Sarmila/GeoWiki-Features huggingface dataset:
Lake Gratiot. Lake Gratiot is a lake in Keweenaw County, Michigan. The lake is surrounded by dense forest of the Keweenaw Peninsula. The bottom is mainly muck and it has a maximum depth of. The lake flows through the Little Gratiot River into Lac La Belle and then into Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: lac la belle
instance_of: Lake
countries: United States
coordinates: lat: 47.374166666667
lon: -87.985555555556
Lake Gratiot. Lake Gratiot is a lake in Keweenaw County, Michigan. The lake is surrounded by dense forest of the Keweenaw Peninsula. The bottom is mainly muck and it has a maximum depth of. The lake flows through the Little Gratiot River into Lac La Belle and then into Lake Superior.

Geographic entities mentioned:
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: lake gratiot
instance_of: Lake
countries: United States
coordinates: lat: 47.355277777778
lon: -88.126944444444
Lake Gratiot. Lake Gratiot is a lake in Keweenaw County, Michigan. The lake is surrounded by dense forest of the Keweenaw Peninsula. The bottom is mainly muck and it has a maximum depth of. The lake flows through the Little Gratiot River into Lac La Belle and then into Lake Superior.

Geographic entities mentioned:
surface_form: lake gratiot
instance_of: Lake
countries: United States
coordinates: lat: 47.355277777778
lon: -88.126944444444
It is among the longest and most water-abundant rivers in the Algiers region. The river originates in the Tell Atlas and the Khachna Mountains, near the municipality of Kedara in the Boumerdes province, flowing through Algiers before draining into Lake Reghaïa near the Réghaïa forest, and eventually emptying into the Mediterranean Sea. Description.

Geographic entities mentioned:
surface_form: Lake Reghaïa
instance_of: Lake
countries: Algeria
France
coordinates: lat: 36.770833333333336
lon: 3.3344444444444443
River mouth location. The mouth of the Reghaïa Valley is located between the municipalities of Reghaïa and H'raoua, in proximity to the confluences of the Buduau Valley and El-Hamiz valley. This picturesque site lies east of the El-Harrach Valley mouth and Sablons beach, making it a strategically location near the railway line connecting El-Harrach to Reghaïa.

