Sarmila/GeoWiki-Features huggingface dataset:
The amphiboles in the rocks formed at depths of. The magma output of Ciomadul is about while magma chamber recharge may have reached. Eruptive history. Ciomadul has been active for over half a million years, with the oldest activity between 1,000,000 and 750,000 years ago forming lava domes.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Older estimates indicate that activity did not start before 250,000 years ago, while more recent research indicated a start of volcanism over 600,000/ 850,000 years ago. Volcanism at Ciomadul consisted mostly of the extrusion of lava domes, their collapse forming block-and-ash flows and subplinian and Vulcanian eruptions separated by long periods of rest.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
The volcanic history of Ciomadul has been subdivided into an effusive phase that lasted until about 440,000 years ago and an explosive phase that began 200,000 years ago during which magma output increased 30-fold and which is known as &quot;young Ciomad&quot;.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomad
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
An alternative description envisages an &quot;old Ciomadul&quot; between 1,000,000 — 300,000 years ago and a &quot;young Ciomad eruptive period&quot; between 160,000 — 30,000 years ago, with the latter in turn subdivided into five stages that emplaced about of rock. A gap of about 500,000 years separates Ciomadul from the activity of other volcanoes in the area.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomad
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
This effusive phase is also known as &quot;old Ciomad&quot;, and eruptions were separated by long pauses without volcanic activity from each other. The dates obtained by potassium-argon dating are much older; there is substantial disagreement between dates obtained by potassium-argon dating or argon-argon dating on the one hand and uranium-thorium dating on the other hand at Ciomadul.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Explosive eruptions became common only about 57,000 years ago. Between 56,000 and 32,000 years ago, explosive activity occurred at Ciomadul. That timespan coincides with the deposition of tephra from volcanoes in Italy in Europe; it is possible that tephra also came from Ciomadul. Indeed, the age of Ciomadul's last eruption overlaps with the age of the Campanian Ignimbrite. Tephras.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Tephras. Ciomad has produced far-flung tephras, which reached as far as Ukraine and have been recovered from the Ursului Cave of the Perșani Mountains. Some tephra layers found in two drilling cores of the Black Sea may have originated at Ciomad but reliably distinguishing between Ciomadul tephras and these from Nisyros and Anatolian volcanoes is difficult.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomad
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Some tephra layers found in two drilling cores of the Black Sea may have originated at Ciomad but reliably distinguishing between Ciomadul tephras and these from Nisyros and Anatolian volcanoes is difficult. The Roxolany Tephra has been found as far as Odesa, Ukraine, away from Ciomadul.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
From the other point of view, the clinopyroxene‐bearing Roxolany tephra was unlikely to be derived from Ciomadul, as it differs significantly from Ciomadul typical phenocryst assemblage containing amphibole.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
After the last eruption, the lava domes were subject to glacial weathering, such as frost shattering that produced stone runs. An 1838 document by an unknown author stated that even old legends do not record eruptive activity at Ciomadul, and there is no evidence in Lake Sfânta Ana sediments of tephra layers that might indicate more recent eruptions. Current status.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Current status. Presently, Ciomadul displays seismic activity, release of carbon dioxide from bubbling pools and bogs and mofettas and anomalous heat flow reaching. Outgassing of carbon dioxide, hydrogen sulfide and mostly abiotic methane have been found at Ciomadul, forming sulfide deposits in some caverns.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
The gases may come directly from the mantle, rather than from magma. At depths of and especially, a magma chamber has been identified beneath Ciomadul, based on magnetotelluric data, and several of magma may still be stored underneath Ciomadul. An alternative explanation is that there are less than a few cubic kilometres of magma.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
A deeper basaltic melt zone may also exist at a depth of around. Further, a zone of low seismic velocity has been identified with geophysical and seismic modelling in the lower crust and upper mantle beneath Ciomad, down to depths of or. Hydrothermal activity has been noted at Ciomadul and Tușnad-Băi, including a high temperature system at depth with temperatures exceeding.

Geographic entities mentioned:
surface_form: ciomad
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Such volcanoes can constitute a threat to regions with seemingly quiet volcanism. Ciomadul has had repose periods that lasted longer than the timespan elapsed since the last eruption. Zircon crystallization data imply that the magma chambers of Ciomadul were active over time spans of over 300,000 years.

