes of Peru which reaches an altitude of approximately. It is located in the Junín Region, Yauli Province, Morococha District, north of Shawaq. Mit'u lies south of the Puka Yaku River (&quot;red water&quot;, hispanicized &quot;Pucayacu&quot;), an affluent of the Mantaro River.

Geographic entities mentioned:
surface_form: Shawaq
instance_of: Mountain
countries: Peru
coordinates: lat: -11.56305556
lon: -76.165
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
surface_form: yauli
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4992
lon: -76.1297
surface_form: shawaq
instance_of: Mountain
countries: Peru
coordinates: lat: -11.56305556
lon: -76.165
Mit'u. Mit'u (Quechua for mud, hispanicized spelling &quot;Mito&quot;) is a mountain in the Andes of Peru which reaches an altitude of approximately. It is located in the Junín Region, Yauli Province, Morococha District, north of Shawaq. Mit'u lies south of the Puka Yaku River (&quot;red water&quot;, hispanicized &quot;Pucayacu&quot;), an affluent of the Mantaro River.

Geographic entities mentioned:
surface_form: mit'u
instance_of: Mountain
countries: Peru
coordinates: lat: -11.53555556
lon: -76.16694444
Mit'u. Mit'u (Quechua for mud, hispanicized spelling &quot;Mito&quot;) is a mountain in the Andes of Peru which reaches an altitude of approximately. It is located in the Junín Region, Yauli Province, Morococha District, north of Shawaq. Mit'u lies south of the Puka Yaku River (&quot;red water&quot;, hispanicized &quot;Pucayacu&quot;), an affluent of the Mantaro River.

Geographic entities mentioned:
surface_form: puka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.6339
lon: -75.5692
The letters read by Antti Litja are available on CDs. His home is somewhere to the west of Lake Päijänne, more or less equidistant from the nearest cities and towns, which appear to be Lahti, Tampere and Jyväskylä, at 300 kilometers from Helsinki, although that would place him slightly to the north of Jyväskylä and into the area of the Savo dialects, which is clearly not where he lives.

Geographic entities mentioned:
surface_form: Lake Päijänne
instance_of: Lake
countries: Finland
coordinates: lat: 61.583333333333
lon: 25.5
The most notable theological divide between Jewish and Samaritan doctrine concerns the holiest site, which the Jews believe is the Temple Mount in Jerusalem and which Samaritans identify as Mount Gerizim near modern Nablus and ancient Shechem in the Samaritan version of Deuteronomy 16:6 Both Jews and Samaritans assert that the Binding of Isaac occurred at their respective holy sites, identifying them as Moriah.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
The reference to Mount Gerizim derives from the biblical story of Moses ordering Joshua to take the Twelve Tribes of Israel to the mountains by Shechem (Nablus) and place half of the tribes, six in number, on Mount Gerizim—the Mount of the Blessing—and the other half on Mount Ebal—the Mount of the Curse. Biblical versions.

Geographic entities mentioned:
surface_form: Mount Ebal
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.234
lon: 35.2733
The defeat of the Jews in the Bar Kokhba revolt, along with the depopulation and destruction of Judea, allowed the Samaritans to expand into former Jewish areas, particularly in northern Judea, establishing themselves in places such as Emmaus and Sha'alavim. Samaritans also settled in the Beit She'an Valley and in coastal cities like Caesarea.

Geographic entities mentioned:
surface_form: Beit She'an Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.4794
lon: 35.5058
Little Bull Lake (Algoma District). Little Bull Lake is a lake in Algoma District, Ontario, Canada. It is about long and wide, and lies at an elevation of. The primary inflow is an unnamed creek from Bull Lake, and the primary outflow is an unnamed creek to Burnett Lake, which flows via Low Creek into the West River aux Sables, a tributary of the River aux Sables.

Geographic entities mentioned:
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.6872
lon: -76.9758
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.5275
lon: -93.9981
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3544
lon: -91.5747
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.105
lon: -67.383
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.55209
lon: -83.13404
surface_form: little bull lake (algoma district)
instance_of: Lake
countries: Canada
coordinates: lat: 46.4383
lon: -82.2136
surface_form: little bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0914
lon: -80.5689
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.4328
lon: -82.19
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.9103
lon: -87.3933
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.1031
lon: -80.5825
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.8981
lon: -80.5561
Little Bull Lake (Algoma District). Little Bull Lake is a lake in Algoma District, Ontario, Canada. It is about long and wide, and lies at an elevation of. The primary inflow is an unnamed creek from Bull Lake, and the primary outflow is an unnamed creek to Burnett Lake, which flows via Low Creek into the West River aux Sables, a tributary of the River aux Sables.

