Sarmila/GeoWiki-Features huggingface dataset:
Distribution of loess. Both the thickness and the size of loess decrease from northwest to southeast. The figure shows the topography of the Chinese Loess Plateau. The loess near the Liu-p’an Mts is the thickest which is around while the loess near the Yellow River is around thick. This is related to the sorting by wind.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
This is related to the sorting by wind. When the monsoon wind and dust storm are blown from the northwest, it carries the loess of different sizes. When it arrives at the Loess Plateau, the energy of the wind starts to decrease, so it drops the largest and heaviest loess first. It continues to move towards the southeast of the Loess Plateau, the energy of the wind keeps decreasing.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
When it arrives at the Loess Plateau, the energy of the wind starts to decrease, so it drops the largest and heaviest loess first. It continues to move towards the southeast of the Loess Plateau, the energy of the wind keeps decreasing. Therefore, the finest loess materials are deposited at the southeast end of the Plateau.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
It continues to move towards the southeast of the Loess Plateau, the energy of the wind keeps decreasing. Therefore, the finest loess materials are deposited at the southeast end of the Plateau. That is why the coarsest loess is at the northwest of the Loess Plateau while the finest is at the southeast. Some studies found that the loess that formed during Middle Pleistocene is expansive and thick.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
That is why the coarsest loess is at the northwest of the Loess Plateau while the finest is at the southeast. Some studies found that the loess that formed during Middle Pleistocene is expansive and thick. Therefore, the main period for the formation of the Loess Plateau is Middle Pleistocene. Most of the loess in the west of Liupan Mountain is yellow.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Besides the variations in the wind intensity, the grain size may also affect by the aridity of the source areas. This changes the transporting distance of the sediments. During interglacial periods, the Loess Plateau retreated northwesterly while it moves towards the southeast during glacial periods. Therefore, the distance between the source areas and the Loess Plateau changes a lot.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
This changes the transporting distance of the sediments. During interglacial periods, the Loess Plateau retreated northwesterly while it moves towards the southeast during glacial periods. Therefore, the distance between the source areas and the Loess Plateau changes a lot. The grain size will increase in some northwest areas during glacial periods, even though the wind intensity does not change.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
From the mineralogical, isotopic, and chemical results, it is easy to find the provenance of the loess. Sources. The sources of loess in the Chinese Loess Plateau are the Gobi Desert and the deserts nearby, including the Tengger Desert, Badain Jaran Desert, Ulan Buh Desert, Mu Us Desert and Hobq Desert. However, the main source is the Gobi Desert.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
These data prove that the loess is from the Gobi Desert. The Gobi Desert is located at the north of the plateau. Although the distance between the Gobi Desert and the Chinese Loess Plateau is quite far, it is possible that the loess can travel such a great distance. There are a few reasons why the source of loess is from the Gobi Desert and the sand deserts.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Prevailing wind: The prevailing wind of the sand deserts and Gobi Desert are from the northwest. Since the Gobi Desert and the sand deserts are located northwest of the Chinese Loess Plateau, the prevailing wind builds a linkage for all these places. The loess can travel to the plateau through the prevailing wind.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Monsoon is also important to determine the source of loess because monsoon will affect the wind direction. There are winter monsoonal winds flowing from Mongolia because of the high-pressure cell in Siberian-Mongolia. This plays an important role in transporting dust and loess to the Loess Plateau. Dust storm: This is the most important factor.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
This plays an important role in transporting dust and loess to the Loess Plateau. Dust storm: This is the most important factor. During Spring, many strong dust storms happen in the Loess Plateau which usually last for more than two days. With a longer dust storm event, the loess can travel a longer distance. The dust storm is blown from northwest to the Loess Plateau. Origin of the loess.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
During Spring, many strong dust storms happen in the Loess Plateau which usually last for more than two days. With a longer dust storm event, the loess can travel a longer distance. The dust storm is blown from northwest to the Loess Plateau. Origin of the loess. Although the source of loess materials is from the Gobi Desert and the sand deserts, they are not produced by those deserts.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