Geographic entities mentioned:
surface_form: El-Harrach Valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.7336
lon: 3.13722
Reghaïa Valley. Reghaïa Valley is one of the rivers in the province of Algiers, stretching 17.13 kilometers to the east of the Algerian capital. Its mouth is located between the municipalities of Reghaïa and H'raoua. It is among the longest and most water-abundant rivers in the Algiers region.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
Description. The spring of Reghaïa Valley is located at Ben Ammar Valley in the municipality of Bouzegza Keddara, within the Khachna Mountains, at an elevation of 500 meters above sea level. The river is part of the Mediterranean basin.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
surface_form: bouzegza
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 36.607807
lon: 3.4443945
The river is part of the Mediterranean basin. Reghaïa Valley serves as a natural boundary between the municipalities of Reghaïa and H'raoua, creating an outlet through a drainage basin that covers an area of approximately 75 to 88 square kilometers and has a perimeter of around 42 kilometers. Geology.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
Geology. Reghaïa Valley site is located at the eastern geological boundary of the Mitidja syncline, a region formed by the emergence of elevations resulting from tectonic movements that brought volcanic rocks and smooth stones from the Tell Atlas, spreading across the entire Mitidja plain.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
The coastal areas along the Mediterranean Sea feature a series of raised surfaces created by the withdrawal of seawater, leaving behind cohesive landforms. The northern banks of the Reghaïa Valley exhibit a steep gradient. During the Pliocene epoch, erosion occurred along the riverbanks, leading to the formation of blue deposition rocks during the piacenzian stage.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
The northern banks of the Reghaïa Valley exhibit a steep gradient. During the Pliocene epoch, erosion occurred along the riverbanks, leading to the formation of blue deposition rocks during the piacenzian stage. The sediments within the stream bed of the Reghaïa Valley are composed of fine gray sand, gravel, and pebble, with a thickness of several meters. Main source.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
Main source. Reghaïa Valley originates in the western part of the Bouzegza Keddara municipality within Boumerdes Province, approximately 14.34 kilometers (8.91 miles) in a straight line from its mouth at the Mediterranean Sea along the coast of Algiers Province. This source is situated within the Tell and Khachna Mountains, which lie between the provinces of Médéa, Bouira, Blida, and Boumerdes.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
surface_form: bouzegza
instance_of: Mountain
countries: Algeria
France
coordinates: lat: 36.607807
lon: 3.4443945
This source is situated within the Tell and Khachna Mountains, which lie between the provinces of Médéa, Bouira, Blida, and Boumerdes. The path. Reghaïa Valley runs through two coastal Algerian states. Water bodies. The Reghaïa Valley intersects with several water bodies as it flows through the provinces of Algiers and Boumerdes in Algeria. National roads.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
The path. Reghaïa Valley runs through two coastal Algerian states. Water bodies. The Reghaïa Valley intersects with several water bodies as it flows through the provinces of Algiers and Boumerdes in Algeria. National roads. Reghaïa Valley crosses several national roads as it traverses through the provinces of Algiers and Boumerdes in Algeria. Train stations.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
National roads. Reghaïa Valley crosses several national roads as it traverses through the provinces of Algiers and Boumerdes in Algeria. Train stations. Reghaïa Valley intersects with several train stations as it flows through the region of Algiers and Boumerdes in Algeria. River mouth.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
River mouth. The mouth of the Reghaïa Valley is situated between the municipalities of Reghaïa and H'raoua in Algiers Province, near the &quot;Soumam&quot; neighborhood. The Valley serves as a boundary separating these two municipalities until it flows into the Mediterranean Sea along the coast of Algiers Province. River mouth location.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
River mouth location. The mouth of the Reghaïa Valley is located between the municipalities of Reghaïa and H'raoua, in proximity to the confluences of the Buduau Valley and El-Hamiz valley. This picturesque site lies east of the El-Harrach Valley mouth and Sablons beach, making it a strategically location near the railway line connecting El-Harrach to Reghaïa.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
This picturesque site lies east of the El-Harrach Valley mouth and Sablons beach, making it a strategically location near the railway line connecting El-Harrach to Reghaïa. The mouth of the Reghaïa Valley is approximately 26 kilometers east of the Casbah of Algiers and overlooks the Mediterranean Sea. Pollution.

Geographic entities mentioned:
surface_form: reghaïa valley
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
In addition to DDT, low concentrations of other chlorinated organic, insecticides, including lindane, heptachlor, aldrin, dieldrin, and endosulfan, have also been identified in the river. Measurements taken in 2004 indicated oxygen concentration values in the Reghaïa River that reflected minimum pollution thresholds, with a recorded level of 7 milligrams per liter at the riverbed.

Geographic entities mentioned:
surface_form: reghaïa river
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.78292
lon: 3.34505
Beyond the Shrouded Horizon. &quot;Beyond the Shrouded Horizon&quot; is the twenty-first studio album by English guitarist and songwriter Steve Hackett. Background and recording. &quot;Loch Lomond&quot; is named after the loch of the same name in Scotland. Hackett described the track as blues-influenced which changes to European music once the strings are heard.

Geographic entities mentioned:
surface_form: loch of the same name
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
It contains marginal notes. The text is rarely corrected. It contains Menologion. In Ephesian 6:14 phrase και ενδυσαμενοι τον θωρακα της δικαιοσυνης is omitted, but it was added at the margin. History. Formerly it was held in the Iviron monastery (825) at Athos peninsula. The codex now is located in the Bible Museum Münster (MS. 13).

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Itombwe Mountains. The Itombwe Mountains (or Itombwe Massif, Plateau) are a range of mountains in the South Kivu province of the Democratic Republic of the Congo (DRC). They run along the west shore of the northern part of Lake Tanganyika. They contain a vast area of contiguous montane forest and are home to a rich diversity of wildlife. Geography.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
The highest peak in the Itombwe range is Mount Mohi, at. Several other peaks are higher than. The mountains drop sharply in the east to the Ruzizi plain bordering Lake Tanganyika. They form a plateau that slopes down more gently to the west. The Elila River rises in the mountains, which are covered by forest except where rock bluffs emerge from the steepest slopes.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
The mountains drop sharply in the east to the Ruzizi plain bordering Lake Tanganyika. They form a plateau that slopes down more gently to the west. The Elila River rises in the mountains, which are covered by forest except where rock bluffs emerge from the steepest slopes. Temperatures range from about to, with a mean temperature of about all year round. Frost is occasionally experienced at night.