Geographic entities mentioned:
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.6872
lon: -76.9758
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.5275
lon: -93.9981
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3544
lon: -91.5747
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.105
lon: -67.383
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.55209
lon: -83.13404
surface_form: little bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.4383
lon: -82.2136
surface_form: little bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0914
lon: -80.5689
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.4328
lon: -82.19
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.9103
lon: -87.3933
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.1031
lon: -80.5825
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.8981
lon: -80.5561
It is about long and wide, and lies at an elevation of. The primary inflow is an unnamed creek from Bull Lake, and the primary outflow is an unnamed creek to Burnett Lake, which flows via Low Creek into the West River aux Sables, a tributary of the River aux Sables. Bull Lake is about north of the community of Massey, where the River aux Sables joins the Spanish River.

Geographic entities mentioned:
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.6872
lon: -76.9758
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.5275
lon: -93.9981
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3544
lon: -91.5747
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.105
lon: -67.383
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.55209
lon: -83.13404
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.4328
lon: -82.19
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.9103
lon: -87.3933
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.1031
lon: -80.5825
surface_form: bull lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.8981
lon: -80.5561
Barwick Valley. Barwick Valley () is an ice-free valley north of Apocalypse Peaks, extending from Webb Glacier to Victoria Valley in Victoria Land, Antarctica. A large part of the valley has been designated an Antarctic Specially Protected Area because of its pristine condition. Naming.

Geographic entities mentioned:
surface_form: Apocalypse Peaks
instance_of: Mountain
coordinates: lat: -77.3833
lon: 160.85
surface_form: Victoria Valley
instance_of: Valley
coordinates: lat: -77.383333333333
lon: 161.93333333333
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Location. The Barwick Valley is one of the McMurdo Dry Valleys. It runs southeast from the Webb Icefall to the Insel Range, where it is joined from the southwest by Balham Valley. The combined valley continues east to Victoria Valley. To the north the valley is bounded by The Fortress and other features of the Cruzen Range (formerly part of the Clare Range).

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Location. The Barwick Valley is one of the McMurdo Dry Valleys. It runs southeast from the Webb Icefall to the Insel Range, where it is joined from the southwest by Balham Valley. The combined valley continues east to Victoria Valley. To the north the valley is bounded by The Fortress and other features of the Cruzen Range (formerly part of the Clare Range).

Geographic entities mentioned:
surface_form: Balham Valley
instance_of: Valley
coordinates: lat: -77.4167
lon: 161.017
Location. The Barwick Valley is one of the McMurdo Dry Valleys. It runs southeast from the Webb Icefall to the Insel Range, where it is joined from the southwest by Balham Valley. The combined valley continues east to Victoria Valley. To the north the valley is bounded by The Fortress and other features of the Cruzen Range (formerly part of the Clare Range).

Geographic entities mentioned:
surface_form: Victoria Valley
instance_of: Valley
coordinates: lat: -77.383333333333
lon: 161.93333333333
The combined valley continues east to Victoria Valley. To the north the valley is bounded by The Fortress and other features of the Cruzen Range (formerly part of the Clare Range). To the west and southwest it is bounded by Mount Bastion, Gibson Spur and the Apocalypse Peaks of the Willett Range, and to the southeast by the Insel Range. Antarctic Specially Protected Area.

Geographic entities mentioned:
surface_form: Mount Bastion
instance_of: Mountain
coordinates: lat: -77.3167
lon: 160.483
surface_form: Gibson Spur
instance_of: Mountain
coordinates: lat: -77.333333333333
lon: 160.66666666667
surface_form: Apocalypse Peaks
instance_of: Mountain
coordinates: lat: -77.3833
lon: 160.85
This designation expired on 30 June 1981. An area of, comprising parts of both Barwick Valley and the adjacent Balham Valley, is now protected under the Antarctic Treaty System as Antarctic Specially Protected Area (ASPA) No.123 because it is one of the least disturbed or contaminated of the McMurdo Dry Valleys.

