Sarmila/GeoWiki-Features huggingface dataset:
On 24 February 1310 (&quot;Sexta Kal. Martii.&quot;) Graf Rudolf transferred &quot;to his parents, his late wife Elisabeth and his own salvation's sake&quot;, the patronage of the church in Dietikon with the presentation right in the chapels of Urdorf and Spreitenbach to the Wettingen Abbey in the Limmat Valley. On 23 March 1310 (&quot;X. Kal. April. Ind.

Geographic entities mentioned:
surface_form: Limmat Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.5
lon: 8.25
Life. Zerahiah went to Rome about 1277, and wrote all his works there before 1290. In writing to the physician Hillel of Verona, he makes the point that while commenting upon the difficult passages of the &quot;Moreh&quot;, he followed the criticisms of Naḥmanides. It may be inferred from his commentary to the Book of Job that Arabic was his native language. Works.

Geographic entities mentioned:
surface_form: Moreh
instance_of: Mountain
countries: Israel
coordinates: lat: 32.615833333333
lon: 35.363611111111
It covers most of the Giant Mountains (), which is the highest range of the country. The park has also been listed as a UNESCO Biosphere Reserve site. It borders Karkonosze National Park in Poland. Krkonoše's highest mountain is Sněžka at, which is also the highest mountain of the entire Czech Republic. The area of the national park is. The protection zone of the park covers.

Geographic entities mentioned:
surface_form: Sněžka
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.736111111111
lon: 15.740277777778
Krkonoše National Park lies primarily within the Giant Mountains, part of the Sudetes mountain system. The park's highest point, Sněžka (1,603 metres above sea level), is also the highest peak in the Czech Republic. The effects of the last glaciation are evident throughout the park, with features such as cirques, glacial valleys, moraines, tors, stone seas, and other glacial relics.

Geographic entities mentioned:
surface_form: Sněžka
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.736111111111
lon: 15.740277777778
The geological subsoil of the Krkonoše national park is highly diverse. Most of the area falls within the so-called Krkonoše-Jizera crystalline complex, a significant part of which—the Krkonoše-Jizera pluton, composed primarily of granitoids—extends into the national park. This formation shapes the main ridge, stretching from Mrtvý vrch (1,060 m) to the western foothills of Sněžka (1,603 m).

Geographic entities mentioned:
surface_form: Sněžka
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.736111111111
lon: 15.740277777778
Tourism. The Giant Mountains are the highest and most visited Czech mountains. Traditional excursion destinations include Sněžka, the source of the Elbe, the Pančava, Elbe and Mumlava waterfalls, the nature trail through the Černohorské rašeliniště peat bog, the Obří důl valley, the ancient forest of Dvorský les and the mountain hut Luční bouda.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
surface_form: Dvorský les
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.6489
lon: 15.8636
and North Korea; however, Kim Jong Un asked Moon to support a common goal to unite North and South Korea instead of supporting the United States. In previous talks, both leaders agreed to reconnect the railways and roads that run through both their countries, normalize a factory park in the Kaesong Industrial Zone, and allow South Korean tourists to visit the Mount Kumgang resort again.

Geographic entities mentioned:
surface_form: Mount Kumgang
instance_of: Mountain
countries: North Korea
coordinates: lat: 38.656763888889
lon: 128.10490277778
The projects funded by their program, the Shelby White-Leon Levy Program for Archaeological Publications, include excavations at some of the highest profile archaeological sites throughout Greece and the Middle East, including Knossos, Aphrodisias, Kition, Ras Shamra, Sarepta, Mount Gerizim, Ekron, Lachish, Megiddo, Jerusalem, Pella, Jerash, the Dead Sea Scrolls, Assur, Nineveh, Nuzi, and Tepe Hissar.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
Achacollo (Peru). Achacollo (possibly from Aymara Jach'a Qullu, &quot;jach'a&quot; big, great, &quot;qullu&quot; mountain, &quot;big mountain&quot;) is a mountain in the Barroso mountain range in the Andes of Peru, about high. It is situated in the Tacna Region, Tacna Province, Palca District, and in the Tarata Province, Estique District, northwest of the Chupiquiña volcano and Huancune.

Geographic entities mentioned:
surface_form: barroso
instance_of: Mountain
countries: Peru
coordinates: lat: -17.556308
lon: -69.5954717
surface_form: achacollo
instance_of: Mountain
countries: Peru
coordinates: lat: -17.5633
lon: -69.8708
Achacollo (Peru). Achacollo (possibly from Aymara Jach'a Qullu, &quot;jach'a&quot; big, great, &quot;qullu&quot; mountain, &quot;big mountain&quot;) is a mountain in the Barroso mountain range in the Andes of Peru, about high. It is situated in the Tacna Region, Tacna Province, Palca District, and in the Tarata Province, Estique District, northwest of the Chupiquiña volcano and Huancune.