Geographic entities mentioned:
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
surface_form: ciomadul
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Magma output progressively decreased during time, with early volcanoes being large stratovolcanoes sometimes featuring caldera-forming eruptions, while more recent activity includes monogenetic volcanoes although more precise dating and volume estimation efforts at Ciomad have found an increase of eruption rates over time.

Geographic entities mentioned:
surface_form: ciomad
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
Explosive eruptions became common only about 57,000 years ago. Between 56,000 and 32,000 years ago, explosive activity occurred at Ciomadul. That timespan coincides with the deposition of tephra from volcanoes in Italy in Europe; it is possible that tephra also came from Ciomadul. Indeed, the age of Ciomadul's last eruption overlaps with the age of the Campanian Ignimbrite. Tephras.

Geographic entities mentioned:
surface_form: ciomad
instance_of: Mountain
countries: Romania
coordinates: lat: 46.13
lon: 25.88
The Schwatka expedition found no remnants of the Franklin expedition south of a place now known as Starvation Cove on the Adelaide Peninsula. This was about north of Crozier's stated goal, the Back River, and several hundred miles away from the nearest Western outpost, on the Great Slave Lake.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
FM 1382. Farm to Market Road 1382 (FM 1382) is located in Dallas County. It runs from I-35E in DeSoto to SH 180 in Grand Prairie. Most of the highway is part of Belt Line Road, becoming its own route through Cedar Hill around Joe Pool Lake. FM 1382 is one of only two farm to market roads remaining in Dallas County, the other being FM 1389. FM 1382 begins at I-35E in DeSoto.

Geographic entities mentioned:
surface_form: Joe Pool Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.628611111111
lon: -97.005277777778
Fiji's third largest island is separated from Vanua Levu by the Somosomo Strait. The island is between wide and long, representing the top of a dormant, elongated shield volcano which erupted from a northeast–southwest trending rift on the ocean floor. About 150 volcanic cones dot the island, including Uluigalau, Fiji's second highest peak at, and Des Vœux Peak, next in height at.

Geographic entities mentioned:
surface_form: Uluigalau
instance_of: Mountain
countries: Fiji
coordinates: lat: -16.8167
lon: 179.967
Particularly hard hit was western North Carolina, where flooding and mudslides led to the closure of more than 40 roads, including parts of the Blue Ridge Parkway. Approximately 2,000 people fled their homes in McDowell County due to the threat of failure of the dam at Lake Tahoma. Alberto caused eight deaths and about $125 million in damage in the United States. Hurricane Beryl.

Geographic entities mentioned:
surface_form: Lake Tahoma
instance_of: Lake
countries: United States
coordinates: lat: 35.7233
lon: -82.08
Hatton railway station is the busiest railway station in the Nuwara Eliya District and the second-busiest railway station in the Central Province. Approximately 1 million passengers use the station during the pilgrimage period to Adam's Peak (Sri Pada) (which begins in December and ends in May).

Geographic entities mentioned:
surface_form: Adam's Peak
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.809444444444445
lon: 80.49972222222222
Calamovilfa arcuata. &quot;Calamovilfa arcuata&quot;, commonly known as Cumberland sandreed, is a species of flowering plant in the grass family. It is native to the southeastern United States, where it is found in river scour zones. Due to its specialized habitat, it has a highly localized range, found only on the Cumberland Plateau and in the Ouachita Mountains. Natural history.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Brooks Mountain. Brooks Mountain is the highest peak in the York Mountains range on the Seward Peninsula in the U.S. state of Alaska. It is located in the central part of the Teller Quadrangle, about east of Cape Prince of Wales. It has an elevation of. It has tin ore deposits, and high-grade uranium has also been found in the form of zeunerite. Geography.

Geographic entities mentioned:
surface_form: brooks mountain
instance_of: Mountain
countries: United States
coordinates: lat: 65.5369
lon: -167.143
It has an elevation of. It has tin ore deposits, and high-grade uranium has also been found in the form of zeunerite. Geography. Brooks Mountain is an extension of the York Mountain Range and is its highest peak. The York Mountains range forms the watershed divide between north flowing rivers which flow into the Arctic Ocean and the streams that flow into the Bering Sea on the south.