Geographic entities mentioned:
surface_form: Balham Valley
instance_of: Valley
coordinates: lat: -77.4167
lon: 161.017
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Webb Cirque. A prominent cirque at the head of Webb Glacier. The cirque is bounded by Vishniac Peak, Skew Peak, and Parker Mesa and is occupied by the névé of the Webb Glacier. Named by Advisory Committee on Antarctic Names (US-ACAN) (2005) in association with the Webb Glacier. Caffin Valley. A cirque-type valley between Mount Bastion and Gibson Spur in the Willett Range.

Geographic entities mentioned:
surface_form: Vishniac Peak
instance_of: Mountain
coordinates: lat: -77.233333333333
lon: 160.51666666667
surface_form: Skew Peak
instance_of: Mountain
coordinates: lat: -77.21666667
lon: 160.7
surface_form: Parker Mesa
instance_of: Landform
coordinates: lat: -77.25
lon: 160.917
Named by Advisory Committee on Antarctic Names (US-ACAN) (2005) in association with the Webb Glacier. Caffin Valley. A cirque-type valley between Mount Bastion and Gibson Spur in the Willett Range. Named by the NZ-APC in 1985 after James M. Caffin, New Zealand Antarctic historian who, from 1973-84, was editor of Antarctic, the popular news bulletin published by the New Zealand Antarctic Society.

Geographic entities mentioned:
surface_form: Mount Bastion
instance_of: Mountain
coordinates: lat: -77.3167
lon: 160.483
surface_form: Gibson Spur
instance_of: Mountain
coordinates: lat: -77.333333333333
lon: 160.66666666667
Named by the NZ-APC in 1985 after James M. Caffin, New Zealand Antarctic historian who, from 1973-84, was editor of Antarctic, the popular news bulletin published by the New Zealand Antarctic Society. Albert Valley. A hanging valley between Conway Peak and Wendler Spur in central Apocalypse Peaks. The valley opens north to Barwick Valley. Named by US-ACAN (2005) after Mary R.

Geographic entities mentioned:
surface_form: Conway Peak
instance_of: Mountain
coordinates: lat: -77.37027778
lon: 160.89583333
Webb Icefall. An icefall just south of Vishniac Peak that descends from Willett Range and nourishes the western tributary at the head of Webb Glacier. Named by American geologist Parker E. Calkin in association with Webb Glacier. Webb Glacier. Glacier just north of Mount Bastion and Gibson Spur, flowing southeast into the head of Barwick Valley. Named by the VUWAE (1958-59) for P.N.

Geographic entities mentioned:
surface_form: Vishniac Peak
instance_of: Mountain
coordinates: lat: -77.233333333333
lon: 160.51666666667
Named by American geologist Parker E. Calkin in association with Webb Glacier. Webb Glacier. Glacier just north of Mount Bastion and Gibson Spur, flowing southeast into the head of Barwick Valley. Named by the VUWAE (1958-59) for P.N. Webb who, with B.C. McKelvey, did the first geological exploration in this area (1957-58) and was in Wright Valley with the VUWAE in 1958-59. Walker Glacier.

Geographic entities mentioned:
surface_form: Mount Bastion
instance_of: Mountain
coordinates: lat: -77.3167
lon: 160.483
surface_form: Gibson Spur
instance_of: Mountain
coordinates: lat: -77.333333333333
lon: 160.66666666667
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Haselton Glacier. A glacier flowing east-northeast between Gibson Spur and the Apocalypse Peaks, terminating as a hanging glacier at Barwick Valley. Named by US-ACAN (2005) in association with Haselton Icefall, a heavily crevassed upper part of the glacier. Haselton Icefall. An icefall descending from the Willett Range between Gibson Spur and Apocalypse Peaks toward Webb Lake. Named by Parker E.