This may even form alluvial fans. There is a huge alluvial fan at the mountain foot of the Gobi Altay Mts. Therefore, the sediments and sands of the desert are from the mountain. After that, the wind will transport the sediments to the Loess Plateau and sort the sediments. Tectonic activities: When there are tectonic activities in High Asia, energy is released.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Besides, the sediments are also produced by the eolian abrasion process in the deserts and the Yellow River. However, these are not the major sources of loess. Therefore, the loess in the Chinese Loess Plateau is mainly produced by the three mountain ranges and deposited in the deserts. Through monsoon wind and dust storms, the loess is transported to the Loess Plateau.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
However, these are not the major sources of loess. Therefore, the loess in the Chinese Loess Plateau is mainly produced by the three mountain ranges and deposited in the deserts. Through monsoon wind and dust storms, the loess is transported to the Loess Plateau. Climate and environmental changes. The population of the Loess Plateau has been increasing since the 1600s.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Through monsoon wind and dust storms, the loess is transported to the Loess Plateau. Climate and environmental changes. The population of the Loess Plateau has been increasing since the 1600s. In 2000, the population has increased to 104 million. The rapid population growth has brought some environmental problems to Loess Plateau. For instance, deforestation.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Climate and environmental changes. The population of the Loess Plateau has been increasing since the 1600s. In 2000, the population has increased to 104 million. The rapid population growth has brought some environmental problems to Loess Plateau. For instance, deforestation. People clear the forest to get more land for agriculture activities and use the wood for fuel and building materials.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
For instance, deforestation. People clear the forest to get more land for agriculture activities and use the wood for fuel and building materials. This is the reason why the forest cover has decreased dramatically. There are more and more abnormal and extreme natural hazards in the Loess Plateau. This may be related to the climate and environmental changes. Natural hazards.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
This may be related to the climate and environmental changes. Natural hazards. Different natural hazards connected with the Loess Plateau include dust storms, floods and droughts, locust swarms and landslides. The number of dust storm events is increasing and they have become stronger. The materials can be carried by the dust storm for a very long distance.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
The Loess Plateau becomes more vulnerable to locust swarms because the climate becomes cooler and more humid. They will destroy the farmland and reduce crop yield. From 1965 to 1979, more than 1000 landslides that happened in the Loess Plateau were triggered by earthquake shocks and monsoonal summer rainfall. Background. The Loess Plateau suffers from one of the world's most severe soil erosion.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Background. The Loess Plateau suffers from one of the world's most severe soil erosion. Soil erosion in the region is affected by many factors, including vegetation cover, precipitation, strength of winds, climate etc. However, human activities contribute the most to soil erosion in the Loess Plateau in recent years.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
However, human activities contribute the most to soil erosion in the Loess Plateau in recent years. It is estimated from historical records that forest cover on the Loess Plateau declined by a factor of eight during the last three millennia, reaching a low in 1949 leading to yearly soil erosion of 3700 tons of soil per km2.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Especially the northern and eastern parts of the region were once covered in forests. The population in the Chinese Loess Plateau has tripled from 1949 to 2000. It has reached 104 million people in 2000. More than 70% of slope land is used for agricultural activities. The farming activities on the steep slopes exposed the loess materials on the slope.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Also, mining and construction also contribute in causing soil erosion. Restoration projects. In 1999, the Chinese government launched the Grain for Green restoration project, backed by the World Bank and the United Nations, piloted at the Loess Plateau. The project banned hillside cropping and free grazing; farmers receive grain-and-cash subsidies to convert fields to grassland or forest.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
The first Loess Plateau restoration project cost US$252 million, as of 2007. From 1975 to 2015, restoration projects in the Beiluo River Basin, southwestern part of the Loess Plateau, restored cropland into grassland and forest, boosting forest cover by about 18% and raising the basin's overall ecosystem service value by roughly 54% (about USD 3.2 billion).