Geographic entities mentioned:
surface_form: brooks mountain
instance_of: Mountain
countries: United States
coordinates: lat: 65.5369
lon: -167.143
The York Mountains range forms the watershed divide between north flowing rivers which flow into the Arctic Ocean and the streams that flow into the Bering Sea on the south. The principal rivers rising from the Brooks Mountain are the Mint River, York Creek which joins the Pinauk River, Anderson Creek tributary of the Don River and the Crystal River which is a tributary of the Lost River.

Geographic entities mentioned:
surface_form: brooks mountain
instance_of: Mountain
countries: United States
coordinates: lat: 65.5369
lon: -167.143
These are sedimentary formations which are interspersed with many dykes of granite and rhyolite, generally oriented in an east and west strike. Tourmaline and garnet are also recorded. Tin Creek and Cassiterite Creek, about south of Brooks Mountain, have tin ore deposits in tourmaline and garnet rocks. Uranium.

Geographic entities mentioned:
surface_form: brooks mountain
instance_of: Mountain
countries: United States
coordinates: lat: 65.5369
lon: -167.143
The group's fourth studio album &quot;I Quit&quot; was released on June 20, 2025 to favorable reviews. Early career. The three sisters, Este Arielle (born March 14, 1986), Danielle Sari (born February 16, 1989) and Alana Mychal (born December 15, 1991) were all born and raised in the San Fernando Valley, California, U.S., to Jewish parents.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
King's Seat Hill. King's Seat Hill is a hill in the Ochil Hills range, part of the Central Lowlands in Scotland. A popular hill, paths originate from the foothill towns of Tillicoultry and Dollar to the southwest and southeast respectively, but the hill is also climbed as part of a cross-range walk.

Geographic entities mentioned:
surface_form: Central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
This list includes significant mountains and hills located in Antigua and Barbuda. Most of the highest mountains and hills of Antigua are located in the Shekerley Mountains, while all of the highest points of Barbuda are located in the Barbuda Highlands. Out of the sixty-five named peaks in the country, the tallest is Boggy Peak, at a height of 402 metres.

Geographic entities mentioned:
surface_form: Boggy Peak
instance_of: Mountain
countries: Antigua and Barbuda
coordinates: lat: 17.05
lon: -61.85
Leaving Singapore on 27 March 1964, she proceeded through the Strait of Malacca, stopped at Penang Island in Malaysia, then crossed the Andaman Sea, Bay of Bengal, and Indian Ocean &ndash; becoming the first ship in the history of the United States Coast Survey or U.S.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The dead bodies of Falck and Gräns were later found at the bottom of the Hammarby Canal in Stockholm. The deaths remain unsolved but later reports claim that they were assassinated in a state-sponsored operation by agents from East Germany. Cats Falck was born in Enskede in Stockholm, Sweden.

Geographic entities mentioned:
surface_form: Hammarby Canal
instance_of: Lake
countries: Sweden
coordinates: lat: 59.3075
lon: 18.1
KV42. Tomb KV42 (Kings Valley 42) is an ancient Egyptian tomb in the Valley of the Kings near Luxor, Egypt. It was constructed for Hatshepsut-Meryetre, the wife of Thutmose III, but she was not buried in the tomb. It may have been reused by Sennefer, a mayor of Thebes during the reign of Amenhotep II, and by several members of his family.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Hystoe. Hystoe or Hystoë was a town of ancient Crete, which the Scholiast on Aratus connects with the Idaean nymph Cynosura, one of the nurses of Zeus.

Geographic entities mentioned:
surface_form: Idaean
instance_of: Mountain
countries: Turkey
Arab sources claim Umayyad commander Qutayba ibn Muslim briefly took Kashgar from China and withdrew after an agreement, but modern historians entirely dismiss this claim. The Arab Umayyad Caliphate in 715 deposed Ikhshid, the king the Fergana Valley, and installed a new king Alutar on the throne. The deposed king fled to Kucha (seat of Anxi Protectorate), and sought Chinese intervention.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Net River (Minnesota). The Net River is a tributary of the South Fork Nemadji River in Pine and Carlton counties, Minnesota, United States. Via the Nemadji River, it flows to Lake Superior at Superior, Wisconsin. &quot;Net River&quot; is probably an English translation of the Ojibwe-language name.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Later in the month the Novgorod Operational Group, under Northwestern Front command, was formed, and by October 1 it consisted of the 185th, 180th, and 305th Rifle Divisions, plus the 3rd Tank Division, which had no tanks and was converting to infantry. The Group was defending a 30km sector along the Volkhov River from Dubrovka to Lake Ilmen. Battle for Kalinin.