Geographic entities mentioned:
surface_form: Elila River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -2.741501
lon: 25.871429
The major mining center of Kamituga is near the north-west edge of the montane forest. Conservation issues. The range is still not protected, although there have been proposals to designate all the montane forest and two patches of lowland forest to the south of the upper Elila River as conservation areas. As of 2010 the mountains were inaccessible to tourists.

Geographic entities mentioned:
surface_form: Elila River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -2.741501
lon: 25.871429
The main axis of the tumulus is aligned in the direction of Mount Fuji, approximately 100 kilometers away, and which can be seen from the summit of the posterior circular portion. The mound is built in two steps, and there is no evidence that fukiishi were used. As with most other tumuli at this site, it has a double rectangular moat.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Rara snowtrout. The Rara snowtrout (&quot;Schizothorax raraensis&quot;), is a cyprinid fish species of the genus &quot;Schizothorax&quot;. The Rara snowtrout was first collected in 1979 in the alpine fresh water Rara Lake located in Nepal's Rara National Park.

Geographic entities mentioned:
surface_form: Rara Lake
instance_of: Lake
countries: Nepal
coordinates: lat: 29.525722222222
lon: 82.090211111111
Damga. Damga () is a summit in the northwestern part of the Rila Mountain in southwestern Bulgaria reaching height of 2,669 m. Damga is the main orographic node of northwestern Rila, connecting the ridges of Malyovitsa and Otovitsa. The peak is an impressive massif with mostly dome-shaped outlines.

Geographic entities mentioned:
surface_form: Malyovitsa
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.173861111111
lon: 23.363083333333
The peak is an impressive massif with mostly dome-shaped outlines. It dominates the western parts of the Urdina cirque containing the Urdini Lakes, where its slopes are steep and rocky. To the west, the slopes of the summit gently descend to the grassy folds of the Malko and Golyamo Pazardere meadows. It is built up of metamorphic rock.

Geographic entities mentioned:
surface_form: Urdini Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 42.2
lon: 23.3
There are several tourist trails accessing Damga. Through its southwestern slopes passes the summer trail the Seven Lakes refuge to the Rila Monastery. The winter trail from the Maliovitsa refuge to Ivan Vazov refuge intersects the highest point and to the north there is a trail to the Seven Rila Lakes.

Geographic entities mentioned:
surface_form: Seven Rila Lakes
instance_of: Group of lakes
countries: Bulgaria
coordinates: lat: 42.2025
lon: 23.315
During the Early Proterozoic they were covered by sediments, most of which has now been eroded away. Greenland is part of Laurentia. The island is separated from North America by the Nares Strait, but this is a Pleistocene erosional feature. The strait is floored with continental crust and shows no indications of a thermal event or seaway tectonism.

Geographic entities mentioned:
surface_form: Nares Strait
instance_of: Watercourse
countries: Greenland
Canada
coordinates: lat: 80
lon: -70
The Laramide orogeny continued to raise the present Rocky Mountains into the Paleocene. The Western Cordillera continued to suffer tectonic deformation, including the formation of the Basin and Range Province in the middle Cenozoic and the uplift of the Colorado Plateau. The Colorado Plateau was uplifted with remarkably little deformation.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
The Colorado Plateau was uplifted with remarkably little deformation. The flood basalts of the Columbia Plateau also erupted during the Cenozoic. The southwestern portion of Laurentia consists of Precambrian basement rocks deformed by continental collisions. This area has been subjected to considerable rifting as the Basin and Range Province has been stretched up to 100% of its original width.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
The Canelo Hills merge with the Huachuca Mountains to the southeast. The San Rafael Valley lies to the southwest of the range and the Patagonia Mountains lie to the west across the Harshaw Creek valley. The Canelo Hills Cienega Reserve and the ghost town of Canelo, Arizona, are located on the eastern side of the hills. Geology.

