Sarmila/GeoWiki-Features huggingface dataset:
Georges Mills, New Hampshire. Georges Mills is an unincorporated community in the town of Sunapee in Sullivan County, New Hampshire, United States. It is located in the northeastern corner of the town, between the northern end of Lake Sunapee and the south shore of Otter Pond. New Hampshire Route 11 runs through the village, leading east to New London and south to the center of Sunapee.

Geographic entities mentioned:
surface_form: Lake Sunapee
instance_of: Lake
countries: United States
coordinates: lat: 43.375833333333
lon: -72.056388888889
Utikuma Lake. Utikuma Lake is a large lake in north-central Alberta, Canada. It is located north of the Lesser Slave Lake, between the Bicentennial Highway and Highway 750. It has a total surface of with island area. The shallow lake (maximum depth is) lies at an elevation of. It is drained by the Utikuma River and then Wabasca River to Peace River.

Geographic entities mentioned:
surface_form: Lesser Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.440556
lon: -115.488611
It has a total surface of with island area. The shallow lake (maximum depth is) lies at an elevation of. It is drained by the Utikuma River and then Wabasca River to Peace River. The name &quot;Uticuma&quot; is Cree for &quot;big whitefish&quot;. The &quot;Utikoomak Lake 155&quot; indian reserve of the Whitefish Lake First Nations is established on the northern shore.

Geographic entities mentioned:
surface_form: whitefish lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.3342
lon: -101.6098
surface_form: whitefish lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.9064
lon: -77.405
surface_form: whitefish lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.218
lon: -90
Utikuma Lake. Utikuma Lake is a large lake in north-central Alberta, Canada. It is located north of the Lesser Slave Lake, between the Bicentennial Highway and Highway 750. It has a total surface of with island area. The shallow lake (maximum depth is) lies at an elevation of. It is drained by the Utikuma River and then Wabasca River to Peace River.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Utikuma Lake. Utikuma Lake is a large lake in north-central Alberta, Canada. It is located north of the Lesser Slave Lake, between the Bicentennial Highway and Highway 750. It has a total surface of with island area. The shallow lake (maximum depth is) lies at an elevation of. It is drained by the Utikuma River and then Wabasca River to Peace River.

Geographic entities mentioned:
surface_form: utikuma lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.833333333333
lon: -115.41666666667
Johns Mountain. Johns Mountain is a summit in the U.S. state of Georgia. With an elevation of, Johns Mountain is the 666th highest summit in the state of Georgia. The mountain is located inside the Chattahoochee-Oconee National Forest. Johns Mountain was named in honor of John Fields, a local Cherokee Indian.

Geographic entities mentioned:
surface_form: johns mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.521388888889
lon: -85.144166666667
surface_form: johns mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.05065
lon: -74.1807
Johns Mountain. Johns Mountain is a summit in the U.S. state of Georgia. With an elevation of, Johns Mountain is the 666th highest summit in the state of Georgia. The mountain is located inside the Chattahoochee-Oconee National Forest. Johns Mountain was named in honor of John Fields, a local Cherokee Indian.

Geographic entities mentioned:
surface_form: chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
against you,&quot; to apply to Pharaoh's driving Moses out from his presence, as well as to Pharaoh's intention to curse Moses when Pharaoh said in Exodus 10:10, &quot;So be the Lord with you.&quot; Thus, Pharaoh sought forgiveness in Exodus 10:17, asking Moses, &quot;Now therefore forgive, I pray, my sin only this once.&quot;
The Mekhilta of Rabbi Ishmael called the east wind with which God brought the plague of the locusts in Exodus 10:13 &quot;the mightiest of winds.&quot; The Mekhilta of Rabbi Ishmael taught that God used the east wind to punish the generation of the Flood, the people of the Tower of Babel, the people of Sodom, the Egyptians in Exodus 10:13, the Tribes of Judah and Benjamin, the Ten Tribes, Tyre, a wanton empire, and the wicked of Gehinnom.

Geographic entities mentioned:
surface_form: Gehinnom
instance_of: Valley
countries: Israel
coordinates: lat: 31.76916667
lon: 35.22805556
But those on their way to appoint a Sabbath station to set the limits of where they may travel on the Sabbath must return immediately to destroy the leaven. Similarly, those who left Jerusalem and recollected that they had consecrated meat with them, if they had passed Mount Scopus, they burned it where they were.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Climbing. The John Muir Trail, which passes below the western base of the peak, provides a climbing approach option. The first ascent of the summit was made August 14, 1922, by Chester Versteeg and Rudolph Berls by ascending the Northwest Ridge and descending the Southwest Slope. The North Slope was first climbed by Fred L. Jones on October 6, 1948.