Geographic entities mentioned:
surface_form: Gibson Spur
instance_of: Mountain
coordinates: lat: -77.333333333333
lon: 160.66666666667
surface_form: Apocalypse Peaks
instance_of: Mountain
coordinates: lat: -77.3833
lon: 160.85
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Webb Lake. A meltwater lake at the terminus of Webb Glacier. Named in 1964 by American geologist Parker E. Calkin in association with Webb Glacier. Hourglass Lake. Small meltwater lake midway between Webb Lake and Lake Vashka. The descriptive name was given in 1964 by American geologist Parker E. Calkin and alludes to the outline of the lake. Lake Vashka.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Albert, Cold Regions Research and Engineering Laboratory, Hanover, NH, who conducted field and laboratory research to characterize ice core, firn, and snow properties from Siple Dome, from the US-ITASE traverses of West Antarctica, and from East Antarctic megadunes, 1996-2003; Member, 2002-, Polar Research Board, National Academy of Sciences; Chair 2003-, United States National Committee for the International Polar Year, 2007-08.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: siple
instance_of: Mountain
coordinates: lat: -73.433333333333
lon: -126.66666666667
The valley opens north to Barwick Valley opposite Lake Vashka. Named by US-ACAN (2005) after Gonzalo J. Hernandez, Department of Earth and Space Sciences, University of Washington, Seattle, WA; United States Antarctic Project (United States ArmyP) high-latitude atmospheric research at Amundsen-Scott South Pole and McMurdo Stations; 15 field seasons 1991-2004. LaBelle Valley.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
The glacier terminates at Barwick Valley short of reaching the south flank of Webb Glacier. Named by the New Zealand Geographic Board (2005) after Barry Walker, a geologist with Victoria University's Antarctic Expeditions (VUWAE) to this area, 1979-80, 1981-82, and 1982-83; field leader for basement geology studies at Mount Bastion. Haselton Glacier.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Haselton Icefall. An icefall descending from the Willett Range between Gibson Spur and Apocalypse Peaks toward Webb Lake. Named by Parker E. Calkin for fellow United States ArmyRP geologist George M. Haselton, who assisted Calkin in the field in this area in the 1961-62 season. Webb Lake. A meltwater lake at the terminus of Webb Glacier. Named in 1964 by American geologist Parker E.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
The valley opens south to Barwick Valley. Named by US-ACAN (2005) after James W. LaBelle, Department of Physics and Astronomy, Dartmouth College, Hanover, NH; USAP principal investigator for the study of low, middle, and high frequency auroral radio noise observed at Amundsen-Scott South Pole Station and at other observatories, 1991-2004. Berkey Valley.

Geographic entities mentioned:
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
The valley opens south to Barwick Valley. Named by US-ACAN (2005) after Frank T. Berkey, Center for Atmospheric and Space Sciences, Utah State University, Logan, UT; United States Antarctic Project (USAP) principal investigator for observation of the ionosphere from Siple Station, 1982 and 1983, and from Amundsen-Scott South Pole Station, 1984-95. Webb Icefall.

Geographic entities mentioned:
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
surface_form: siple
instance_of: Mountain
coordinates: lat: -73.433333333333
lon: -126.66666666667
Barwick Valley. Barwick Valley () is an ice-free valley north of Apocalypse Peaks, extending from Webb Glacier to Victoria Valley in Victoria Land, Antarctica. A large part of the valley has been designated an Antarctic Specially Protected Area because of its pristine condition. Naming.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Naming. Barwick Valley was named by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59) for Richard Essex Barwick (1929-2012), summer biologist with the New Zealand party of the Commonwealth Trans-Antarctic Expedition (1956–58) who worked in this area in 1957–58 and as a member of the VUWAE, 1958–59. Location. The Barwick Valley is one of the McMurdo Dry Valleys.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Antarctic Specially Protected Area. The greater part of the Barwick Valley was designated Antarctic Site of Special Scientific Interest No.3 under the Antarctic Treaty System, covering about between the Olympus Range to the south, Willett Range to the east and Clare Range to the north. It contained parts of several glaciers, a lake about connected by a stream to Lake Vashka, and exposed soils.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Named by the NZ-APC in 1985 after James M. Caffin, New Zealand Antarctic historian who, from 1973-84, was editor of Antarctic, the popular news bulletin published by the New Zealand Antarctic Society. Albert Valley. A hanging valley between Conway Peak and Wendler Spur in central Apocalypse Peaks. The valley opens north to Barwick Valley. Named by US-ACAN (2005) after Mary R.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Papitashvili Valley. A hanging valley between Wendler Spur and Besson Spur in Apocalypse Peaks. The valley opens north to Barwick Valley opposite Hourglass Lake and is ice free but for a glacier at the headwall. Named by the United States Advisory Committee on Antarctic Names (US-ACAN) (2005) after Vladimir O.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Hernandez Valley. An ice-free valley, which is the eastmost of four aligned hanging valleys in Apocalypse Peaks. The valley opens north to Barwick Valley opposite Lake Vashka. Named by US-ACAN (2005) after Gonzalo J.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
LaBelle Valley. A valley long between Peterson Terrace and Price Terrace in Cruzen Range. The valley opens south to Barwick Valley. Named by US-ACAN (2005) after James W.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Berkey Valley. A valley long on the east side of Price Terrace in Cruzen Range. The valley opens south to Barwick Valley. Named by US-ACAN (2005) after Frank T.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Webb who, with B.C. McKelvey, did the first geological exploration in this area (1957-58) and was in Wright Valley with the VUWAE in 1958-59. Walker Glacier. An attenuated glacier flowing northeast in Caffin Valley closely following the west side of Gibson Spur, Willett Range. The glacier terminates at Barwick Valley short of reaching the south flank of Webb Glacier.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
Hourglass Lake. Small meltwater lake midway between Webb Lake and Lake Vashka. The descriptive name was given in 1964 by American geologist Parker E. Calkin and alludes to the outline of the lake. Lake Vashka. A lake near the center of Barwick Valley, about east of Webb Glacier. Named by the VUWAE (1958-59) after Vashka (Vaska), a sled dog of the BrAE, 1910-13.