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
From the program beginning to 2020, the Jinghe River watershed area observed reclaimed forest and grassland on the hills, which improved soil and water conservation and ecosystem services. Overall, it is estimated that forest cover increased by 15,000 km² from 2007 to 2017 on the plateau. Between 2000 and 2024, the Loess Plateau changed to a warming, slightly wetter climate.

Geographic entities mentioned:
surface_form: loess plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 36.883333333333
lon: 108.71666666667
Loess Plateau. The Loess Plateau is a plateau in north-central China formed of loess, a clastic silt-like sediment formed by the accumulation of wind-blown dust. It is located southeast of the Gobi Desert and is surrounded by the Yellow River. It includes parts of the Chinese provinces of Qinghai, Gansu, Shaanxi and Shanxi.

Geographic entities mentioned:
surface_form: qinghai
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37
lon: 100
Dresden to Teplitz Post Road. The Old and New Dresden to Teplitz Post Roads () are passes over the Ore Mountains and form part of the well-known ancient road system known as the Kulmer Steig, which ran from the Elbe Valley near Dresden over the Eastern Ore Mountains to Teplitz (now Teplice), Bohemia.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Lomako River. The Lomako River is a river in Équateur province, Democratic Republic of the Congo. The Lomako is a tributary of the Maringa River. The Maringa River joins with the Lopori River to the north, to form the Lulonga River, a tributary of the Congo River.

Geographic entities mentioned:
surface_form: Maringa River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 1.228572
lon: 19.817963
The Lomako River is a river in Équateur province, Democratic Republic of the Congo. The Lomako is a tributary of the Maringa River. The Maringa River joins with the Lopori River to the north, to form the Lulonga River, a tributary of the Congo River. The Lomako flows through the Lopori / Maringa basin, also known as the Maringa-Lopori-Wamba Landscape, an area of great ecological importance.

Geographic entities mentioned:
surface_form: Lopori River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 1.236166
lon: 19.811654
It occurs in association with afwillite, calcite, larnite, spurrite, halite, brownmillerite, hydrocalumite, mayenite and ettringite. It was first described in 1933 for an occurrence at Scawt Hill, Larne, County Antrim, Northern Ireland. It was named portlandite because the chemical calcium hydroxide is a common hydration phase of Portland cement.

Geographic entities mentioned:
surface_form: Scawt Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.9105
lon: -5.9154
The Indian survey had an enormous scientific impact. It was responsible for one of the first accurate measurements of a section of an arc of longitude, and for measurements of the geodesic anomaly. It named and mapped Mount Everest and the other Himalayan peaks. Surveying became a professional occupation in high demand at the turn of the 19th century with the onset of the Industrial Revolution.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Over the 16th century, the Landstände managed the reconstruction and fortification of the city, ultimately designating Klagenfurt as the new capital of Carinthia. As early as 1527, the 4.5-kilometer-long Lend Canal was constructed to supply the city with water from Lake Wörthersee, to feed the city moat, which began excavation in 1534, and to serve as a transport route for building materials.

Geographic entities mentioned:
surface_form: Wörthersee
instance_of: Lake
countries: Austria
coordinates: lat: 46.625
lon: 14.15
The cellar was adorned with murals created by local Carinthian artists, including Eduard Manhart's &quot;Ankogel,&quot; Switbert Lobisser's &quot;Kirchgang,&quot; &quot;Keusche am Berg,&quot; and &quot;Kärntnerhimmel,&quot; Josef Prokop's &quot;Schimmelreiten im Gurktal,&quot; and Richard Knaus's &quot;Stern- oder Dreikönigssingen in Paternion&quot; and &quot;Bandltanz.&quot; Unfortunately, all of the paintings except Lobisser’s “Carinthian Sky” were lost in a fire in 1949 and during renovations in 1969.

Geographic entities mentioned:
surface_form: Ankogel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.05111111111111
lon: 13.248611111111112
Although the name suggests that they are located in the Berner Oberland region of the canton of Bern, portions of the Bernese Alps are in the adjacent cantons of Valais, Fribourg and Vaud, the latter being usually named &quot;Fribourg Alps&quot; and &quot;Vaud Alps&quot; respectively. The highest mountain in the range, the Finsteraarhorn, is also the highest point in the canton of Bern.

Geographic entities mentioned:
surface_form: Finsteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.537472222222
lon: 8.1260277777778
The Rhône valley separates them from the Chablais Alps in the west and from the Pennine Alps in the south; the upper Rhône valley separates them from the Lepontine Alps to the southeast; the Grimsel Pass and the Aare valley separates them from the Uri Alps in the east, and from the Emmental Alps in the north; their northwestern edge is not well defined, describing a line roughly from Lake Geneva to Lake Thun.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: Lake Thun
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.683333333333
lon: 7.7166666666667
The principal ridge, a chain that runs from west (Dent de Morcles) to east (Sidelhorn), whose highest peak is the Finsteraarhorn, forms the watershed between the cantons of Bern and Valais. Except for the westernmost part, it is also the watershed between the Rhine (North Sea) and the Rhône (Mediterranean Sea).