Geographic entities mentioned:
surface_form: San Rafael Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.3833
lon: -110.584
The southwest margin extending toward the Patagonias is underlain by Cretaceous–Eocene volcanics. The southern end of the Canelo Hills contain evidence for a volcanic caldera, the Parker Canyon Caldera. This caldera is mapped as a kidney shaped feature stretching from just north of Canelo Pass some to the southeast into the Huachucas and underlying the eastern portion of the San Rafael Valley.

Geographic entities mentioned:
surface_form: san rafael valley
instance_of: Valley
countries: United States
coordinates: lat: 31.3833
lon: -110.584
Canelo Hills. The Canelo Hills are a range of low mountains or hills in eastern Santa Cruz County, Arizona. The range consists of a series of northwest–southeast trending ridges extending from the Sonoita Creek valley southwest of Sonoita to the Parker Canyon Lake area in southwest Cochise County, Arizona. The Canelo Hills merge with the Huachuca Mountains to the southeast.

Geographic entities mentioned:
surface_form: canelo hills
instance_of: Landform
countries: United States
coordinates: lat: 31.5319
lon: -110.589
The Canelo Hills merge with the Huachuca Mountains to the southeast. The San Rafael Valley lies to the southwest of the range and the Patagonia Mountains lie to the west across the Harshaw Creek valley. The Canelo Hills Cienega Reserve and the ghost town of Canelo, Arizona, are located on the eastern side of the hills. Geology.

Geographic entities mentioned:
surface_form: canelo hills
instance_of: Landform
countries: United States
coordinates: lat: 31.5319
lon: -110.589
The Canelo Hills Cienega Reserve and the ghost town of Canelo, Arizona, are located on the eastern side of the hills. Geology. The Canelo Hills are underlain by northwest striking folded and faulted Permian sedimentary rocks and Jurassic–Triassic volcanic rocks. The southwest margin extending toward the Patagonias is underlain by Cretaceous–Eocene volcanics.

Geographic entities mentioned:
surface_form: canelo hills
instance_of: Landform
countries: United States
coordinates: lat: 31.5319
lon: -110.589
The southwest margin extending toward the Patagonias is underlain by Cretaceous–Eocene volcanics. The southern end of the Canelo Hills contain evidence for a volcanic caldera, the Parker Canyon Caldera. This caldera is mapped as a kidney shaped feature stretching from just north of Canelo Pass some to the southeast into the Huachucas and underlying the eastern portion of the San Rafael Valley.

Geographic entities mentioned:
surface_form: canelo hills
instance_of: Landform
countries: United States
coordinates: lat: 31.5319
lon: -110.589
Expansion and growth. Initially, the three Affiliated Colleges were located at different sites around San Francisco, but near the end of the 19th Century interest in bringing them together grew. To make this possible, San Francisco Mayor Adolph Sutro donated 13 acres in Parnassus Heights at the base of Mount Parnassus (now known as Mount Sutro).

Geographic entities mentioned:
surface_form: Mount Sutro
instance_of: Mountain
countries: United States
coordinates: lat: 37.758106
lon: -122.4571803
The two countries signed a border treaty in 1962 to resolve their un-demarcated land border. China received 40% of the disputed crater lake on Paektu Mountain (known as Changbai Mountain in China), while North Korea held the remaining land. In the 1950s and 1960s, many ethnic Koreans in Northeast China crossed the border into North Korea to escape economic hardship and famine in China.

Geographic entities mentioned:
surface_form: Paektu Mountain
instance_of: Mountain
countries: North Korea
People's Republic of China
coordinates: lat: 41.992777777778
lon: 128.07722222222
It is in the Peak District, between the towns of Macclesfield in Cheshire and Buxton in Derbyshire, and is on the administrative boundary between Derbyshire and Cheshire East. The hill is at the south end of a north-south moorland ridge, which also includes Cats Tor, high. There is also another hill named Shining Tor, above Dovedale in Derbyshire, at grid reference. Ascent.

Geographic entities mentioned:
surface_form: Dovedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.066666666667
lon: -1.7833333333333
There is also another hill named Shining Tor, above Dovedale in Derbyshire, at grid reference. Ascent. The hill offers many walking routes to the top, perhaps most commonly from the Upper Goyt Valley by Errwood reservoir, perhaps combined with a walk along the ridge north from Shining Tor over Cats Tor. It can also be gained with less climbing from the Cat and Fiddle Inn. Views.