Geographic entities mentioned:
surface_form: Chester Versteeg
instance_of: Mountain
countries: United States
coordinates: lat: 36.64769
lon: -118.32557
Mount Bolton Brown. Mount Bolton Brown is a mountain summit located on the shared border of Fresno County and Inyo County in California, United States. Description. The peak is set on the crest of the Sierra Nevada mountain range, just south of the Palisades area. It is also situated on the boundary shared by Kings Canyon National Park and John Muir Wilderness.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount bolton brown
instance_of: Mountain
countries: United States
coordinates: lat: 37.04632
lon: -118.44121
Mount Bolton Brown. Mount Bolton Brown is a mountain summit located on the shared border of Fresno County and Inyo County in California, United States. Description. The peak is set on the crest of the Sierra Nevada mountain range, just south of the Palisades area. It is also situated on the boundary shared by Kings Canyon National Park and John Muir Wilderness.

Geographic entities mentioned:
surface_form: mount bolton brown
instance_of: Mountain
countries: United States
coordinates: lat: 37.04632
lon: -118.44121
It is also situated on the boundary shared by Kings Canyon National Park and John Muir Wilderness. Mount Bolton Brown ranks as the 64th-highest peak in California. Precipitation runoff from this mountain drains east to Tinemaha Reservoir via Tinemaha Creek; south into headwaters of South Fork Kings River; and northwest to Palisade Creek which is a tributary of the Middle Fork Kings River.

Geographic entities mentioned:
surface_form: mount bolton brown
instance_of: Mountain
countries: United States
coordinates: lat: 37.04632
lon: -118.44121
The necessary closure of the old branch would have caused the water pressure in the main stream to rise significantly, with the result of flooding the island of Nonnenwerth. The island lies morphologically immediately before the Rhine emerges from the Rhenish Slate Mountains in the Lower Rhine Bay and is thus placed at the beginning of the transition from the Middle Rhine to the Lower Rhine.

Geographic entities mentioned:
surface_form: Middle Rhine
instance_of: Valley
countries: Germany
coordinates: lat: 50.364166666667
lon: 7.6055555555556
Mount Bessan. is located on the border of Gujō, Gifu Prefecture, and Hakusan, Ishikawa Prefecture, Japan, and rises to a height of. There are two triangulation stations at the top of the mountain. Mount Haku can be seen from the north. Bessan Shrine (別山神社 &quot;Bessan Jinja&quot;) is a short distance from the peak. This area is part of Hakusan National Park. (Note: there is also a Mt.

Geographic entities mentioned:
surface_form: mount bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
Bessan in located in Toyama Prefecture.)
History. Mount Haku has been climbed for religious purposes for centuries. One popular hiking route from the Gifu Prefecture side of the mountains to Mount Haku's peak runs through Mount Bessan. Mount Bessan, whose name means &quot;Separate Mountain,&quot; received its name because it is slightly separated from the south side of Mount Haku.

Geographic entities mentioned:
surface_form: mount bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
surface_form: mount bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
Bessan in located in Toyama Prefecture.)
History. Mount Haku has been climbed for religious purposes for centuries. One popular hiking route from the Gifu Prefecture side of the mountains to Mount Haku's peak runs through Mount Bessan. Mount Bessan, whose name means &quot;Separate Mountain,&quot; received its name because it is slightly separated from the south side of Mount Haku.

Geographic entities mentioned:
surface_form: mount bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
Geography. Though Mount Haku, the main peak in the Ryōhaku Mountains, was created by an active stratovolcano, Mount Bessan is made up of sedimentary rock. On the southern face of the mountain is a rock wall called the Taihei Wall (太平壁 &quot;Taihei-kabe&quot;). Near the peak of the mountain is the tree line made up of Siberian Dwarf Pines. In the beginning of summer, alpine plants like anemones.

Geographic entities mentioned:
surface_form: mount bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
Mount Bessan. is located on the border of Gujō, Gifu Prefecture, and Hakusan, Ishikawa Prefecture, Japan, and rises to a height of. There are two triangulation stations at the top of the mountain. Mount Haku can be seen from the north. Bessan Shrine (別山神社 &quot;Bessan Jinja&quot;) is a short distance from the peak. This area is part of Hakusan National Park. (Note: there is also a Mt.

Geographic entities mentioned:
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
There are two triangulation stations at the top of the mountain. Mount Haku can be seen from the north. Bessan Shrine (別山神社 &quot;Bessan Jinja&quot;) is a short distance from the peak. This area is part of Hakusan National Park. (Note: there is also a Mt. Bessan in located in Toyama Prefecture.)
History. Mount Haku has been climbed for religious purposes for centuries.

Geographic entities mentioned:
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
Mount Bessan, whose name means &quot;Separate Mountain,&quot; received its name because it is slightly separated from the south side of Mount Haku. To the south of Mount Bessan is a small flat area called the Bessan Plain (別山平 &quot;Bessan Hira&quot;) and Lake Mitarashi (御手洗池 &quot;Mitarashi Ike&quot;).