Geographic entities mentioned:
surface_form: Dent de Morcles
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.198888888889
lon: 7.0758333333333
surface_form: Sidelhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.552388888889
lon: 8.3126944444444
surface_form: Finsteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.537472222222
lon: 8.1260277777778
There the mountains progressively become lower and disappear into the hilly Swiss Plateau. The Bernese Alps have a large influence on the climate of Switzerland: while their north side is very exposed to weather, their south side is protected from it.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
It also marks the separation between two distinct sections of the Bernese Alps: the chain west of Gemmi Pass, consisting mainly of foothills with a few large glacier-covered mountains (notably Dent de Morcles, Grand Muveran, Diablerets, Wildhorn and Wildstrubel) around, and the chain east of Gemmi Pass, consisting mainly of summits around on several subranges, with large valley glaciers between them.

Geographic entities mentioned:
surface_form: Grand Muveran
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.237222222222
lon: 7.1261111111111
surface_form: Diablerets
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.303888888889
lon: 7.1891666666667
surface_form: Wildhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.354583333333
lon: 7.3608611111111
surface_form: Wildstrubel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.400277777778
lon: 7.5286111111111
Thus the Tschingel Glacier and the Kander Glacier, separate the portion of the main range lying between the Gemmi Pass and the Mittaghorn from the equally high parallel range of the Doldenhorn and Blümlisalp on its northern side.

Geographic entities mentioned:
surface_form: Doldenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.468611111111
lon: 7.735
To the south, the same portion of the main range is divided from the still higher parallel range whose summits are the Aletschhorn and the Bietschhorn by the Lötschental and the Lötschenlücke. To this again succeeds the deep trench through which the lower part of the Aletsch Glacier flows down to the Rhône, enclosed by the minor ridge that culminates at the Eggishorn.

Geographic entities mentioned:
surface_form: Aletschhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.465277777778
lon: 7.9936111111111
surface_form: Bietschhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.39125
lon: 7.850075
surface_form: Lötschental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.416666666667
lon: 7.8333333333333
To the south, the same portion of the main range is divided from the still higher parallel range whose summits are the Aletschhorn and the Bietschhorn by the Lötschental and the Lötschenlücke. To this again succeeds the deep trench through which the lower part of the Aletsch Glacier flows down to the Rhône, enclosed by the minor ridge that culminates at the Eggishorn.

Geographic entities mentioned:
surface_form: Eggishorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.427222222222
lon: 8.0933333333333
Notwithstanding the activity of their predecessors, the members of the English Alpine Club have found scope for further exploits, amongst which may be reckoned the first ascents of the Aletschhorn and the Schreckhorn, and the still more arduous enterprise of crossing the range bypasses, such as the Jungfraujoch and Eigerjoch, which are considered among the most difficult in the Alps.

Geographic entities mentioned:
surface_form: Aletschhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.465277777778
lon: 7.9936111111111
surface_form: Schreckhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.58993
lon: 8.11816
The Jungfrau-Aletsch area is located in the eastern Bernese Alps in the most glaciated region of the Alps. It was inscribed as a UNESCO World Heritage Site (&quot;Swiss Alps Jungfrau-Aletsch&quot;) in 2001 and further expanded in 2007. Its name comes from the Aletsch Glacier and the two summits of the Jungfrau and Bietschhorn, which constitute some of the most impressive features of the site.

Geographic entities mentioned:
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
surface_form: Bietschhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.39125
lon: 7.850075
Brewster Hill, New York. Brewster Hill is a hamlet (and census-designated place) located in the town of Southeast in Putnam County, New York, United States. As of the 2010 census, the population was 2,089. Brewster Hill is located on the eastern side of Tonetta Lake and is east of Interstate 84. Geography. Brewster Hill is located at (41.422880, -73.604277).

Geographic entities mentioned:
surface_form: Tonetta Lake
instance_of: Lake
countries: United States
coordinates: lat: 41.421111111111
lon: -73.610833333333
Geography. Au Sable Forks is located on the border of Clinton and Essex counties at (44.444063, −73.676013), centered on the point where the West Branch and the East Branch of the Au Sable River join to form the main confluence which flows into Au Sable Chasm and thence, into Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Owned by: Max and Rex (D-Team)
Other Info: It also fights against Seth's Black Tyrannosaurus. First Activated: The egg that its card was in is opened underwater. Found in place: In Loch Ness, Scotland
Other Info: It was first mistakenly believed to be the Loch Ness Monster by the local Scottish. First Activated: Lightning strikes the area the egg containing its card and Move Card in.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
She has shadow directed on Showtime's &quot;Dexter&quot; (with Steve Shill) and TNT's &quot;Leverage&quot; (with Rod Hardy.)
In 2008, Heck traveled to the tallest peak in the world, Mount Everest, where she lived with a professional climbing team as part of her research for an upcoming feature film. She currently lives in New York City and resides part-time in Los Angeles, California.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Priest. Pilgrim was of old Bavarian stock, a member of the Aribonid and Sighardinger kin groups, whose members had at times held the bishopric of Freising in the past. He was already a clergyman when in 889 King Arnulf of Germany granted him a large forest, the Zillertal, which remained under the lordship of the rulers of Salzburg until 1810.