Geographic entities mentioned:
surface_form: huancune
instance_of: Mountain
countries: Peru
coordinates: lat: -17.5952
lon: -69.7893
Achacollo (Peru). Achacollo (possibly from Aymara Jach'a Qullu, &quot;jach'a&quot; big, great, &quot;qullu&quot; mountain, &quot;big mountain&quot;) is a mountain in the Barroso mountain range in the Andes of Peru, about high. It is situated in the Tacna Region, Tacna Province, Palca District, and in the Tarata Province, Estique District, northwest of the Chupiquiña volcano and Huancune.

Geographic entities mentioned:
surface_form: achacollo (peru)
instance_of: Mountain
countries: Peru
coordinates: lat: -17.5633
lon: -69.8708
Gantrisch. The Gantrisch is a mountain in the north-western Bernese Alps, located between the Simmental and the Aar valley in the canton of Bern. The mountain lies near Gurnigel Pass, from where it is usually climbed. A trail leads to the summit.

Geographic entities mentioned:
surface_form: Simmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.55
lon: 7.36
surface_form: gantrisch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.705166666667
lon: 7.4505
Gantrisch. The Gantrisch is a mountain in the north-western Bernese Alps, located between the Simmental and the Aar valley in the canton of Bern. The mountain lies near Gurnigel Pass, from where it is usually climbed. A trail leads to the summit.

Geographic entities mentioned:
surface_form: Gurnigel Pass
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7334
lon: 7.45277
Gantrisch. The Gantrisch is a mountain in the north-western Bernese Alps, located between the Simmental and the Aar valley in the canton of Bern. The mountain lies near Gurnigel Pass, from where it is usually climbed. A trail leads to the summit.

Geographic entities mentioned:
surface_form: gantrisch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.705166666667
lon: 7.4505
Longtime WDIO news anchor Dennis Anderson joined the station in 1969, initially as anchor of the nightly news' &quot;Action Line&quot; segment. He was promoted to chief anchor of the evening newscasts in 1970; he later was the first local TV anchor to announce the sinking of the ore freighter Edmund Fitzgerald which sank in Lake Superior on November 10, 1975.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Pronotum posseses basolateral seti. This species is known from the Kohala Mts. and windward forests on Mauna Loa. If this species’ distribution is congruent with other occupants of the windward wet forests, populations on Mauna Kea are predicted. This species to tell apart from Mecyclothorax konanus without dissection, as there is much overlap in size, color and external traits.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
Embu people. The Embu or Aembu (sometimes called Waembu) are a Bantu ethnic group indigenous to Embu county. The region is situated on the southern slopes of Mount Kenya in the former Eastern province. To the West, Embu neighbours the Kikuyu, The Meru people border the Embu to the North and the Kamba border the Embu to the East and South. Origin. The Embu are of Bantu origin.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
To the West, Embu neighbours the Kikuyu, The Meru people border the Embu to the North and the Kamba border the Embu to the East and South. Origin. The Embu are of Bantu origin. They are also known as the 'Aembu'. They are closely related in language and culture to the Kikuyu, Meru, and Kamba. They inhabit the southern windward slopes and farmlands of Mount Kenya.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
One chartered Public university, The University of Embu was the first to be established in Embu region. Economy. Embu lies on the windward slopes of Mount Kenya. It remarkably occupies the most prime fertile lands of the Kenya highlands. Two seasons are enjoyed each year, and the weather is favourable for diverse agricultural activities.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Battle. Pedro Fajardo de Zúñiga and Requesens, Marquis de los Vélez sent a large contingent of troops on 20 January by Gelida and Castellví de Rosanes, in order to cut the possible retreat of the Catalan troops by the right bank of the Llobregat. But these troops were repulsed by the miquelets commanded by Dídac de Vergós.

Geographic entities mentioned:
surface_form: Llobregat
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.282412
lon: 2.012826
However, as names are applied on a larger scale, they may become less useful as place names. For instance, a relatively small, distinct upland valley (e.g. Swaledale) clearly represents a definable geographic location. However, the broad, extended valley of a major river, such as the Trent, is not easily understood as a single location.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
In Shropshire and Herefordshire many Welsh place names are found in the borderlands such as Pontrilas and Trefonen. In Cornwall most place-names are Cornish in origin, whilst in Cumbria there remain a number of place names in Cumbric, the Brythonic language of this region; examples including Carlisle, Helvellyn and Blencathra.