Geographic entities mentioned:
surface_form: Upper Goyt Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.2965
lon: -1.9805
As it is the highest point around (it is some higher than the summit of Axe Edge Moor above Buxton), the views are pleasant, though the relatively flat uplands mean they are not extensive in all directions: the view to the southwest of the peak of Shutlingsloe above Wildboarclough is particularly notable, and in clear conditions Winter Hill near Bolton, the city of Manchester and much of the Cheshire Plain can be seen, including the radio telescopes at Jodrell Bank to the west.

Geographic entities mentioned:
surface_form: Shutlingsloe
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.223211111111
lon: -2.0367305555556
Carbonatite liquid compositions are significantly more alkaline than what is preserved in the fossil carbonatite rock record as composition of the melt inclusions shows. Only one carbonatite volcano is known to have erupted in historical time, the active Ol Doinyo Lengai volcano in Tanzania. It erupts with the coolest lava in the world, at.

Geographic entities mentioned:
surface_form: Ol Doinyo Lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
The magmatic origin of carbonatite was argued in detail by Swedish geologist Harry von Eckermann in 1948 based on his study of Alnö Complex. It was however the 1960 eruption of Ol Doinyo Lengai in Tanzania that led to geological investigations that finally confirmed the view that carbonatite is derived from magma. Evidence for each process exists, but the key is that these are unusual phenomena.

Geographic entities mentioned:
surface_form: Ol Doinyo Lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
Known examples. In 2017, the discovery of a new carbonatite deposit was confirmed north-west of Prince George, British Columbia, in a region termed the &quot;Rocky Mountain Rare Metal Belt&quot;. The volcano Ol Doinyo Lengai, in the East African Rift is the world's only active carbonatite volcano. Other older carbonatite volcanoes are located in the same region, including Mount Homa.

Geographic entities mentioned:
surface_form: Ol Doinyo Lengai
instance_of: Mountain
countries: Tanzania
coordinates: lat: -2.7616666666667
lon: 35.913333333333
In 2017, the discovery of a new carbonatite deposit was confirmed north-west of Prince George, British Columbia, in a region termed the &quot;Rocky Mountain Rare Metal Belt&quot;. The volcano Ol Doinyo Lengai, in the East African Rift is the world's only active carbonatite volcano. Other older carbonatite volcanoes are located in the same region, including Mount Homa. Economic importance.

Geographic entities mentioned:
surface_form: Mount Homa
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.38
lon: 34.5
Grotta dell'Addaura. The Addaura cave (Italian: Grotta dell'Addaura) is a complex of three natural grottoes located on the northeast side of Mount Pellegrino in Palermo, Sicily, Southern Italy. The importance of the complex is due to the presence of cave-wall engravings dated to the late Epigravettian (contemporaneous with the Magdalenian) and the Mesolithic.

Geographic entities mentioned:
surface_form: Mount Pellegrino
instance_of: Mountain
countries: Italy
coordinates: lat: 38.17
lon: 13.351388888889
Highway 12 was first established in early 1922 between Highway 2 in Whitby and Lindsay. The section running east from Sunderland became part of Highway 7 before route numbering was introduced in 1925. Highway 12 was then routed through Beaverton and around the eastern and northern shores of Lake Simcoe to Orillia and later to Midland; Beaverton was bypassed during the 1960s.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Blue Jacket's Crossing. Proceeding west from Independence, Missouri, the Oregon Trail kept a distance south from the incised bluffs nearer the Kansas River. However, it was unavoidable to cross the Wakarusa River and gain the crest of the hogback ridge between the Wakarusa and Kansas Rivers. Here, the Wakarusa had steep banks about 20 feet high.

Geographic entities mentioned:
surface_form: hogback ridge
instance_of: Mountain
countries: United States
coordinates: lat: 38.9631
lon: -95.2571
Long after these sedimentary rocks were deposited, the Colorado Plateau was uplifted relatively evenly, keeping the layers roughly horizontal, but Capitol Reef is an exception because of the Waterpocket Fold, a classic monocline, which formed between 50 and 70 million years ago during the Laramide Orogeny. Climate. Spring and fall are the most favorable seasons to visit Needle Mountain.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Needle Mountain. Needle Mountain is a elevation summit located in Capitol Reef National Park, in Wayne County of Utah, United States. This remote erosional remnant is situated north-northwest of the park's visitor center, and east of Cathedral Mountain, in the Middle Desert of the park's North (Cathedral Valley) District.