Geographic entities mentioned:
surface_form: Zillertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.333333333333
lon: 11.866666666667
Besh-Tash Lake. Besh-Tash Lake () is a rock-dammed lake in Talas Province of Kyrgyzstan. It is located at the altitude of about 3,000 m in riverbed of Besh-Tash river, left tributary of Talas River.

Geographic entities mentioned:
surface_form: besh-tash lake
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.20638889
lon: 72.49611111
Kimberly Dilts. Kimberly Dilts is an American actress and filmmaker, most known for producing &quot;Angel's Perch&quot;. Early life. Born in New York, she attended the University of Texas in Austin where she gained a M.F.A in acting. Career. Initially working in her theatre, she produced, wrote and starred in a tour of &quot;Abby & June&quot;, a two-person play about travel and identity.

Geographic entities mentioned:
surface_form: Angel's Perch
instance_of: Mountain
countries: United States
coordinates: lat: 43.7972
lon: -114.067
She also provided voice work for &quot;The Princess Blade&quot; and &quot;Sakura Wars&quot;. &quot;Angel's Perch&quot;. In 2013, Dilts produced the movie &quot;Angel's Perch&quot;. &quot;Tired of waiting for the phone to ring,&quot; she and her husband, writer and producer J.T. Arbogast, decided to make the film themselves.

Geographic entities mentioned:
surface_form: Angel's Perch
instance_of: Mountain
countries: United States
coordinates: lat: 43.7972
lon: -114.067
Seven years later, Kennicott moved with his wife and two sons to Northfield Township, Cook County, Illinois, an area that was almost completely undeveloped. He made a claim of several hundred acres south of Half Day between Lake Michigan and the Des Plaines River. Naming his homestead &quot;The Grove&quot; for the abundance of trees, Kennicott built a house on it around 1856.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Tundavala Gap. Tundavala Gap (Portuguese: &quot;Fenda da Tundavala&quot;) is a canyon on the escarpment of the Serra da Leba near Lubango, Huíla Province, Angola. The escarpment marks the western limit of the Humpata Plateau, part of the Great Escarpment of Southern Africa, and creates a natural boundary between Huíla Province and Namibe Province.

Geographic entities mentioned:
surface_form: Serra da Leba
instance_of: Mountain
Plateau
countries: Angola
coordinates: lat: -15.07108333
lon: 13.24863889
Geography. Tundavala Gap is located about from Lubango, in the Huíla Province of Angola. It sits on the western edge of the Humpata Plateau, an extension of the Huíla Plateau, inside the Serra da Leba mountain range. It opens westward towards Namibe Province, overlooking northwest towards Moçâmedes. At its peak, Tundavala Gap reaches a height of about, and its cliffs are about deep.

Geographic entities mentioned:
surface_form: Serra da Leba
instance_of: Mountain
Plateau
countries: Angola
coordinates: lat: -15.07108333
lon: 13.24863889
Smith Reservoir (Costilla County, Colorado). Smith Reservoir is located in Costilla County, Colorado, south of Blanca in the San Luis Valley. The reservoir is owned by the Trinchera Irrigation Company. Dam. The rockfill dam, Smith Dam, was built in 1914 and — according to the National Inventory of Dams — stores of water. It impounds Trinchera Creek.

Geographic entities mentioned:
surface_form: San Luis Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
In 1663, Charguaje and Tama Indians attacked Mocoa and &quot;shattered all the crosses that they found&quot;. In Santafé, with the help of the syndic Francisco de Caldas Barboza, he opened the first public slaughterhouse, finished the building of the tower and the porch at the Catedral Primada de Colombia and built bridges over the rivers San Agustín, San Francisco and Funza. Death.