Geographic entities mentioned:
surface_form: Helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: Blencathra
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.63985
lon: -3.0504611111111
One place in Yorkshire which retains Celtic toponymy is Pen-y-ghent (one of the Yorkshire Three Peaks), whose name means Hill-by-the-Border in Cumbric, a Brittonic language. Wales. The vast majority of place names in Wales are Welsh by origin, containing elements such as Llan-, Aber-, Pen- etc.

Geographic entities mentioned:
surface_form: Pen-y-ghent
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.155277777778
lon: -2.2497222222222
Death Valley Suite. The &quot;Death Valley Suite&quot; is a short symphonic suite written by American composer Ferde Grofé in 1949, depicting the westward travels of pioneers through the 'harsh lands' of Death Valley in California.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Later that month it defended the southern approaches to Leningrad in the Kolpino direction. The 70th fought in fierce defense battles in the area of Kolpino, Pushkin, Pulkovo, Krasny Bor, and Ust-Tosno, among others, between September and April 1942 as part of the 55th Army of the Leningrad Front during the siege of Leningrad.

Geographic entities mentioned:
surface_form: Pulkovo
instance_of: Landform
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.771811
lon: 30.326047
Sekizan Myōjin is primarily considered a god of destiny, and in this capacity can be identified as a representation of the so-called &quot;auxiliary star” of the Northern Dipper, Hosei (Alcor). He can also function as a protective god of Mount Hiei or as a deity associated with pestilence. In art he is depicted as an old man resembling the Ten Kings of Hell, sometimes armed with a bow and arrow.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Sekizan Myōjin is also considered a &quot;gohōjin&quot;, a deity regarded as the protector of dharma. He can be considered a protective deity of Mount Hiei and of the Sanmon lineage of Tendai. A further role which can be assigned to him is that of a deity of pestilence.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Descriptions of Sekizan Myōjin as a figure clad in armor are also known. On ema (絵馬; votive tablets), he can be accompanied by a monkey holding a &quot;gohei&quot;, an animal symbol of Mount Hiei, regarded as a messenger of Sannō. The oldest surviving depictions of Sekizan Myōjin only date back to the Edo period. One example is known from the Ichigami Shrine.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Worship. Sekizan Myōjin is worshiped in the Tendai school of Japanese Buddhism. His temple is known as (赤山禅院). It is located on the western foot of Mount Hiei, to the northeast of Kyoto. The location was selected based on the fact that the eastern side already was the site of a shrine dedicated to the deity Sannō (山王).

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Alanqa. &quot;Alanqa&quot; is a genus of azhdarchoid pterodactyloid pterosaur from the Late Cretaceous period (Cenomanian stage) of what is now the Kem Kem Group of southeastern Morocco. The name &quot;Alanqa&quot; comes from the Arabic word العنقاء &quot;al-‘Anqā’&quot;, for a mythical bird of Arabian culture. Discovery.

Geographic entities mentioned:
surface_form: Kem Kem Group
instance_of: Mountain
countries: Morocco
coordinates: lat: 30.9
lon: -4
The former was recovered as an azhdarchid, while &quot;Alanqa&quot; was recovered as a basal azhdarchoid related to &quot;Keresdrakon&quot;, both forming the new clade Alanqidae. Paleoecology. &quot;Alanqa&quot; was recovered from the Kem Kem Group of the late Cenomanian period, then a freshwater delta system.

Geographic entities mentioned:
surface_form: Kem Kem Group
instance_of: Mountain
countries: Morocco
coordinates: lat: 30.9
lon: -4
It is the municipal seat for the municipality of Tianguistenco. It is located in the southwest part of the Valley of Toluca at the edge of the Ajusco mountain range that separates it from Mexico City. The name Tianguistenco (Tyanguistengko) is from Nahuatl and means “at the edge of the tianguis,” which is a traditional Aztec market.