Geographic entities mentioned:
surface_form: Lake Ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
Pearl Peak. Pearl Peak is a summit in the southern part of the Ruby Mountains, in Elko County, Nevada in the United States. The peak, which is within the Humboldt-Toiyabe National Forest, is primarily composed of Ordovician to early Devonian dolomite and limestone, with minor amounts of sandstone and quartzite. It hosts a stand of bristlecone pine.

Geographic entities mentioned:
surface_form: pearl peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.236
lon: -115.5412
The peak, which is within the Humboldt-Toiyabe National Forest, is primarily composed of Ordovician to early Devonian dolomite and limestone, with minor amounts of sandstone and quartzite. It hosts a stand of bristlecone pine. Pearl Peak is about south of Elko and north of Eureka. The Ruby Lake National Wildlife Refuge is located a short distance to the southeast.

Geographic entities mentioned:
surface_form: pearl peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.236
lon: -115.5412
Tingri Plain. The Tingri Plain is a plateau in Tibet Autonomous Region, China, not far north of Mount Everest. Climbers who are headed to Everest often cross this plain after making a base in the town of Tingri. Many folk legends in the history of Nepal are linked with it, especially about Kathmandu. The Powerful goddess 'Taleju Bhawani' a Yakshini is said to be from the Tingri Plain.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Although as late as the mid-1950s most of the SBH congregation remained in the Central District, the neighborhood was becoming increasingly African American, its Jews were becoming increasingly educated and prosperous, and most of the Jews were moving out, especially to the Eastside suburbs, Mercer Island in Lake Washington, and the south Seattle neighborhood of Seward Park.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
This village is the only urban area in the municipality according to Statistics Norway. The village lies in the Glåma river valley and the mountain Håmmålsfjellet lies about south of the village. The village of Dalsbygda lies about to the northwest of this village and the village of Narbuvoll lies about to the southeast of this village.

Geographic entities mentioned:
surface_form: Håmmålsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.429611111111
lon: 11.274611111111
Maracaibo. Maracaibo (,;) is a city and municipality in northwestern Venezuela, located on the western shore of the strait that connects Lake Maracaibo to the Gulf of Venezuela. It is the capital of Zulia state and the second-largest city in Venezuela and is the second-largest city proper in Venezuela, after the national capital, Caracas.

Geographic entities mentioned:
surface_form: Lake Maracaibo
instance_of: Lake
countries: Venezuela
coordinates: lat: 9.8158333333333
lon: -71.556666666667
Yunus resumed his role as the deputy of his brother upon Fakhr al-Din's return in 1618. The Ma'ns expanded their control and tax farms to the Beqaa Valley and much of the Tripoli Eyalet, and their defiance of the Ottomans led to another punitive campaign in 1633. Ali was killed in the fighting, while Yunus was captured along with Mulhim and his brother Hamdan in the Jabal Amil area.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
The tax farm was renewed on an almost yearly basis until 1657. Consolidation in Mount Lebanon. In November 1650 he defeated Ibshir Mustafa Pasha, the governor of Damascus in an engagement in the Qarnana Valley. Another account held that Mulhim, with backing from the Ma'ns' longtime allies the Shihabs of Wadi al-Taym, defeated Damascene government forces hired by Alam al-Din in that clash.

Geographic entities mentioned:
surface_form: Wadi al-Taym
instance_of: Valley
countries: Lebanon
coordinates: lat: 33.4333
lon: 35.7
The mountain consists of an upper summit ridge with two distinct peaks and a lower plateau and ledge that hangs just above the center of Farmington. This ledge is contiguous with the lower ridges of Talcott Mountain to the north and Rattlesnake Mountain to the south. The Metacomet Ridge continues north and south from Farmington Mountain over those peaks.