Geographic entities mentioned:
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
To the south of Mount Bessan is a small flat area called the Bessan Plain (別山平 &quot;Bessan Hira&quot;) and Lake Mitarashi (御手洗池 &quot;Mitarashi Ike&quot;). Near the lake are the ruins for the Bessan Room (別山室 &quot;Bessan-ya&quot;), which was used as a rest house for those making the pilgrimage up the mountain. Geography.

Geographic entities mentioned:
surface_form: bessan
instance_of: Mountain
countries: Japan
coordinates: lat: 36.10555556
lon: 136.76555556
The Klintzkopf is part of a nature reserve and it only can be accessed from July to November. It hosts the highest beech forest of the Vosges Mountains. To the northwest lies the Lauchenkopf. Access to the summit. The summit of the Klintzkopf can be accessed on foot from the nearby Route des Crêtes. It offers a good point of view of the southern part of the Vosges Mountains.

Geographic entities mentioned:
surface_form: Lauchenkopf
instance_of: Mountain
countries: France
coordinates: lat: 47.95611111
lon: 7.03944444
Klintzkopf. The Klintzkopf, located in the French region of Alsace, is the fifth-highest summit of the Vosges Mountains. Geography. The mountain is divided between the French municipalities of Guebwiller and Munster (department of Haut-Rhin, Alsace). The Klintzkopf is part of a nature reserve and it only can be accessed from July to November.

Geographic entities mentioned:
surface_form: klintzkopf
instance_of: Mountain
countries: France
coordinates: lat: 47.94944444
lon: 7.05611111
Geography. The mountain is divided between the French municipalities of Guebwiller and Munster (department of Haut-Rhin, Alsace). The Klintzkopf is part of a nature reserve and it only can be accessed from July to November. It hosts the highest beech forest of the Vosges Mountains. To the northwest lies the Lauchenkopf. Access to the summit.

Geographic entities mentioned:
surface_form: klintzkopf
instance_of: Mountain
countries: France
coordinates: lat: 47.94944444
lon: 7.05611111
The Klintzkopf is part of a nature reserve and it only can be accessed from July to November. It hosts the highest beech forest of the Vosges Mountains. To the northwest lies the Lauchenkopf. Access to the summit. The summit of the Klintzkopf can be accessed on foot from the nearby Route des Crêtes. It offers a good point of view of the southern part of the Vosges Mountains.

Geographic entities mentioned:
surface_form: klintzkopf
instance_of: Mountain
countries: France
coordinates: lat: 47.94944444
lon: 7.05611111
He is founder and CEO of the publishing company Amstel Music, which he established in 1989. When not traveling, de Meij divides his time between Hudson Valley and Manhattan with his wife Dyan.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Wienerwaldsee. The Wienerwaldsee (English:&quot;Vienna Forest Lake&quot;) is a shallow reservoir, located 20 kilometres west of Vienna, Austria. It is located just north of Austria's main motorway, the West Autobahn, between Tullnerbach and Neu-Purkersdorf. It was created over three years, 1895–1897, by damming the Wienfluss (The Wien) and letting it fill the valley behind.

Geographic entities mentioned:
surface_form: wienerwaldsee
instance_of: Lake
countries: Austria
coordinates: lat: 48.1806
lon: 16.1203
The area around the lake is a nature conservation area. The area is a water protection zone where activities like swimming and ice skating are prohibited. Accordingly, the Wienerwaldsee has established itself as a habitat for a diverse range of flora and fauna. On the northern shore, near the weir, stands the statue of Wilhelm Kress.

Geographic entities mentioned:
surface_form: wienerwaldsee
instance_of: Lake
countries: Austria
coordinates: lat: 48.1806
lon: 16.1203
The northern boundary of the township follows the ridgecrest of Huntington Mountain, while Lee Mountain is south of it, running nearly parallel to it. The two ridges converge to form Knob Mountain, which is primarily west of the township. According to the United States Census Bureau, the township has a total area of, of which is land and, or 1.04%, is water. Demographics.

Geographic entities mentioned:
surface_form: Knob Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.7344
lon: -78.3447
Q'asiri (Aymara for bawler, also spelled &quot;Khasiri&quot;) is a mountain in the Cordillera Real in the Bolivian Andes. It lies in the La Paz Department, Murillo Province, at the border of the La Paz Municipality and the Palca Municipality. Q'asiri is situated south of the mountains Sirk'i Qullu and Jathi Qullu, north-west of the mountain Sura Qullu and north-east of the mountain Ch'iyar Qullu.