Geographic entities mentioned:
surface_form: cathedral mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.49303
lon: -111.36712
surface_form: cathedral mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.27498
lon: -112.95772
Cathedral Valley was so named in 1945 by Charles Kelly, first superintendent of Capitol Reef National Monument, because the valley's sandstone monoliths reminded early explorers of ornate, Gothic cathedrals, with fluted walls, alcoves, and pinnacles. The free-standing Needle Mountain towers above its surrounding terrain, which is within the Fremont River drainage basin. John C.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Needle Mountain. Needle Mountain is a elevation summit located in Capitol Reef National Park, in Wayne County of Utah, United States. This remote erosional remnant is situated north-northwest of the park's visitor center, and east of Cathedral Mountain, in the Middle Desert of the park's North (Cathedral Valley) District.

Geographic entities mentioned:
surface_form: needle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.49053
lon: -111.3549
Cathedral Valley was so named in 1945 by Charles Kelly, first superintendent of Capitol Reef National Monument, because the valley's sandstone monoliths reminded early explorers of ornate, Gothic cathedrals, with fluted walls, alcoves, and pinnacles. The free-standing Needle Mountain towers above its surrounding terrain, which is within the Fremont River drainage basin. John C.

Geographic entities mentioned:
surface_form: needle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.49053
lon: -111.3549
Geology. Needle Mountain is composed of unfractured Entrada Sandstone which was originally deposited as sandy mud on a tidal flat and is believed to have formed about 160 million years ago during the Jurassic period as a giant sand sea, the largest in Earth's history. Stratum in Cathedral Valley have a gentle inclination of three to five degrees to the east, and appear nearly horizontal.

Geographic entities mentioned:
surface_form: needle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.49053
lon: -111.3549
Climate. Spring and fall are the most favorable seasons to visit Needle Mountain. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below, and at least 50% of the total annual precipitation being received during the spring and summer.

Geographic entities mentioned:
surface_form: needle mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.49053
lon: -111.3549
The Rural Municipality of Lakeshore is a rural municipality (RM) in the Parkland Region of Manitoba, Canada. Lakeshore is named for the proximity of the shoreline of Dauphin Lake, which splits the municipality into north and south. The RM is anchored on its south end by the Rainbow Beach Provincial Park on Dauphin Lake, and on its north end by Manipogo Provincial Park on Lake Manitoba. History.

Geographic entities mentioned:
surface_form: Dauphin Lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.2696
lon: -99.7792
The Rural Municipality of Lakeshore is a rural municipality (RM) in the Parkland Region of Manitoba, Canada. Lakeshore is named for the proximity of the shoreline of Dauphin Lake, which splits the municipality into north and south. The RM is anchored on its south end by the Rainbow Beach Provincial Park on Dauphin Lake, and on its north end by Manipogo Provincial Park on Lake Manitoba. History.

Geographic entities mentioned:
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Little Jack (disambiguation). 19dtywaf2mhu8hh6hykvskd3yv1r" xml:space="preserve">Little Jack is a mountain in Washington state.

Geographic entities mentioned:
surface_form: Little Jack
instance_of: Mountain
countries: United States
coordinates: lat: 48.74388888888889
lon: -120.9786111111111
Little Temple. Little Temple is a mountain summit located in Banff National Park of the Canadian Rockies of Alberta, Canada. Little Temple is situated in the Bow River Valley between Paradise Creek and Moraine Creek, south of Lake Louise, Alberta. The mountain can be seen from the Icefields Parkway along with its nearest higher peak, Mount Temple, to the southwest. Geology.

Geographic entities mentioned:
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: little temple
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37
lon: -116.18666666666667
Little Temple. Little Temple is a mountain summit located in Banff National Park of the Canadian Rockies of Alberta, Canada. Little Temple is situated in the Bow River Valley between Paradise Creek and Moraine Creek, south of Lake Louise, Alberta. The mountain can be seen from the Icefields Parkway along with its nearest higher peak, Mount Temple, to the southwest. Geology.