Geographic entities mentioned:
surface_form: Funza
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
Valinda, California. Valinda is a census-designated place (CDP) in the San Gabriel Valley, in Los Angeles County, California, in the United States. At the 2020 census, the population was 22,437, down from 22,822 at the 2010 census. Geography. Valinda is located at (34.037760, -117.928939). According to the United States Census Bureau, the CDP has a total area of, all land. Demographics.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Significance. It is one of the shrines of the 275 Paadal Petra Sthalams - Shiva Sthalams glorified in the early medieval &quot;Tevaram&quot; poems by Tamil Saivite Nayanars Tirunavukkarasar and Sundarar. It is the 88th Paadal Petra Sthalam and the 34th Sthalam on the north side of the river Kaveri in the Chola country.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
History. From 1770 to 1794, the Karlsschule was the only university in Stuttgart. Since its founding in 1818, Stuttgart's oldest university has been the University of Hohenheim. The eruption of the Indonesian volcano Mount Tambora in 1815 triggered a global climate change and was one of the causes of the massive famine suffered in the Kingdom of Württemberg at the beginning of the 19th century.

Geographic entities mentioned:
surface_form: Mount Tambora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.2452777777778
lon: 117.99277777778
Cumberland Plateau salamander. The Cumberland Plateau salamander (&quot;Plethodon kentucki&quot;) is a species of salamander in the family Plethodontidae. It is endemic to the Cumberland Plateau, the southeastern United States. Its natural habitat is temperate forests. It is threatened by habitat loss. Description.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
This species likely hybridizes with &quot;Plethodon glutinosus&quot;; hybridization is common with other members of the slimy salamander complex. Distribution. Found in the Cumberland plateau in eastern Kentucky, western West Virginia, northern Tennessee and western Virginia, the species is not found east of the Kanawha and New rivers.

Geographic entities mentioned:
surface_form: Cumberland plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Kemp, a friend of the Duke and Duchess, knew nothing of the letter, and Wagner and the solicitors confirmed it was a forgery. The mystery was never solved, but it was apparently connected with an incident where the Duke went hunting with hawks at Devil's Dyke and forced a farmer to move his sheep elsewhere. Wagner's churches.

Geographic entities mentioned:
surface_form: Devil's Dyke
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.885
lon: -0.205
Alpinism. Dent's first ascents in the Alps include the Lenzspitze (4,294 m) in the Pennine Alps in August 1870, with Alexander Burgener and a porter, Franz Burgener (of whom Dent wrote 'his conversational powers were limited by an odd practice of carrying heavy parcels in his mouth'), and the Portjengrat (Pizzo d'Andollo, 3,654 m) above the valley of Saas-Fee in 1871.

Geographic entities mentioned:
surface_form: Lenzspitze
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.104638888889
lon: 7.8684444444444
On 5 September 1872 the combined parties of Dent and guide Alexander Burgener, with George Augustus Passingham, and his guides Ferdinand Imseng and Franz Andermatten, made the first ascent of the south-east ridge of the Zinalrothorn (4,221 m); this is the current &quot;voie normale&quot; on the mountain.

Geographic entities mentioned:
surface_form: Zinalrothorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.064722222222
lon: 7.69
Dent may have been the first person to have written – in his book &quot;Above the Snow Line&quot; (1885) – that an ascent of Mount Everest was possible.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Gooimeer. The Gooimeer (Gooi Lake) is a bordering lake in the Netherlands between the southeastern part of North Holland (the Gooi) and Flevoland. There is a railroad bridge over the narrow west side, between Weesp and Almere Poort, with a parallel highway bridge, the Hollandse Brug. The narrow eastern border of the lake is crossed by two parallel highway bridges.

Geographic entities mentioned:
surface_form: gooimeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.321389
lon: 5.206389
The narrow eastern border of the lake is crossed by two parallel highway bridges. On the south bank of Gooimeer, which used to be the IJsselmeer, before the creation of the new polder Flevoland, the old cities of Naarden and Huizen can be found. The Naarderwoonbos, part of the Naarderbos, was built in the eighties. It is situated directly adjacent to the southern shore of the Gooimeer.

Geographic entities mentioned:
surface_form: gooimeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.321389
lon: 5.206389
The Naarderwoonbos, part of the Naarderbos, was built in the eighties. It is situated directly adjacent to the southern shore of the Gooimeer. The Gooimeer is related to the crash of El Al Flight 1862 in 1992, as the two right-hand side jet engines of the Boeing 747-200F serving the route separated from the plane and fell into the lake, witnessed by a fishing off-duty police officer.