Geographic entities mentioned:
surface_form: Sirk'i Qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.383333333333
lon: -67.866666666667
surface_form: Jathi Qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4317
lon: -67.9414
surface_form: Sura Qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4503
lon: -67.9044
surface_form: sirk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9658
lon: -66.6606
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.9
lon: -68.5
surface_form: sirk'i qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.383333333333
lon: -67.866666666667
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.8583
lon: -68.5819
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4636
lon: -67.9556
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6144
lon: -67.81
surface_form: sirk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.9375
lon: -66.4533
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.43333333
lon: -67.38333333
surface_form: sirk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.35
lon: -69.4
surface_form: jathi qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4317
lon: -67.9414
surface_form: sirk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.65
lon: -66.45
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4444
lon: -67.9375
surface_form: sura qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4503
lon: -67.9044
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.5044
lon: -67.975
surface_form: ch'iyar qullu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.2556
lon: -68.2831
Q'asiri (Murillo). Q'asiri (Aymara for bawler, also spelled &quot;Khasiri&quot;) is a mountain in the Cordillera Real in the Bolivian Andes. It lies in the La Paz Department, Murillo Province, at the border of the La Paz Municipality and the Palca Municipality.

Geographic entities mentioned:
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.9
lon: -68.5
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4444
lon: -67.9375
Q'asiri is situated south of the mountains Sirk'i Qullu and Jathi Qullu, north-west of the mountain Sura Qullu and north-east of the mountain Ch'iyar Qullu. Q'asiri lies between the lakes Q'asiri Quta (&quot;Q'asiri lake&quot;, &quot;Khasiri Kkota&quot;) in the north-east and Jach'a Q'asiri Quta (&quot;big Q'asiri lake&quot;, &quot;Laguna Jachcha Khasiri&quot;) in the south-west.

Geographic entities mentioned:
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.9
lon: -68.5
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.9
lon: -68.5
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.9
lon: -68.5
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.9
lon: -68.5
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4444
lon: -67.9375
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4444
lon: -67.9375
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4444
lon: -67.9375
surface_form: q'asiri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.4444
lon: -67.9375
Subduction of the Nazca Plate beneath the South American Plate is responsible for most of the volcanism in the CVZ. After activity in the volcanic arc of the western Maricunga Belt ceased six million years ago, volcanism commenced in the Incapillo region, forming the high volcanic edifices Monte Pissis, Cerro Bonete Chico and Sierra de Veladero.

Geographic entities mentioned:
surface_form: Monte Pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: Cerro Bonete Chico
instance_of: Mountain
countries: Argentina
coordinates: lat: -28.01861111111111
lon: -68.75611111111111
surface_form: Sierra de Veladero
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.916666666667
lon: -68.916666666667
Incapillo is part of the Andean Central Volcanic Zone (CVZ), which extends through the countries of Chile, Bolivia, and Argentina and includes six or more Quaternary caldera or ignimbrite systems, about 44 stratovolcanoes, and over 18 smaller centres. One of these stratovolcanoes, Ojos del Salado, is the world's highest volcano.

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
One of these stratovolcanoes, Ojos del Salado, is the world's highest volcano. This zone also includes the Altiplano–Puna volcanic complex and the Galán caldera south of it.

Geographic entities mentioned:
surface_form: Galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
This zone also includes the Altiplano–Puna volcanic complex and the Galán caldera south of it. Incapillo is the southernmost volcano of the CVZ that erupted during the Pleistocene; the next volcano to the south to have erupted during the Pleistocene epoch is Tupungato in the Southern Volcanic Zone at 33° southern latitude. Incapillo is a caldera with a diameter of and lies at an elevation of or.

Geographic entities mentioned:
surface_form: Tupungato
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -33.358555555555554
lon: -69.77041666666666
Phases of ignimbritic and stratovolcanic activity occurred, including Copiapo volcano, until activity ceased with the last eruption of Nevado de Jotabeche 6million years ago. South of Incapillo, the Pampean flat slab region is associated with tectonic deformation and lack of volcanic activity until Tupungatito volcano farther south. S. L. de Silva and P.

Geographic entities mentioned:
surface_form: Tupungatito
instance_of: Mountain
countries: Chile
coordinates: lat: -33.423888888889
lon: -69.798055555556
This magmatic inactivity occurs because the flat slab removes the asthenospheric wedge. Incapillo is part of a volcanic system active between 3.5 and 2million years ago that includes Ojos del Salado and Nevado Tres Cruces. It was the last volcanic centre formed in the region; one view is that subsequently, the shallowing of the subducting slab prevented volcanism east and south of it.