Geographic entities mentioned:
surface_form: barwick valley
instance_of: Valley
coordinates: lat: -77.35
lon: 161.167
New Melones Dam. New Melones Dam is an earth and rock filled embankment dam on the Stanislaus River, about west of Jamestown, California, United States, on the border of Calaveras County and Tuolumne County. The water impounded by the dam forms New Melones Lake, California's fourth-largest reservoir, in the foothills of the Sierra Nevada east of the San Joaquin Valley.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
McCall later served in the United States Agency for International Development. In the early 1990s, his efforts focused on Somalia and other humanitarian problems in the Horn of Africa. In the later 1990s, he focused on efforts at bringing peace to the African Great Lakes region, including conflicts in and among Sudan, Rwanda, the Democratic Republic of the Congo, and Zimbabwe.

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
This purchase was later ratified by Chilean courts and serves to illustrate how Chilean authorities ignored their own legal order that guaranteed Huilliche property. As result of the establishment of Chilean and European settlers, including Germans, around Bueno River, Osorno Huilliches living in the Central Valley migrated to the coastal region of Osorno.

Geographic entities mentioned:
surface_form: Central Valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
In 1842, while living in LaSalle County, Illinois, he became a member of the LDS Church. After joining the church, he became a missionary to Norwegians living in Wisconsin. Peterson led a company of Mormon pioneers to the Salt Lake Valley in 1849. He was one of the founders of Lehi in Utah Territory.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Fründenhorn. The Fründenhorn is a mountain of the Bernese Alps, overlooking Lake Oeschinen in the Bernese Oberland.

Geographic entities mentioned:
surface_form: oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
surface_form: lake oeschinen
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.498333333333
lon: 7.7269444444444
surface_form: fründenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.476944444444
lon: 7.7575
Fründenhorn. The Fründenhorn is a mountain of the Bernese Alps, overlooking Lake Oeschinen in the Bernese Oberland.

Geographic entities mentioned:
surface_form: fründenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.476944444444
lon: 7.7575
Location. Mangroves are found along the coast of Colombia and Ecuador from the Gulf of Tribugá in the north to Mompiche Bay in the south. Between these bays there are extensive stands of mangroves in the mouths of the San Juan, Naya, Guapi, Mira and Esmeraldas rivers. The largest block is the almost continuous strip from the Mataje River to Chanzará bay near Guapi.

Geographic entities mentioned:
surface_form: Naya
instance_of: Watercourse
countries: Colombia
coordinates: lat: 3.308349
lon: -77.486502
surface_form: Guapi
instance_of: Watercourse
countries: Colombia
coordinates: lat: 3.5030555555556
lon: -77.23
Between these bays there are extensive stands of mangroves in the mouths of the San Juan, Naya, Guapi, Mira and Esmeraldas rivers. The largest block is the almost continuous strip from the Mataje River to Chanzará bay near Guapi. In 1996 it was estimated that of mangroves were growing in the four Colombian Pacific coast departments.

Geographic entities mentioned:
surface_form: Mataje River
instance_of: Watercourse
countries: Ecuador
Colombia
coordinates: lat: 1.46958
lon: -78.8687