Geographic entities mentioned:
surface_form: Valley of Toluca
instance_of: Valley
countries: Mexico
coordinates: lat: 19.2865
lon: -99.5595
surface_form: Ajusco
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.2075
lon: -99.258055555556
In 1982, the museum's exhibits were redesigned. New exhibits highlighted the broader history of the towpath canal era and the industrial heritage of the Lehigh Valley. During this period, the National Canal Museum began hosting several major events, including the annual Canal Festival and annual Canal History and Technology Symposium, the latter being held at Lafayette College.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
The building holds a reception area, exhibit spaces, offices, and the Hugh Moore Park and Museums Archives. The building opened in 2007. The inaugural exhibit, &quot;From this Valley: Iron, Steel and the Birthplace of the American Industrial Revolution,&quot; tells the story of the Lehigh Valley's critical role in the Industrial Revolution.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
There are two cinder cones and a lava flow at least long which is present below parts of the tree covered area. The subdued form of Volcanic Creek cone is visible directly below the largest snow patch. The cone has probably suffered through at least one glacial episode. Volcanic Creek cone is part of the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
surface_form: volcanic creek cone
instance_of: Mountain
countries: Canada
coordinates: lat: 59.76
lon: -133.38
Volcanic Creek Cone. Volcanic Creek Cone is a small cinder cone northeast of Atlin in northwestern British Columbia. There are two cinder cones and a lava flow at least long which is present below parts of the tree covered area. The subdued form of Volcanic Creek cone is visible directly below the largest snow patch. The cone has probably suffered through at least one glacial episode.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: volcanic creek cone
instance_of: Mountain
countries: Canada
coordinates: lat: 59.76
lon: -133.38
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: atlin
instance_of: Lake
countries: Canada
coordinates: lat: 60.0133333
lon: -133.8308333
Volcanic Creek Cone. Volcanic Creek Cone is a small cinder cone northeast of Atlin in northwestern British Columbia. There are two cinder cones and a lava flow at least long which is present below parts of the tree covered area. The subdued form of Volcanic Creek cone is visible directly below the largest snow patch. The cone has probably suffered through at least one glacial episode.

Geographic entities mentioned:
surface_form: volcanic creek cone
instance_of: Mountain
countries: Canada
coordinates: lat: 59.76
lon: -133.38
It is located in the Cochabamba Department, Ayopaya Province, Morochata Municipality. It lies north of the lakes named Q'umir Qucha (&quot;green lake&quot;, &quot;Khomer Khocha&quot;), Yana Qucha (&quot;black lake&quot;, &quot;Yana Khocha&quot;), Parinani (&quot;the one with flamingos&quot;) and Wallatani (&quot;the one with Andean geese&quot;, &quot;Huallatani&quot;).

Geographic entities mentioned:
surface_form: wallatani
instance_of: Lake
countries: Bolivia
coordinates: lat: -17.008333333333333
lon: -67.34722222222223
surface_form: q'umir qucha
instance_of: Lake
countries: Bolivia
coordinates: lat: -19.788888888888888
lon: -65.65972222222223
Salla Willk'i Punta. Salla Willk'i Punta (Aymara &quot;salla&quot; rocks, cliffs, &quot;willk'i&quot; gap, also spelled &quot;Salla Willkhi Punta&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, Ayopaya Province, Morochata Municipality.

Geographic entities mentioned:
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: salla willk'i punta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.04888889
lon: -66.47972222
Salla Willk'i Punta. Salla Willk'i Punta (Aymara &quot;salla&quot; rocks, cliffs, &quot;willk'i&quot; gap, also spelled &quot;Salla Willkhi Punta&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, Ayopaya Province, Morochata Municipality.

Geographic entities mentioned:
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: willk'i
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.39861111
lon: -69.02222222
surface_form: salla willk'i punta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.04888889
lon: -66.47972222
As of the 2012 census of agriculture, there were over 35,000 farms covering an area of which contributed $5.4 billion in gross sales value and $1.2 billion in net farm income to the national economy. The Finger Lakes region is the center of state agriculture, and the state is a top-ten national producer of cow milk, apples, grapes, onions, sweet corn, tomatoes, and maple syrup.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
The border then follows this river south forming a broad S-shape. The river ends near Yardımlı, with the border then curving south-eastwards, proceeding overland in that direction through the Talysh Mountains, then turning east along the Astarachay river, following its course all the way to the Caspian Sea. History.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
It is situated on the western slopes of the Gran Sasso, at about 800 meters above sea level, along the state road 17-bis that from goes up to Campo Imperatore passing through Paganica, Tempera, Assergi and Fonte Cerreto, once an autonomous municipality before being aggregated to the capital and now seat of the ninth district of the municipality.

Geographic entities mentioned:
surface_form: Campo Imperatore
instance_of: Plateau
countries: Italy
coordinates: lat: 42.443698
lon: 13.558333
Construction of the initial route was completed in 1932. The western and eastern sections follow the rugged coastline, with views of the ocean. The southwestern section passes through the Margaree River valley before passing along Bras d'Or Lake. The route is within the county municipalities of Victoria and Inverness.

Geographic entities mentioned:
surface_form: Bras d'Or Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.860277777778
lon: -60.778888888889
Alongside the term &quot;Ćiribirci&quot;, in the narrow sense, it is an exonym referring to a community of the Istro-Romanians in the village Žejane in a small part of eastern Ćićarija and the villages around the former Lake Čepić west of the Učka range in Istria, Croatia. Etymology.