Geographic entities mentioned:
surface_form: Nevado Tres Cruces
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.098055555556
lon: -68.778055555556
Rammelsberg. The Rammelsberg () is a mountain, high, on the northern edge of the Harz range, south of the historic town of Goslar in the North German state of Lower Saxony. The mountain is the location of an important silver, copper, and lead mine. When it closed in 1988, it had been the only mine still working continuously for over 1,000 years.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
The mountain is the location of an important silver, copper, and lead mine. When it closed in 1988, it had been the only mine still working continuously for over 1,000 years. Because of its long history of mining and testimony to the advancement and exchange of technology over many centuries, the visitor mine of Rammelsberg was inscribed as a UNESCO World Heritage Site in 1992. Name.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
In Italian today &quot;rame&quot; means &quot;copper&quot;. Ore formation. Unlike the mineral deposits of the Upper Harz, the ore deposits at the Rammelsberg were caused by the escape of hot, metal-bearing, thermal springs on the sea floor in the Devonian period. This formation is referred to as a sedimentary exhalative deposit.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
Initially the main product was copper ore, then, (much) later lead, and with lead, silver. The analysis of written sources and archaeological finds of unsmelted pieces of ore and slag found during archaeological excavations between 1981 and 1985 at Düna (near Osterode) in the South Harz indicates that the earliest mining activity at the Rammelsberg occurred in the late 7th century AD.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
The mining settlement of Goslar was not mentioned until 979. In 1005, attracted by the presence of silver, King Henry II of Germany had the Imperial Palace of Goslar (&quot;Kaiserpfalz Goslar&quot;) built at the foot of Mt. Rammelsberg, and held his first Imperial Assembly there in 1009.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
The main ores mined at Rammelsberg were lead-zinc ore, copper ore, sulphur ore, mixed ore (&quot;Melierterz&quot;), brown spar (&quot;Braunerz&quot;), barite ore (&quot;Grauerz&quot;), banding ore (&quot;Banderz&quot;) and kniest along with the important minerals of galena, chalcopyrite, sphalerite, baryte and vitriols.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
During the Thirty Years' War the Goslar citizens once again tried to regain the Rammelsberg mines distinguishing themselves as loyal supporters of the Imperial forces against the Protestant commander Christian the Younger of Brunswick; however, to no avail as his nephew Duke Augustus the Younger reconciled with Emperor Ferdinand in 1642.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
Under the Welf dukes, gold was also won from the 18th century onwards. With Goslar the Rammelsberg mines passed to the Kingdom of Hanover in 1814 and to the Kingdom of Prussia in 1866. Under the 1936/37 &quot;Rammelsbergprojekt&quot;, the mine was greatly expanded at the behest of the Nazi authorities as part of the Four-year plan.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
Under the 1936/37 &quot;Rammelsbergprojekt&quot;, the mine was greatly expanded at the behest of the Nazi authorities as part of the Four-year plan. The Nazis saw the Rammelsberg with its metal ores as vital to their war efforts and the difficulty of mineral dressing the ore had been technically solved (using froth flotation).

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
Prospecting in 2009. In February 2009, the company, Scandinavian Highlands Holding A/S, published the results of geophysical investigations by its subsidiary, Harz Minerals GmbH, according to which hitherto unknown mineral deposits of the size of those at the Rammelsberg may be present, two kilometres west of the Rammelsberg ore deposits.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
World Heritage Site. In 1992 the museum became a UNESCO World Heritage project together with Goslar's Old Town. In 2010 this World Heritage Site was expanded to include the Upper Harz Water Regale, Walkenried Abbey and the historic Samson Pit. The Rammelsberg Museum and Visitor Mine is an anchor point on the European Route of Industrial Heritage (ERIH). Master Malter's Tower.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
The Rammelsberg Museum and Visitor Mine is an anchor point on the European Route of Industrial Heritage (ERIH). Master Malter's Tower. The Master Malter's Tower (&quot;Maltermeisterturm&quot;) is the oldest surviving above-ground mine building on the Rammelsberg and, probably, in Germany as well. It was built around 1500 on a slagheap on the side of the Rammelsberg.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
Once again the mine architect, Fritz Schupp, was responsible for planning the facilities. The site was linked to the Rammelsberg mine via the pit railway through the Gelenbeek Gallery. The removal of concentrates to the lead smelter at Oker and the Harlingerode zinc works was facilitated by a standard gauge railway line. Commemorative coin.

Geographic entities mentioned:
surface_form: rammelsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.8875
lon: 10.431666944444444
Holmes Ridge. l2ojuxzss25tqyudj5imr734xcj0" xml:space="preserve">Holmes Ridge () is a rock ridge, long, which is the largest feature in the western part of the Finger Ridges in the Cook Mountains of Antarctica. It was named after Robert E.

Geographic entities mentioned:
surface_form: cook
instance_of: Mountain
coordinates: lat: -67.91667
lon: 56.46667
surface_form: holmes
instance_of: Mountain
coordinates: lat: -66.78333333
lon: -64.26666667
surface_form: holmes ridge
instance_of: Mountain
coordinates: lat: -79.16666667
lon: 156.7
Holmes Ridge. l2ojuxzss25tqyudj5imr734xcj0" xml:space="preserve">Holmes Ridge () is a rock ridge, long, which is the largest feature in the western part of the Finger Ridges in the Cook Mountains of Antarctica. It was named after Robert E.