Geographic entities mentioned:
surface_form: gooimeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.321389
lon: 5.206389
Of the agricultural land, 22.6% is used for growing crops and 10.1% is pastures, while 3.5% is used for orchards or vine crops. The municipality is located on the right bank of Lake Geneva between Bellevue and Versoix. It consists of the village of Genthod and the hamlets of Malagny and Creux-de-Genthod. It is home to the Creux-de-Genthod yacht club.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Geography. It is located at, above sea level. Location. National Highway 49 passes through Bangriposi. The town is surrounded by Similipal National park. The temple of Goddess Maa Dwarasuni is situated here. Budhabalanga river passes through Bangriposi. Bangriposi railway station serves with all the necessary facilities to the peoples. It has a great role in promoting tourism here. Demographics.

Geographic entities mentioned:
surface_form: Budhabalanga river
instance_of: Watercourse
countries: India
coordinates: lat: 21.469543
lon: 87.065675
Behrent was born in Oamaru in 1990. She received her schooling at Southland Girls' High School in Invercargill. Behrent had planned to start her tertiary education at the University of Otago in 2010 when she received her call to the New Zealand rowing squad. She moved to Cambridge to be at the New Zealand training centre at Lake Karapiro and studied at the University of Waikato instead. Rowing.

Geographic entities mentioned:
surface_form: Lake Karapiro
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.943167
lon: 175.560833
Rowing. She never took up rowing while at high school; it was at Lake Ruataniwha in November 2008 when she supported her younger brother at a rowing regatta that she was asked by Southland coach John O'Connor whether she wanted to try rowing herself as she had the right physical attributes.

Geographic entities mentioned:
surface_form: Lake Ruataniwha
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.281
lon: 170.071
It is unclear if Arduin was appointed to Ivrea by the king–emperor Otto III or if he succeeded as Conrad's heir. The March of Ivrea, since its restructuring under Berengar II in 950, consisted of the counties of Burgaria, Ivrea, Lomello, Ossola, Pombia, Stazzona, and Vercelli, and the dioceses of Ivrea, Novara, Vercelli, and Vigevano, plus part of the dioceses of Pavia and Milan.

Geographic entities mentioned:
surface_form: Ossola
instance_of: Valley
countries: Italy
coordinates: lat: 46.283333333333
lon: 8.35
As confidence in Arduin waned from this time on, Henry's power prevailed everywhere.&quot;
King in the northwest. At this point, Henry was satisfied by his formal recognition as ruler of Italy and returned to Germany in the early summer of 1004. Arduin had withdrawn to his stronghold in the Orco Valley, and Henry chose not to pursue him with the main body of his army.

Geographic entities mentioned:
surface_form: Orco Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.417
lon: 7.467
Geography. Mezzocorona is located in the Rotaliana Plain, an alluvial plain situated at the confluence of the Non Valley with the Etschtal. The village lies at the foot of a steep rocky mountain wall (&quot;Monte di Mezzocorona&quot;) that shields it from the cold northern winds.

Geographic entities mentioned:
surface_form: Non Valley
instance_of: Valley
countries: Italy
coordinates: lat: 46.366666666667
lon: 11.033333333333
surface_form: Etschtal
instance_of: Valley
countries: Italy
coordinates: lat: 46.07
lon: 11.12
In World War I, as Lieutenant general, he commanded first the 10th Division and later the 4th Division. On 23 May 1916, he was placed at the head of the XX Army Corps, with which he fought on the Monte Piana and in the Battle of Mount Ortigara. In August 1917, he led the II Army Corps during the Eleventh Battle of the Isonzo.

Geographic entities mentioned:
surface_form: Monte Piana
instance_of: Mountain
countries: Italy
coordinates: lat: 46.61527778
lon: 12.23944444
Cox Bluff (Tasmania). Cox Bluff is the ocean end of the New Harbour Range, on the south coast of Tasmania. It is situated on the west side of Cox Bight, and east of New Harbour, located at the south-west corner of Tasmania, Australia.

Geographic entities mentioned:
surface_form: cox bluff (tasmania)
instance_of: Mountain
countries: Australia
coordinates: lat: -43.5242
lon: 146.2
Cox Bluff (Tasmania). Cox Bluff is the ocean end of the New Harbour Range, on the south coast of Tasmania. It is situated on the west side of Cox Bight, and east of New Harbour, located at the south-west corner of Tasmania, Australia.

Geographic entities mentioned:
surface_form: cox bluff
instance_of: Mountain
countries: Australia
coordinates: lat: -43.5242
lon: 146.2
There are at least a dozen pygmy groups, sometimes unrelated to each other. The best known are the Mbenga (Aka and Baka) of the western Congo Basin, who speak Bantu and Ubangian languages; the Mbuti (Efe &quot;etc.&quot;) of the Ituri Rainforest, who speak Bantu and Central Sudanic languages, and the Twa of the African Great Lakes, who speak Bantu Rundi and Kiga.