Geographic entities mentioned:
surface_form: Lake Čepić
instance_of: Body of water
countries: Croatia
coordinates: lat: 45.2089
lon: 14.16
Rainbow Peak. Rainbow Peak () is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. The namesake Rainbow Glacier is immediately east and northeast of Rainbow Peak. Rainbow Peak is the ninth-tallest mountain in Glacier National Park and rises over above Bowman Lake. From the parking lot at the Bowman Lake Campground, the elevation gain is.

Geographic entities mentioned:
surface_form: bowman lake
instance_of: Lake
countries: United States
coordinates: lat: 48.8667
lon: -114.164
surface_form: rainbow peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8792
lon: -114.097
Rainbow Peak is the ninth-tallest mountain in Glacier National Park and rises over above Bowman Lake. From the parking lot at the Bowman Lake Campground, the elevation gain is. In July 1998 the peak was the site of the death of two climbers who were climbing a snow-covered chimney when a cornice collapsed, causing the two climbers to fall to their deaths.

Geographic entities mentioned:
surface_form: bowman lake
instance_of: Lake
countries: United States
coordinates: lat: 48.8667
lon: -114.164
Rainbow Peak. Rainbow Peak () is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. The namesake Rainbow Glacier is immediately east and northeast of Rainbow Peak. Rainbow Peak is the ninth-tallest mountain in Glacier National Park and rises over above Bowman Lake. From the parking lot at the Bowman Lake Campground, the elevation gain is.

Geographic entities mentioned:
surface_form: rainbow peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.8792
lon: -114.097
Kanaka Creek Regional Park. Kanaka Creek Regional Park is a regional park of the Greater Vancouver Regional District, located in the city of Maple Ridge, British Columbia, flanking both sides of Kanaka Creek from its confluence with the Fraser River just east of Haney and extending approximately 11 km (7 mi) up the creek to just south of the community of Webster's Corners.

Geographic entities mentioned:
surface_form: Kanaka Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.2006
lon: -122.586
It flows from Linnie Lac to Little Muskego Lake, and is the primary tributary of Little Muskego Lake. Despite its relative proximity to Lake Michigan, Jewel Creek is part of the Mississippi River Watershed. Jewel Creek has a drainage area of 8.16 square miles. Between the years 2000 and 2003, its average flow rate was 6.52 cubic feet per second. Dams.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Zackenberg. Zackenberg or Zackenburg is a mountain in Wollaston Foreland, NE Greenland. Geography. This dark-hued mountain is located at the southern end of the western section of the Wollaston Foreland. Zackenberg rises steeply from the shore of the Zackenberg Bay on the northern side the Young Sound ().

Geographic entities mentioned:
surface_form: zackenberg
instance_of: Mountain
countries: Greenland
coordinates: lat: 74.49555556
lon: -20.76638889
Zackenberg. Zackenberg or Zackenburg is a mountain in Wollaston Foreland, NE Greenland. Geography. This dark-hued mountain is located at the southern end of the western section of the Wollaston Foreland. Zackenberg rises steeply from the shore of the Zackenberg Bay on the northern side the Young Sound ().

Geographic entities mentioned:
surface_form: zackenberg
instance_of: Mountain
countries: Greenland
coordinates: lat: 74.49555556
lon: -20.76638889
surface_form: zackenburg
instance_of: Mountain
countries: Greenland
coordinates: lat: 74.49555556
lon: -20.76638889
Geography. This dark-hued mountain is located at the southern end of the western section of the Wollaston Foreland. Zackenberg rises steeply from the shore of the Zackenberg Bay on the northern side the Young Sound (). It is a high massive mountain with a number of peaks, hence its German name 'Zackenberg', referring to its serrated top.

Geographic entities mentioned:
surface_form: zackenberg
instance_of: Mountain
countries: Greenland
coordinates: lat: 74.49555556
lon: -20.76638889
surface_form: zackenberg
instance_of: Mountain
countries: Greenland
coordinates: lat: 74.49555556
lon: -20.76638889
Zackenberg rises steeply from the shore of the Zackenberg Bay on the northern side the Young Sound (). It is a high massive mountain with a number of peaks, hence its German name 'Zackenberg', referring to its serrated top. A river flows on its northern and eastern side forming a valley between this mountain and the higher Dombjerg to the north.

Geographic entities mentioned:
surface_form: zackenberg
instance_of: Mountain
countries: Greenland
coordinates: lat: 74.49555556
lon: -20.76638889
It is a high massive mountain with a number of peaks, hence its German name 'Zackenberg', referring to its serrated top. A river flows on its northern and eastern side forming a valley between this mountain and the higher Dombjerg to the north. The Zackenberg Station, a research facility, is built at the foot of the mountain.