Geographic entities mentioned:
surface_form: holmes
instance_of: Mountain
coordinates: lat: -66.78333333
lon: -64.26666667
surface_form: holmes ridge
instance_of: Mountain
coordinates: lat: -79.16666667
lon: 156.7
It was named after Robert E. Holmes of the Space Science and Engineering Center, University of Wisconsin–Madison, who was involved with the siting and operation of automatic weather station units throughout Antarctica, 1991–97.

Geographic entities mentioned:
surface_form: holmes
instance_of: Mountain
coordinates: lat: -66.78333333
lon: -64.26666667
The Park lies within the Polish Jura formation also known as the Polish Jurassic Highland or Kraków-Częstochowa Upland (), stretching between the cities of Kraków, Częstochowa and Wieluń. The Polish Jura, along with its numerous medieval castles () built by King Casimir (1310–1370), is visited by roughly 400,000 visitors a year.

Geographic entities mentioned:
surface_form: Kraków-Częstochowa Upland
instance_of: Plateau
countries: Poland
coordinates: lat: 50.2067
lon: 19.8292
In recent years, the population has greatly increased due to an influx of immigrants, from Western Sahara, Colombia, Cuba, and other African and Latin American countries. The municipality extends from the altitudinous center of the island -Mount Guajara (2,718 m, the third-highest mountain on the island, after Teide and Pico Viejo) is situated in this municipality- to the Atlantic Ocean.

Geographic entities mentioned:
surface_form: Mount Guajara
instance_of: Mountain
countries: Spain
coordinates: lat: 28.21694444
lon: -16.61166667
surface_form: Pico Viejo
instance_of: Mountain
countries: Spain
coordinates: lat: 28.263888888889
lon: -16.664722222222
Ernesto Schiaparelli. Ernesto Schiaparelli (; 12 July 1856 &ndash; 14 February 1928) was an Italian Egyptologist. Biography. Schiaparelli was born on 12 July 1856, in Biella. He found Queen Nefertari's tomb in Deir el-Medina in the Valley of the Queens (1904) and excavated the TT8 tomb of the royal architect Kha (1906), found intact and displayed &quot;in toto&quot; in Turin.

Geographic entities mentioned:
surface_form: Valley of the Queens
instance_of: Valley
countries: Egypt
coordinates: lat: 25.7275
lon: 32.593055555556
Mitchell's Bay, Ontario. Mitchell's Bay is a community in the regional municipality of Chatham-Kent, Ontario, located on the eastern shore of Lake St. Clair.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
Geography. Kaisermühlen is a quasi-island, connected to the mainland by only two narrow strips of land. It is bordered by the Old Danube to the east and the New Danube to the west. The area includes the Donaupark, Donau City, part of the Donauinsel, and the Gänsehäufel Island. To the north, Kaisermühlen borders the district of Floridsdorf, while the Reichsbrücke links it to Leopoldstadt.

Geographic entities mentioned:
surface_form: Old Danube
instance_of: Lake
countries: Austria
coordinates: lat: 48.2321
lon: 16.4278
Area. The province was much smaller than the present-day Southland region. The area was bounded by the Mataura River (east), the Waiau River (west), and a line from Eyre Peak to Lake Manapouri (north). Stewart Island was purchased by the Crown in 1863 and added to the area. The capital and largest settlement of Southland Province was Invercargill. Railways.

Geographic entities mentioned:
surface_form: Lake Manapouri
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.514
lon: 167.508
Le Cren sold his business interests in Timaru to Miles and Company in 1866 but he remained manager for a while. He held sheep stations at Simon's Pass near Lake Pukaki, Peel Forest, and Otaio. In 1873 or 1874 he sold his homestead and moved his family to London having before 1873 established a new business there, Russell Le Cren and Co, in partnership with Dunedin's George Gray Russell.

Geographic entities mentioned:
surface_form: Lake Pukaki
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.116666666667
lon: 170.16666666667
Lohara dynasty. The Lohara dynasty was a dynasty that ruled over Kashmir and surrounding regions in the northwestern part of the Indian subcontinent between 1003 CE and approximately 1320 CE.

Geographic entities mentioned:
surface_form: Kashmir
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Sammanthurai. Sammanthurai (;,), is a town in Ampara District of Eastern Province of Sri Lanka. Sammanthurai situated at, is 4.8 km west of the Bay of Bengal coast. It lies between the towns of Ampara and Karaitivu along the A31 road. It is surrounded by paddy fields and it is renowned for its rice paddies and its inner harbour from ancient times. Sammanthurai is the birthplace of M. H. M.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Access to the base of the peak is generally from Geeveston via Farmhouse Creek and Moss Ridge or Scotts Peak via the Eastern Arthurs. The first route is the shorter of two - generally three days to the peak. The Eastern Arthurs via Scotts Peak Dam takes at least 7 days finishing at Farmhouse Creek; up to 10 days with bad weather. Winter ascents.