Geographic entities mentioned:
surface_form: Talcott Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.825
lon: -72.798
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.458333333333
lon: -121.80611111111
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.25243
lon: -115.60644
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1322
lon: -74.8634
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6997
lon: -72.8328
surface_form: rattlesnake mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.4056
lon: -119.611
Recreation and conservation. Both the Hill-Stead Museum and the town of Farmington manage networks of walking paths on the mountain. Farmington Mountain is also traversed by the Metacomet Trail, (maintained by the Connecticut Forest and Park Association), which extends from the Hanging Hills of Meriden, Connecticut, to the Massachusetts border.

Geographic entities mentioned:
surface_form: Hanging Hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
The historic Hill-Stead Museum, known for its French Impressionist masterpieces, architecture, and stately grounds is located on the northern part of the ridgeline. The southern half of the mountain is made up of largely wooded cliffs; the Farmington Reservoir is nestled between the ridge high point and the edge of the lower plateau. Other parts of the mountain are occupied by suburban housing.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
Farmington Mountain. Farmington Mountain, is a traprock ridge located southwest of Hartford, Connecticut, in the town of Farmington. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Other parts of the mountain are occupied by suburban housing. The east side of Farmington Mountain drains into Trout Brook, then to the Park River, thence into the Connecticut River and Long Island Sound; the west side into the Farmington River, thence to the Connecticut River. Geology and ecology.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
Farmington Mountain. Farmington Mountain, is a traprock ridge located southwest of Hartford, Connecticut, in the town of Farmington. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border. Farmington Mountain is known for its microclimate ecosystems, rare plant communities, and for the historic Hill-Stead Museum. Farmington Mountain is traversed by the Metacomet Trail. Geography.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
Farmington Mountain is traversed by the Metacomet Trail. Geography. Roughly long by wide, Farmington Mountain rises steeply above the town of Farmington to the west. The mountain consists of an upper summit ridge with two distinct peaks and a lower plateau and ledge that hangs just above the center of Farmington.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
This ledge is contiguous with the lower ridges of Talcott Mountain to the north and Rattlesnake Mountain to the south. The Metacomet Ridge continues north and south from Farmington Mountain over those peaks. The wooded ridgeline of Farmington Mountain is less distinct that its neighboring peaks on the Metacomet Ridge. Nonetheless, the mountain contains a number of prominent features.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
Geology and ecology. Farmington Mountain, like much of the Metacomet Ridge, is composed of basalt, also called traprock, a volcanic rock. The mountain formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
The mountain formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the cliffs and ridgeline of Farmington Mountain.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Farmington Mountain is also an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Farmington Mountain). Hill-Stead.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
Hill-Stead. Hill-Stead, now a museum, was created on of Farmington Mountain as a country estate for wealthy industrialist Alfred Atmore Pope, to the designs of his daughter Theodate Pope Riddle in 1901. Theodate inherited the house after her parents deaths, and prior to her own passing in 1946 willed Hill-Stead Museum as a memorial to her parents.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
The Farmington Reservoir Trail, located on the southwest side of the mountain and managed by the town of Farmington, is open to hiking, bird watching, picnicking, snowshoeing, and other passive pursuits. The Metacomet Trail can be accessed from the same trailhead. The ecosystem and ridgeline of Farmington Mountain are most threatened by development.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
In 2000, Farmington Mountain was included in a study by the National Park Service for the designation of a new National Scenic Trail now tentatively called the New England National Scenic Trail, which would include the Metacomet-Monadnock Trail in Massachusetts and the Mattabesett Trail and Metacomet Trail trails in Connecticut.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
The is active in the conservation of Farmington Mountain and its viewshed. The trust has secured a number of easements on the lower slopes of the mountain and adjacent parts of Metacomet Ridge.