Geographic entities mentioned:
surface_form: zackenberg
instance_of: Mountain
countries: Greenland
coordinates: lat: 74.49555556
lon: -20.76638889
Ústí nad Labem District borders Germany in the north. The terrain is very varied—mostly hilly except in the west, and divided by the Elbe river valley. The territory extends into four geomorphological mesoregions: Central Bohemian Uplands (most of the territory), Most Basin (west), Ore Mountains (north) and Elbe Sandstone Mountains (a small part in the northeast with the Tisá Rocks).

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
From the total district area of, agricultural land occupies, forests occupy, and water area occupies. Forests cover 33.2% of the district's area. The most important river is the Elbe, which drains the entire territory. The Bílina flows into the Elbe in Ústí nad Labem. The largest body of water is Lake Milada, an extensive artificial lake created by flooding mine.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The most important river is the Elbe, which drains the entire territory. The Bílina flows into the Elbe in Ústí nad Labem. The largest body of water is Lake Milada, an extensive artificial lake created by flooding mine. There are two protected landscape areas: České středohoří that extends into the district in the south and east, and Labské pískovce that extends into the district in the northeast.

Geographic entities mentioned:
surface_form: Lake Milada
instance_of: Lake
countries: Czech Republic
coordinates: lat: 50.653611111111
lon: 13.944444444444
A shallow gap exists between Campgaw Mountain and the Preakness and Goffle Hill ranges of the Watchungs to the south, somewhat isolating the ridge from the rest of the Watchung Mountains despite contiguous geology below the surface. In the north, the mountain terminates at the Ramapo Fault, the western border of the Newark Basin.

Geographic entities mentioned:
surface_form: Goffle Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.9761
lon: -74.1689
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
The effect of this is that, when traveling north from the Preakness Range and Goffle Hill, the ridges of First and Second Watchung Mountain seem to slowly dip back into the Earth before reemerging again as Campgaw Mountain. Despite the apparent gap at the surface, Campgaw Mountain is firmly linked to the rest of the Watchungs by the continuity of the ridges through the anticline. Ecology.

Geographic entities mentioned:
surface_form: Goffle Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.9761
lon: -74.1689
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
surface_form: goffle hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.9761
lon: -74.1689
Today, chestnuts have been eliminated by the accidental importation of chestnut blight in the early twentieth century. Redcedar, however, is still abundant along the ridgeline, unlike on nearby Goffle Hill, where the tree has been all but extirpated, and in the Preakness Range, where redcedar has become rare. Recreation. There are two 18-hole disc golf courses at Campgaw.

Geographic entities mentioned:
surface_form: Goffle Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.9761
lon: -74.1689
surface_form: goffle hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.9761
lon: -74.1689
Campgaw Mountain. Campgaw Mountain is the northernmost ridge of the volcanically formed Watchung Mountains, along the border of Franklin Lakes, Oakland, and Mahwah in Bergen County, New Jersey, United States. Located almost entirely within the bounds of Campgaw Mountain Reservation, the mountain offers numerous outdoor recreational opportunities, including the only ski slope in the Watchungs.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
Campgaw Mountain is commonly considered to be part of the greater Ramapo Mountains region, but the flora and geology of the mountain is quite different from the surrounding area and more closely resembles the nearby Preakness Range to the south. Geography. Campgaw Mountain extends for three miles approximately north to south along the border of Franklin Lakes, Oakland, and Mahwah.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
Geography. Campgaw Mountain extends for three miles approximately north to south along the border of Franklin Lakes, Oakland, and Mahwah. The peak of the mountain rises to in Mahwah, becoming the fourth highest peak of Watchungs, though the height of the mountain as measured from its base is generally less than.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
In the north, the mountain terminates at the Ramapo Fault, the western border of the Newark Basin. Campgaw Mountain also marks the eastern edge of the Ramapo River Valley, forming a sizable basin between itself and the Ramapo Mountains. An unusual trait of Campgaw Mountain is that it is composed of the ridges of both First and Second Watchung Mountain.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
In the north, the mountain terminates at the Ramapo Fault, the western border of the Newark Basin. Campgaw Mountain also marks the eastern edge of the Ramapo River Valley, forming a sizable basin between itself and the Ramapo Mountains. An unusual trait of Campgaw Mountain is that it is composed of the ridges of both First and Second Watchung Mountain.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
An unusual trait of Campgaw Mountain is that it is composed of the ridges of both First and Second Watchung Mountain. Fyke Brook, a tributary of the Ramapo River, divides the two ridges, running northwest through a narrow valley along the northeastern corner of the mountain. Second Watchung Mountain comprises the majority of Campgaw Mountain at the surface. History.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
Second Watchung Mountain comprises the majority of Campgaw Mountain at the surface. History. Before the arrival of Europeans, Campgaw Mountain was inhabited by Munsee (Minsi) Lenape. Evidence of the Lenape presence around Campgaw can be found in a former village that existed on the north side of the mountain, along the south bank of the Ramapo River.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
Taken literally, the syllables in the name &quot;Kum-Kow&quot; probably translate to &quot;goose-hedgehog&quot;. A historical account from 1834 indicates that Campgaw Mountain's summits were once under extensive cultivation. That would seem to explain the numerous stone walls, apparently former property boundaries, running through the woods along the mountain.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
That would seem to explain the numerous stone walls, apparently former property boundaries, running through the woods along the mountain. Another historical work from 1894 detailing New Jersey's forests shows that Campgaw Mountain was covered by a nearly unbroken expanse of chestnut, oak, and redcedar, indicating that cultivation along the ridgeline may have declined by that time.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
Campgaw Mountain was essentially wilderness in 1960 when property on the ridge was taken by the Bergen County Park Commission to create Campgaw Mountain Reservation. The park, which opened in June 1961, forced many of the Ramapough Mountain Indians inhabiting Campgaw Mountain and the surrounding area off their land.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
The park, which opened in June 1961, forced many of the Ramapough Mountain Indians inhabiting Campgaw Mountain and the surrounding area off their land. In addition to the development of the park, Campgaw Mountain saw the construction of a Nike missile base during the height of the Cold War.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
At the time the mountain occupied the northern section of an active rift valley running through northern and central New Jersey and part of Pennsylvania. After the rift failed in the early Jurassic, the mountain was elevated as erosion removed the sandstone and shale surrounding the basalt lava flows of Campgaw Mountain.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
The combined ridges of First and Second Watchung Mountain make a slight turn to the west before terminating at the Ramapo Fault, marking the northernmost limit of the Watchung
Campgaw Mountain appears somewhat detached from the rest of the Watchungs because it occupies a local syncline (downfold) that is itself somewhat detached from the main Watchung syncline by an intervening anticline (upfold).