Geographic entities mentioned:
surface_form: little temple
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37
lon: -116.18666666666667
Little Temple. Little Temple is a mountain summit located in Banff National Park of the Canadian Rockies of Alberta, Canada. Little Temple is situated in the Bow River Valley between Paradise Creek and Moraine Creek, south of Lake Louise, Alberta. The mountain can be seen from the Icefields Parkway along with its nearest higher peak, Mount Temple, to the southwest. Geology.

Geographic entities mentioned:
surface_form: little temple
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37
lon: -116.18666666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain can be seen from the Icefields Parkway along with its nearest higher peak, Mount Temple, to the southwest. Geology. Like other mountains in Banff Park, Little Temple is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: little temple
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37
lon: -116.18666666666667
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Little Temple is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: little temple
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37
lon: -116.18666666666667
Climate. Based on the Köppen climate classification, Little Temple is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Little Temple drains into the Bow River which is a tributary of the Saskatchewan River.

Geographic entities mentioned:
surface_form: little temple
instance_of: Mountain
countries: Canada
coordinates: lat: 51.37
lon: -116.18666666666667
Little Temple. Little Temple is a mountain summit located in Banff National Park of the Canadian Rockies of Alberta, Canada. Little Temple is situated in the Bow River Valley between Paradise Creek and Moraine Creek, south of Lake Louise, Alberta. The mountain can be seen from the Icefields Parkway along with its nearest higher peak, Mount Temple, to the southwest. Geology.

Geographic entities mentioned:
surface_form: mount temple
instance_of: Mountain
countries: Canada
coordinates: lat: 51.35055555555556
lon: -116.20666666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Miller announced in May 2004 that Toronto would install over 2,000 energy-efficient traffic signal lights. He also endorsed the Deep lake water cooling project, in which water from Lake Ontario is used to cool office buildings in downtown Toronto. In early 2005, he and Chicago Mayor Richard M. Daley made a joint address to the Great Lakes Congressional Breakfast in Washington, D.C.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Saalfelden Basin. To the south the basin is generally open, running into the Zell Basin (&quot;Zeller Becken&quot;) with Lake Zell and the Salzach river – hence the term Zell-Saalfelden Basin &quot;Zeller-Saalfeldener Becken&quot; is also used for the whole valley – and enables a view of the High Tauern, especially the prominent Kitzsteinhorn and Wiesbachhorn peaks.

Geographic entities mentioned:
surface_form: Lake Zell
instance_of: Lake
countries: Austria
coordinates: lat: 47.316666666667
lon: 12.8
surface_form: Kitzsteinhorn
instance_of: Mountain
countries: Austria
coordinates: lat: 47.188055555556
lon: 12.6875
This trough is one of the largest inner-Alpine basins. The main river in the basin is the Saalach. It rises in the upper Glemm Valley, empties into the basin south of Saalfelden and passes through it from south to north. A right tributary of the Saalach flowing through the borough of Saalfelden from east to west is the Urslau creek.

Geographic entities mentioned:
surface_form: Glemm Valley
instance_of: Valley
countries: Austria
coordinates: lat: 47.3833
lon: 12.6333
Lake Lagunillas. Lake Lagunillas is a lake in the Andes of far southeastern Peru. Lagunillas is at an altitude of about and it is located just northwest of Lake Saracocha. These two lakes are part of the system drained by the Coata River, which flows in a generally easterly direction until entering westernmost Lake Titicaca, about from Lake Lagunillas as the crow flies.

Geographic entities mentioned:
surface_form: Lake Saracocha
instance_of: Lake
countries: Peru
coordinates: lat: -15.781111111111
lon: -70.622222222222
surface_form: saracocha
instance_of: Lake
countries: Peru
coordinates: lat: -15.781111111111
lon: -70.622222222222
Lake Lagunillas. Lake Lagunillas is a lake in the Andes of far southeastern Peru. Lagunillas is at an altitude of about and it is located just northwest of Lake Saracocha. These two lakes are part of the system drained by the Coata River, which flows in a generally easterly direction until entering westernmost Lake Titicaca, about from Lake Lagunillas as the crow flies.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
surface_form: lake lagunillas
instance_of: Lake
countries: Peru
coordinates: lat: -15.725
lon: -70.735555555556
Lake Lagunillas. Lake Lagunillas is a lake in the Andes of far southeastern Peru. Lagunillas is at an altitude of about and it is located just northwest of Lake Saracocha. These two lakes are part of the system drained by the Coata River, which flows in a generally easterly direction until entering westernmost Lake Titicaca, about from Lake Lagunillas as the crow flies.