Geographic entities mentioned:
surface_form: farmington mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.713433333333
lon: -72.815652777778
Vodno. Vodno () is a mountain in North Macedonia. It is located in the northern part of the country, to the southwest of the capital city Skopje. The highest point of the mountain is on &quot;Krstovar peak&quot;, at 1066 meters and the submontane is at 337 meters (Middle Vodno is on 557 m). In 2002, on Krstovar peak the Millennium Cross was built, one of the biggest Christian Crosses in the world.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
In 2002, on Krstovar peak the Millennium Cross was built, one of the biggest Christian Crosses in the world. Climate. The climate in Vodno is cold and temperate. Vodno has a significant amount of rainfall during the year. This is true even for the driest month. The average temperature is.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
The average temperature is. The lowest temperature measured on the mountain, in January 2017, is; and the highest measured temperature, in July 2005, is. Hydrography. Vodno has a heterogeneous hydrographic web: streams, vaults, waterfalls, springs. Vodno has a lot of streams which are used by the shepherds for feeding their goats and for watering the wild chestnuts.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
The water is bacteriologically and chemically clean. Vodno has a mini waterfall which is 15 meters high and is more active in spring when the snow coverlet is melting. Vodno has a lot of springs too that are used for the need of the local people. Vegetation. On Vodno mountain, deciduous and evergreen plants can be found. From the deciduous, there is the wild chestnut, lime tree, oak etc.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
Recently it has attracted people from Skopje, who have a weekend house or have permanently relocated there, due to its proximity to the capital and its clean air, beautiful surroundings, and medieval churches. Additionally the hike from Middle Vodno (557 m) to the Krstovar Peak (1066 m), where the Millennium Cross is located, has become a highly attractive leisure activity.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
The increase in interest in this activity can be attributed to the opening of a bus-line that makes round-trips from the Skopje City Centre to Middle Vodno, as well as the availability of cable transport from Middle Vodno to Krstovar Peak. Cultural Tourism. Various manifestations, churches, monasteries and monuments can be found on Vodno. Churches and Monasteries.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
The increase in interest in this activity can be attributed to the opening of a bus-line that makes round-trips from the Skopje City Centre to Middle Vodno, as well as the availability of cable transport from Middle Vodno to Krstovar Peak. Cultural Tourism. Various manifestations, churches, monasteries and monuments can be found on Vodno. Churches and Monasteries.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
They attract more visitors due to their historical significance. Monuments. The monuments are the most visited attractions on Mount Vodno. One of the most distinct landmarks on Mount Vodno is the Millennium Cross. Found on the peak of Mount Vodno, and standing at 66 metres high, it is one of the most visited locations in the Skopje region.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
One of the most distinct landmarks on Mount Vodno is the Millennium Cross. Found on the peak of Mount Vodno, and standing at 66 metres high, it is one of the most visited locations in the Skopje region. It was constructed in 2002, in order to commemorate 2000 years since the birth of Christ, and serves as a memorial of two millennia of Christianity. Cable car.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
Cable car. As of 2011, a gondola lift has been in operation to allow an easy ascent to visit the Millennium Cross. The ropeway includes 28 regular gondolas for eight persons and two VIP gondolas for four people. The lift starts at Middle Vodno and ends at the Millennium Cross. The route is 1,750m long, with the ride lasting 6–8 minutes.

Geographic entities mentioned:
surface_form: vodno
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.96527778
lon: 21.39444444
Thomson's launched her on 20 May 1893 and quickly her fitted out, giving her a capacity for a combined total of 1,065 passengers and crew. The B&CDR named her &quot;Slieve Donard&quot; after the highest peak in the Mourne Mountains in County Down. At the same time Thomson built an exact sister ship, for the Glasgow and South Western Railway.

Geographic entities mentioned:
surface_form: Slieve Donard
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.180277777778
lon: -5.9208333333333
Winter temperatures can drop below −20 °C with wind chill factors reaching temperatures below −30 °C. Despite the modest elevation, the climate supports a glacier in the north cirque. Most precipitation runoff from Mount Begbie drains east into tributaries of the Columbia River; however, a portion drains west into the Eagle River, a tributary of the Fraser River. Geology.