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
The effect of this is that, when traveling north from the Preakness Range and Goffle Hill, the ridges of First and Second Watchung Mountain seem to slowly dip back into the Earth before reemerging again as Campgaw Mountain. Despite the apparent gap at the surface, Campgaw Mountain is firmly linked to the rest of the Watchungs by the continuity of the ridges through the anticline. Ecology.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
Despite the apparent gap at the surface, Campgaw Mountain is firmly linked to the rest of the Watchungs by the continuity of the ridges through the anticline. Ecology. Campgaw Mountain, while adjacent to the Ramapo Mountains, features a unique ecosystem in relation to the surrounding area. In fact, according to the U.S.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
Ecology. Campgaw Mountain, while adjacent to the Ramapo Mountains, features a unique ecosystem in relation to the surrounding area. In fact, according to the U.S. EPA, Campgaw Mountain is in a level III and IV ecoregion that is completely different from the Ramapo Mountains.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
Features of this ecoregion include thin, well-drained soils and oak forests. Hemlock forests on northern facing slopes are also common to this ecoregion, and these are characteristically present along the northeastern slope of Campgaw Mountain. In addition to oak, chestnut and redcedar were historically prominent on Campgaw Mountain.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
Hemlock forests on northern facing slopes are also common to this ecoregion, and these are characteristically present along the northeastern slope of Campgaw Mountain. In addition to oak, chestnut and redcedar were historically prominent on Campgaw Mountain. Today, chestnuts have been eliminated by the accidental importation of chestnut blight in the early twentieth century.

Geographic entities mentioned:
surface_form: campgaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0543
lon: -74.1993
The highest waterfall on the River Eden, Hellgill Force, with a drop of about 9.75 metres (according to recent measurements) is just to the north, at. The river itself rises (at first as Red Gill beck, later becoming Hell Gill beck) below Hugh Seat in the peat bogs above here. It finally becomes the river Eden after merging with the Ais Gill beck, which flows down from Wild Boar Fell.

Geographic entities mentioned:
surface_form: Hugh Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3875
lon: -2.2939
The river itself rises (at first as Red Gill beck, later becoming Hell Gill beck) below Hugh Seat in the peat bogs above here. It finally becomes the river Eden after merging with the Ais Gill beck, which flows down from Wild Boar Fell. Aisgill is at both a county and a natural geographical boundary.

Geographic entities mentioned:
surface_form: Wild Boar Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.384111111111
lon: -2.3741194444444
Aisgill is at both a county and a natural geographical boundary. It is at the watershed (sometimes called &quot;the watershed of England&quot;) from which the Eden flows north towards the Irish Sea via the Solway Firth, while the River Ure flows south towards Wensleydale, and eventually into the North Sea.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
Upon this ancient denuded land surface the Torridonian strata rest horizontally or with gentle inclination. Some of the peaks, such as Beinn Eighe, are capped with white quartzite, giving them a distinctive appearance when seen from afar. Some of the quartzite contains fossilized worm burrows and is known as &quot;pipe rock&quot;. It is about 500 million years old.