Geographic entities mentioned:
surface_form: Scotts Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.004
lon: 146.279
Federation Peak. Federation Peak is a Tasmanian mountain with a sharp spire-like shape, which marks the southern end of the Eastern Arthur Range in the Southwest National Park. The peak, approximately south-west from Hobart, was named after the Federation of Australia.

Geographic entities mentioned:
surface_form: federation peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.271388888889
lon: 146.47555555556
The first westerner to sight the peak was the surveyor James Sprent who was carrying out a trigonometrical survey of Tasmania. He described it as &quot;the Obelisk&quot;. It became known as Sprent's Obelisk, however in 1901 it was officially named Federation Peak in honour of the Federation of Australia by Thomas Bather Moore while cutting a track from Hastings to Port Davey via Old River.

Geographic entities mentioned:
surface_form: federation peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.271388888889
lon: 146.47555555556
Blade Ridge was first successfully used as a route up Federation Peak in February 1968, by Peter Heddles, Rod Harris, David Neilson and Jack Woods
Most bushwalkers with minimal or no climbing gear take the exposed 'Direct Ascent' scramble from the Southern Traverse of the peak above a drop of into Lake Geeves (approximately Australian climbing grade 5).

Geographic entities mentioned:
surface_form: federation peak
instance_of: Mountain
countries: Australia
coordinates: lat: -43.271388888889
lon: 146.47555555556
The mining town of Tungsten, site of the Cantung Mine, is in the Mackenzie Mountains. Only two roads lead into the Mackenzie Mountains, both in Yukon: the Nahanni Range Road leading to the townsite of Tungsten and the Canol Road leading to the Macmillan Pass. The highest mountain in this range is Keele Peak at, in Yukon. The second-highest mountain is Mount Nirvana.

Geographic entities mentioned:
surface_form: Keele Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 63.431388888889
lon: -130.32388888889
Only two roads lead into the Mackenzie Mountains, both in Yukon: the Nahanni Range Road leading to the townsite of Tungsten and the Canol Road leading to the Macmillan Pass. The highest mountain in this range is Keele Peak at, in Yukon. The second-highest mountain is Mount Nirvana. It is, at, the highest mountain in the Northwest Territories.

Geographic entities mentioned:
surface_form: Mount Nirvana
instance_of: Mountain
countries: Canada
coordinates: lat: 61.8747
lon: -127.68
The earthquake resulted in &quot;many fatalities&quot;. Tectonic setting. Bhutan lies across the southern margin of the Himalayas. This mountain belt, and the Tibetan Plateau that lies north of it, is the result of the ongoing collision of the Indian Plate with the Eurasian Plate. The main active structures on the margin are a series of major thrust faults.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Intensities have been estimated from his descriptions at three locations, Wangdue Phodrang, the Punakha valley and the Thimphu valley. The Gangteng Monastery in Phobjikha Valley was also severely damaged. There are records of damage reported from northeastern India at three locations, Tingkhong, Charaideo and Garhgaon.

Geographic entities mentioned:
surface_form: Phobjikha Valley
instance_of: Valley
countries: Bhutan
coordinates: lat: 27.5
lon: 90.16666667
Mount Niobe. Mount Niobe is a summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated northwest of Squamish, and southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Lydia Mountain, to the west-northwest, and Omega Mountain lies to the east.

Geographic entities mentioned:
surface_form: Mount Tantalus
instance_of: Mountain
countries: Canada
coordinates: lat: 49.818111111111
lon: -123.32938888889
It is situated northwest of Squamish, and southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Lydia Mountain, to the west-northwest, and Omega Mountain lies to the east. Lake Lovely Water lies below the northern slope of the peak and precipitation runoff from the peak drains into tributaries of the Squamish River.

Geographic entities mentioned:
surface_form: Lydia Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.775277777777774
lon: -123.29333333333334
surface_form: Omega Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.771388888888886
lon: -123.24111111111111
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Niobe. Mount Niobe is a summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated northwest of Squamish, and southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Lydia Mountain, to the west-northwest, and Omega Mountain lies to the east.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount niobe
instance_of: Mountain
countries: Canada
coordinates: lat: 49.768
lon: -123.2661
Its nearest higher peak is Lydia Mountain, to the west-northwest, and Omega Mountain lies to the east. Lake Lovely Water lies below the northern slope of the peak and precipitation runoff from the peak drains into tributaries of the Squamish River. The first ascent of the mountain was made in 1910 by E. Kingsford-Smith and G. Warren via the south side.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The first ascent of the mountain was made in 1910 by E. Kingsford-Smith and G. Warren via the south side. The mountain's name was officially adopted on June 6, 1957, by the Geographical Names Board of Canada. The mountain was named for Niobe, daughter of Tantalus in Greek mythology, with several peaks in the Tantalus Range being named for family members of Tantalus. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Niobe. Mount Niobe is a summit located in the Tantalus Range, in Tantalus Provincial Park, in southwestern British Columbia, Canada. It is situated northwest of Squamish, and southeast of Mount Tantalus, which is the highest peak in the Tantalus Range. Its nearest higher peak is Lydia Mountain, to the west-northwest, and Omega Mountain lies to the east.