Geographic entities mentioned:
surface_form: eagle river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.8431
lon: -119.011
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount begbie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8848
lon: -118.2506
Mount Begbie. Mount Begbie is a mountain summit located in the Gold Range of the Monashee Mountains in British Columbia, Canada. Situated west of the Columbia River high above the shore of Upper Arrow Lake, this prominent peak is visible from the Trans-Canada Highway, Revelstoke, and Revelstoke Mountain Resort ski area. Mt. Begbie Brewing Company, a brewery, was named after the mountain.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount begbie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8848
lon: -118.2506
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Begbie. Mount Begbie is a mountain summit located in the Gold Range of the Monashee Mountains in British Columbia, Canada. Situated west of the Columbia River high above the shore of Upper Arrow Lake, this prominent peak is visible from the Trans-Canada Highway, Revelstoke, and Revelstoke Mountain Resort ski area. Mt. Begbie Brewing Company, a brewery, was named after the mountain.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: upper arrow lake
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
surface_form: arrow lake
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The nearest peak is Mount Tilley, to the west, and the nearest higher peak is Blanket Mountain, to the south. History. Mount Begbie is named for Sir Matthew Baillie Begbie (1819–1894), a prominent judge in the British Columbia colony. The first ascent of the mountain was accomplished June 11, 1907, by James Robert Robertson, J. Herdman, and Rupert W. Haggen, with Edward Feuz Jr. as guide.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount begbie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8848
lon: -118.2506
Mount Begbie. Mount Begbie is a mountain summit located in the Gold Range of the Monashee Mountains in British Columbia, Canada. Situated west of the Columbia River high above the shore of Upper Arrow Lake, this prominent peak is visible from the Trans-Canada Highway, Revelstoke, and Revelstoke Mountain Resort ski area. Mt. Begbie Brewing Company, a brewery, was named after the mountain.

Geographic entities mentioned:
surface_form: mount begbie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8848
lon: -118.2506
Climate. Based on the Köppen climate classification, Mount Begbie is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors reaching temperatures below −30 °C. Despite the modest elevation, the climate supports a glacier in the north cirque.

Geographic entities mentioned:
surface_form: mount begbie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8848
lon: -118.2506
Geology. Mount Begbie is part of the Monashee complex located in the southern part of the Omineca Belt of the Canadian Cordillera (Okulitch 1984, Wheeler & McFeely 1991). The Monashee complex is the lowest structural unit of the Shuswap Metamorphic Complex and exposes rock of ancestral North America (Canadian shield).

Geographic entities mentioned:
surface_form: mount begbie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8848
lon: -118.2506
Mount Begbie. Mount Begbie is a mountain summit located in the Gold Range of the Monashee Mountains in British Columbia, Canada. Situated west of the Columbia River high above the shore of Upper Arrow Lake, this prominent peak is visible from the Trans-Canada Highway, Revelstoke, and Revelstoke Mountain Resort ski area. Mt. Begbie Brewing Company, a brewery, was named after the mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mt. Begbie Brewing Company, a brewery, was named after the mountain. The nearest peak is Mount Tilley, to the west, and the nearest higher peak is Blanket Mountain, to the south. History. Mount Begbie is named for Sir Matthew Baillie Begbie (1819–1894), a prominent judge in the British Columbia colony. The first ascent of the mountain was accomplished June 11, 1907, by James Robert Robertson, J.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount tilley
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8882
lon: -118.3015
The nearest peak is Mount Tilley, to the west, and the nearest higher peak is Blanket Mountain, to the south. History. Mount Begbie is named for Sir Matthew Baillie Begbie (1819–1894), a prominent judge in the British Columbia colony. The first ascent of the mountain was accomplished June 11, 1907, by James Robert Robertson, J. Herdman, and Rupert W. Haggen, with Edward Feuz Jr. as guide.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Haggen, with Edward Feuz Jr. as guide. The mountain's name was officially adopted in 1932 when approved by the Geographical Names Board of Canada, although this toponym had appeared in publications as early as 1887, if not earlier. Climate. Based on the Köppen climate classification, Mount Begbie is located in a subarctic climate zone with cold, snowy winters, and mild summers.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Unterseen literally means &quot;Lower Lake&quot;, which is correct, since Unterseen is located on the flat area on the eastern shore of Lake Thun between the two creek Lombach below the &quot;Chienberg&quot; to the north and the Aare to the south, which both flow into Lake Thun.