Geographic entities mentioned:
surface_form: Beinn Eighe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.37
lon: -5.24
The route along the Northern Pinnacles is considered a rock climb, although another route to the top from Coire na Caime only involves a short steep scramble on the final 50m to gain the ridge. Irvine Butterfield considers Meall Dearg &quot;The most difficult top in the British Isles challenged only by the Inaccessible Pinnacle of Sgùrr Dearg&quot;.

Geographic entities mentioned:
surface_form: Sgùrr Dearg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.2127
lon: -6.2348388888889
Liathach. Geology. The mountain is composed of Torridonian sandstone which forms massive near-horizontal strata. They form the numerous terraces that are obvious from afar. The rocks are mainly red and chocolate sandstones, arkoses, flagstones and shales with coarse conglomerates locally at the base.

Geographic entities mentioned:
surface_form: liathach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.564327777778
lon: -5.4621222222222
It is about 500 million years old. The Torridon landscape is itself highly denuded by glacial and alluvial action, and represents the remnants of an ancient peneplain. Climbing. Liathach has four listed &quot;Tops&quot; in the Munro Tables, Meall Dearg at 3133 feet (955 m) stands off the main ridge at the end of the Northern Pinnacles which run north from Mullach an Rathain.

Geographic entities mentioned:
surface_form: mullach an rathain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.564327777778
lon: -5.4621222222222
The second floor contains bedrooms, bathrooms, kitchens, dining rooms, storage, and a sewing room. The attic originally included a screened-in sleeping area for the hot San Joaquin Valley but it was later closed in after the installation of air conditioning. Julia Morgan designed many other YWCA buildings in California and beyond.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Women's groups honored Mink by forming a human lei of approximately 900 women who surrounded the tent where Mink's casket stood in the capital atrium, while singing Hawaiian songs. She was buried at the National Memorial Cemetery of the Pacific, near the Punchbowl Crater.

Geographic entities mentioned:
surface_form: Punchbowl Crater
instance_of: Mountain
countries: United States
coordinates: lat: 21.3125
lon: -157.84611111111
Wellsee. Wellsee is a lake in Schleswig-Holstein, Germany. At an elevation of 29 m, its surface area is 0.25 km².

Geographic entities mentioned:
surface_form: wellsee
instance_of: Lake
countries: Germany
coordinates: lat: 54.280555555556
lon: 10.183888888889
Its three massive terraces rise above the desert floor and into the cliffs of Deir el-Bahari. Hatshepsut's tomb, KV20, lies inside the same massif capped by El Qurn, a pyramid for her mortuary complex. At the edge of the desert, east, connected to the complex by a causeway, lies the accompanying valley temple.

Geographic entities mentioned:
surface_form: El Qurn
instance_of: Mountain
countries: Egypt
coordinates: lat: 25.73638889
lon: 32.59611111
Mortuary complex. It has been suggested that Hatshepsut's tomb in the Valley of the Kings, KV20, was meant to be an element of the mortuary complex at Deir el-Bahari. The arrangement of the temple and tomb bear a spatial resemblance to the pyramid complexes of the Old Kingdom, which comprised five central elements: valley temple, causeway, mortuary temple, main pyramid, and cult pyramid.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Hatshepsut's temple complex included the valley temple, causeway, and mortuary temple. Her tomb was built into the massif of the same cliffs as the temple, beneath the dominating peak of El Qurn (AMSL) that caps her tomb, in a sense, like the pyramid capped the tomb of an Old Kingdom pharaoh. Further, her tomb aligns with the offering hall of the mortuary cult complex.

Geographic entities mentioned:
surface_form: El Qurn
instance_of: Mountain
countries: Egypt
coordinates: lat: 25.73638889
lon: 32.59611111
Shaheeya Lake. Shaheeya Lake is located in Glacier National Park, in the U.S. state of Montana. Shaheeya Lake is east of Shaheeya Peak.

Geographic entities mentioned:
surface_form: Shaheeya Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.9558
lon: -113.973
surface_form: shaheeya lake
instance_of: Lake
countries: United States
coordinates: lat: 48.9561
lon: -113.959
Shaheeya Lake. Shaheeya Lake is located in Glacier National Park, in the U.S. state of Montana. Shaheeya Lake is east of Shaheeya Peak.

Geographic entities mentioned:
surface_form: shaheeya lake
instance_of: Lake
countries: United States
coordinates: lat: 48.9561
lon: -113.959