Geographic entities mentioned:
surface_form: mount niobe
instance_of: Mountain
countries: Canada
coordinates: lat: 49.768
lon: -123.2661
Climate. Based on the Köppen climate classification, Mount Niobe is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mount niobe
instance_of: Mountain
countries: Canada
coordinates: lat: 49.768
lon: -123.2661
Mertz competed in several national competitions; in 1906 he was third in the Swiss cross-country skiing championship, and second in the German championship. In 1908, he won the Swiss ski jumping championship, with a distance of. As a mountaineer, he was particularly prolific in the Alps; he climbed Mont Blanc—the highest peak in the range—and claimed several first ascents of other mountains.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Location and features. Lake Canobolas, formerly known as Meadow Creek Dam across the Molong Creek, is located approximately to the southwest of Orange, below Mount Canobolas, an extinct volcano and one of the highest peaks between the Blue Mountains and Perth. Between 1918 and 1957, the dam was managed by Canobolas Shire Council and used for water supply to the town of Orange.

Geographic entities mentioned:
surface_form: Mount Canobolas
instance_of: Mountain
countries: Australia
coordinates: lat: -33.3442
lon: 148.982
surface_form: lake canobolas
instance_of: Lake
countries: Australia
coordinates: lat: -33.304722222222
lon: 149.02777777778
Lake Canobolas. Lake Canobolas is a man-made reservoir located near Orange, in the central west region of New South Wales, Australia. Completed in the early 1900s, between 1918 and 1957 the lake supplied water to Orange and since the 1970s has been used for recreation purposes. Location and features.

Geographic entities mentioned:
surface_form: lake canobolas
instance_of: Lake
countries: Australia
coordinates: lat: -33.304722222222
lon: 149.02777777778
Between 1918 and 1957, the dam was managed by Canobolas Shire Council and used for water supply to the town of Orange. Since that time the administration of the area surrounding Lake Canobolas and the dam were taken over by the Orange City Council and were developed for recreational purposes.

Geographic entities mentioned:
surface_form: lake canobolas
instance_of: Lake
countries: Australia
coordinates: lat: -33.304722222222
lon: 149.02777777778
Mount Hilgard. Mount Hilgard is a mountain summit located west of the crest of the Sierra Nevada mountain range in Fresno County of northern California, United States. It is situated in the John Muir Wilderness on land managed by Sierra National Forest, approximately eight miles east-southeast of Lake Thomas A Edison, and immediately above the west end of Lake Italy.

Geographic entities mentioned:
surface_form: Lake Italy
instance_of: Lake
countries: United States
coordinates: lat: 37.358055555556
lon: -118.80638888889
It is situated in the John Muir Wilderness on land managed by Sierra National Forest, approximately eight miles east-southeast of Lake Thomas A Edison, and immediately above the west end of Lake Italy. The nearest higher neighbor is Mount Gabb, to the northeast, and Recess Peak is to the northwest. The John Muir Trail follows Bear Creek to the west of this remote peak, providing an approach. Mt.

Geographic entities mentioned:
surface_form: Mount Gabb
instance_of: Mountain
countries: United States
coordinates: lat: 37.37666667
lon: -118.8025
surface_form: Recess Peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.382777777778
lon: -118.85472222222
The nearest higher neighbor is Mount Gabb, to the northeast, and Recess Peak is to the northwest. The John Muir Trail follows Bear Creek to the west of this remote peak, providing an approach. Mt. Hilgard ranks as the 82nd highest summit in California. History. This mountain was named by Sierra Club explorer Theodore Solomons for Eugene W.

Geographic entities mentioned:
surface_form: mt. hilgard
instance_of: Mountain
countries: United States
coordinates: lat: 37.360277777778
lon: -118.82722222222
Mount Hilgard. Mount Hilgard is a mountain summit located west of the crest of the Sierra Nevada mountain range in Fresno County of northern California, United States. It is situated in the John Muir Wilderness on land managed by Sierra National Forest, approximately eight miles east-southeast of Lake Thomas A Edison, and immediately above the west end of Lake Italy.

Geographic entities mentioned:
surface_form: mount hilgard
instance_of: Mountain
countries: United States
coordinates: lat: 37.360277777778
lon: -118.82722222222