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
Frank Kingdon-Ward in the early 20th century reported a tribe of pygmy Tibeto-Burman speakers known as the Taron inhabiting the remote region of Mt. Hkakabo Razi in Southeast Asia on the border of China (Yunnan and Tibet), Burma, and India. A Burmese survey done in the 1960s reported a mean height of an adult male Taron at and that of females at.

Geographic entities mentioned:
surface_form: Hkakabo Razi
instance_of: Mountain
countries: Myanmar
coordinates: lat: 28.333055555556
lon: 97.466666666667
Great White Pagoda. The Great White Pagoda (), or Sarira Stupa of Tayuan Temple, is a brick stupa located at Mount Wutai of Wutai County, Shanxi province, China. History. The stupa was constructed during the Wanli reign of the Ming dynasty (1368&ndash;1644 AD), as recorded on a stone tablet there composed by the high minister Zhang Juzheng (1525&ndash;1582). Architectural features.

Geographic entities mentioned:
surface_form: Mount Wutai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 39.081388888889
lon: 113.56694444444
&quot;Gorleston&quot; escorted Arabian Sea convoys until transferred to Colombo in June 1945. &quot;Gorleston&quot; spent the remainder of the war escorting Bay of Bengal convoys in support of Operation Zipper. &quot;Gorleston&quot; was returned to the United States on 23 April 1946 and re-designated USCGC &quot;Itasca&quot; until scrapped in 1950.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
In 1724 he became the first rector of the rebuilt St Mary-le-Strand, London. In the summer of 1725 he took his family to Geneva, where he left his sons to learn French. In the following year his second son Charles was drowned in the River Rhône in the rapid water where it runs out of Lake Geneva. Heylyn gained a Doctor of Divinity in 1728. He became chaplain in ordinary to George II.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Thus the Gauls find themselves continually chased and delayed by the Romans, but are assisted by the hotel manager Petitsuix, bank manager Zurix, and some Helvetian veterans who hold a celebration at Lake Geneva.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Since it was so unusual, English workers were brought over to build the house, which early on earned the disparaging local nickname of &quot;Mud House&quot;. The concrete used for the precast blocks was Rosendale cement, made at what is now the Register-listed Snyder Estate Natural Cement Historic District in Rosendale, further north in the Hudson Valley.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Some researchers postulated that the cache might have represented a large habitation camp; a hunting toolkit, buried and then dug up for seasonal stalking of game; a ceremonial or funeral site; or a ritual offering to stave off ecological harm brought on by the eruption of nearby Glacier Peak, 11,250 radiocarbon years BP, even though the presence of large amounts of debitage and fragmented bone is a good indicator that the site didn't represent a cache at all and the Glacier Peak eruption is thought to have occurred over two centuries before the emergence of the Clovis culture.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
Jack Oyugi. Jack Oyugi is an entrepreneur from Kenya known for developing Aquaprotein animal feed from water hyacinth, an invasive species in Lake Victoria. Oyugi worked as a dairy farm manager and observed that water hyacinth would be consumed by cows up to the point where it became inundated with heavy metals.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Located in the central part of the state, it stands at an altitude of above sea level, on the banks of the Río Mololoa and the Río Tepic, approximately north-west of Guadalajara, Jalisco. Nearby are the volcanoes of San Juan, Las Navajas, and Sangangüey. Tepic is the primary urban center of this rich agricultural region; major crops include sugarcane, tobacco and citrus fruits.

Geographic entities mentioned:
surface_form: Sangangüey
instance_of: Mountain
countries: Mexico
coordinates: lat: 21.4504
lon: -104.733
Albreda Lake. Albreda Lake is a lake in Thompson-Nicola Regional District in the Interior region of British Columbia, Canada. It is in the Pacific Ocean drainage basin. The primary inflow, at the northeast, and outflow, at the southeast, is the Albreda River, which flows via the North Thompson River, the Thompson River and the Fraser River to the Pacific Ocean.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: albreda lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.630277777778
lon: -119.15777777778
The locality of Albreda is to the north, and both British Columbia Highway 5 and the Canadian National Railway transcontinental main line (used by freight traffic and the Via Rail &quot;Canadian&quot; train) pass by to the east of the eastern shore of the lake.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556