Geographic entities mentioned:
surface_form: Lake Thun
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.683333333333
lon: 7.7166666666667
The historic town however is mainly found at the northern bank of the Aare, which flows here from Lake Brienz to Lake Thun (therefore &quot;lower lake&quot;). Just across the Aare is the town of Interlaken. Both municipalities are located on the flat alluvial land among steep mountains, which is also called the Bödeli.

Geographic entities mentioned:
surface_form: Lake Brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
Both municipalities are located on the flat alluvial land among steep mountains, which is also called the Bödeli. Unterseen belongs to the Small Agglomeration &quot;Interlaken&quot; with 23,300 inhabitants (2014). Along with Interlaken, Unterseen is an important tourist center in the Bernese Highlands, and from the town one can see the mountains Eiger, Mönch and Jungfrau. History.

Geographic entities mentioned:
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
surface_form: Mönch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.558333333333
lon: 7.9972222222222
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
Of the water in the municipality, 0.2% is in lakes and 2.4% is in rivers and streams. Of the unproductive areas, 2.7% is unproductive vegetation and 1.4% is too rocky for vegetation. The municipality is located on the alluvial land called Bödeli between Lake Thun and Lake Brienz. It is across the Aare to the north from the town of Interlaken.

Geographic entities mentioned:
surface_form: Lake Thun
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.683333333333
lon: 7.7166666666667
surface_form: Lake Brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
Neale was the chief pilot for all four survey flights. During this period, several new salt lakes were discovered. The largest was named Lake Mackay, and another Lake Neale. The aircraft used for the 1930 series were English built Air Navigation Experimental Company ANEC IIIs, which were converted in Australia by Larkin's Company.

Geographic entities mentioned:
surface_form: Lake Mackay
instance_of: Lake
countries: Australia
coordinates: lat: -22.5
lon: 128.58333333333
One premium of $1,107.60 was paid before the incident. Mr. Small had two properties previously destroyed by mysterious fires before the one that claimed the life of his third wife, Florence. Crime. Mrs. Small's body was found in the ruins of the couple's burnt two-story cottage in Ossipee, New Hampshire, near Ossipee Lake following a fire that occurred during the evening of September 28, 1916. Mr.

Geographic entities mentioned:
surface_form: Ossipee Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.791388888889
lon: -71.139722222222
According to the 2021 census, the Municipality of Lamia has a population of 66,657 while Lamia itself has 47,529 inhabitants. The city is located on the slopes of Mount Othrys, near the river Spercheios. It serves as the agricultural center of a fertile rural and livestock area. Name.

Geographic entities mentioned:
surface_form: Mount Othrys
instance_of: Mountain
countries: Greece
coordinates: lat: 39.016944444444
lon: 22.709722222222
It forms the end of a mountain ridge that runs from the 2,249 m high &quot;Hochkogel&quot; over the 2,092 m high &quot;Saalbachkogel&quot; and the 2,123 m high &quot;Stemmerkogel&quot; to the north. To the west is the &quot;Schwarzachgraben&quot; stream, to the east the valley of the &quot;Löhnersbach&quot; which descends into the Glemmtal.

Geographic entities mentioned:
surface_form: Glemmtal
instance_of: Valley
countries: Austria
coordinates: lat: 47.3833
lon: 12.6333
surface_form: glemmtal
instance_of: Valley
countries: Austria
coordinates: lat: 47.3833
lon: 12.6333
Schattberg (Saalbach-Hinterglemm). The Schattberg is a high mountain in the Kitzbühel Alps in the Austrian state of Salzburg. Location and surrounding area. The Schattberg is the local mountain for the Pinzgau parish of Saalbach-Hinterglemm, that lies about 3 kilometres to the north.

Geographic entities mentioned:
surface_form: schattberg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.3628
lon: 12.6274
Location and surrounding area. The Schattberg is the local mountain for the Pinzgau parish of Saalbach-Hinterglemm, that lies about 3 kilometres to the north. It forms the end of a mountain ridge that runs from the 2,249 m high &quot;Hochkogel&quot; over the 2,092 m high &quot;Saalbachkogel&quot; and the 2,123 m high &quot;Stemmerkogel&quot; to the north.

Geographic entities mentioned:
surface_form: schattberg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.3628
lon: 12.6274