Geographic entities mentioned:
surface_form: lake lagunillas
instance_of: Lake
countries: Peru
coordinates: lat: -15.725
lon: -70.735555555556
The mountain is named after Thomas Jefferson, the third president of the United States, and is part of the Presidential Range of the White Mountains. Mount Jefferson is flanked by Mount Adams (to the northeast) and Mount Clay (to the south). The mountain has several interesting features, making it a popular hike. Two distinct ridges lead to its summit: Ridge of the Caps and Castle Ridge.

Geographic entities mentioned:
surface_form: Mount Clay
instance_of: Mountain
countries: United States
coordinates: lat: 44.285166666667
lon: -71.315833333333
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.3522
lon: -68.2828
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4584
lon: -74.6196
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 44.0867
lon: -74.0258
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.752
lon: -116.927
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.0328
lon: -78.5222
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 38.0075
lon: -105.605
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.3042
lon: -71.3168
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 44.320555555556
lon: -71.291388888889
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4918
lon: -72.0395
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.6028
lon: -112.006
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 36.403055555556
lon: -81.463333333333
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
surface_form: mount adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.562
lon: -111.505
Mount Jefferson (New Hampshire). Mount Jefferson is located in Coos County, New Hampshire, and is the third highest mountain in the state. The mountain is named after Thomas Jefferson, the third president of the United States, and is part of the Presidential Range of the White Mountains. Mount Jefferson is flanked by Mount Adams (to the northeast) and Mount Clay (to the south).

Geographic entities mentioned:
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.3522
lon: -68.2828
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4584
lon: -74.6196
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.752
lon: -116.927
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.0328
lon: -78.5222
surface_form: mount jefferson (new hampshire)
instance_of: Mountain
countries: United States
coordinates: lat: 44.3042
lon: -71.3168
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4918
lon: -72.0395
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.6028
lon: -112.006
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 36.403055555556
lon: -81.463333333333
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.562
lon: -111.505
Mount Jefferson (New Hampshire). Mount Jefferson is located in Coos County, New Hampshire, and is the third highest mountain in the state. The mountain is named after Thomas Jefferson, the third president of the United States, and is part of the Presidential Range of the White Mountains. Mount Jefferson is flanked by Mount Adams (to the northeast) and Mount Clay (to the south).

Geographic entities mentioned:
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.3522
lon: -68.2828
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4584
lon: -74.6196
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.752
lon: -116.927
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.0328
lon: -78.5222
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.3042
lon: -71.3168
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4918
lon: -72.0395
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.6028
lon: -112.006
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 36.403055555556
lon: -81.463333333333
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.562
lon: -111.505
Finally, Monticello Lawn is a large expanse of alpine sedge and rush near the otherwise talus-covered summit cone. When viewed from the Mount Washington Auto Road, Jefferson features an arrow-shaped bald patch pointing to its summit. Mount Jefferson has a direct ascent along the Caps Ridge Trail, whose base, Jefferson Notch, is the highest point of any public road in New Hampshire at.

Geographic entities mentioned:
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.3522
lon: -68.2828
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4584
lon: -74.6196
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.752
lon: -116.927
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 38.0328
lon: -78.5222
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.3042
lon: -71.3168
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 42.4918
lon: -72.0395
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 45.6028
lon: -112.006
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 36.403055555556
lon: -81.463333333333
surface_form: mount jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.562
lon: -111.505
Mount Jefferson (New Hampshire). Mount Jefferson is located in Coos County, New Hampshire, and is the third highest mountain in the state. The mountain is named after Thomas Jefferson, the third president of the United States, and is part of the Presidential Range of the White Mountains. Mount Jefferson is flanked by Mount Adams (to the northeast) and Mount Clay (to the south).

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
The mountain has several interesting features, making it a popular hike. Two distinct ridges lead to its summit: Ridge of the Caps and Castle Ridge. The mountain is surrounded by the three dramatic glacial cirques of Jefferson Ravine, Castle Ravine, and the Great Gulf. Finally, Monticello Lawn is a large expanse of alpine sedge and rush near the otherwise talus-covered summit cone.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611