Sarmila/GeoWiki-Features huggingface dataset:
Nahta Cone. Nahta Cone is a small cinder cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and lies near the northern edge of the Arctic Lake Plateau, a glacially scored plateau of the Tahltan Highland which in turn extends along the western side of the Stikine Plateau.

Geographic entities mentioned:
surface_form: Arctic Lake Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
The cone is about south-southeast of the community of Telegraph Creek and lies in the southwestern corner of Mount Edziza Provincial Park, one of the largest provincial parks in British Columbia. Nahta Cone is a part of the Mount Edziza volcanic complex and overlies a limestone hill.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Access to this isolated volcanic cone is limited to float plane or helicopter. Geography. Nahta Cone is located in Cassiar Land District of northwestern British Columbia, Canada, near the northern edge of the Arctic Lake Plateau. It has an elevation of and rises about above the glacially scored surface of the plateau to a circular crater breached on the east.

Geographic entities mentioned:
surface_form: Arctic Lake Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
It has an elevation of and rises about above the glacially scored surface of the plateau to a circular crater breached on the east. The cone is surrounded by Mess Creek valley to the west, Wetalth Ridge and Little Arctic Lake to the east, Tadekho Hill to the northeast, Exile Hill to the north and Arctic Lake to the south.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: Wetalth Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.2275
lon: -130.786
surface_form: Tadekho Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
surface_form: Exile Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
With an area of, Mount Edziza Provincial Park is one of the largest provincial parks in British Columbia and was established in 1972 to showcase the volcanic landscape. It also includes the Spectrum Range to the northeast and Mount Edziza further to the north which are separated by the broad east–west valley of Raspberry Pass.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
It also includes the Spectrum Range to the northeast and Mount Edziza further to the north which are separated by the broad east–west valley of Raspberry Pass. Mount Edziza Provincial Park is in the Tahltan Highland, a southeast-trending upland area extending along the western side of the Stikine Plateau. Geology.

Geographic entities mentioned:
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Mount Edziza Provincial Park is in the Tahltan Highland, a southeast-trending upland area extending along the western side of the Stikine Plateau. Geology. Nahta Cone is the southernmost cinder cone of the Big Raven Formation, the youngest and least voluminous geological formation of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Five tiny hawaiite conelets consisting of black and brick-red scoria blocks comprise Nahta Cone; the hawaiite contains phenocrysts of olivine and plagioclase. Nahta Cone is somewhat older than The Ash Pit in the Mess Lake Lava Field which may be the youngest cinder cone of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: The Ash Pit
instance_of: Mountain
countries: Canada
coordinates: lat: 57.45
lon: -130.78
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mess lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
It means in the Tahltan language, referring to the last seven survivors of the Wetalth people who were outcasted or exiled from the Tahltans in times past. Several other features on the Arctic Lake Plateau such as Wetalth Ridge, Outcast Hill, Exile Hill and Tadekho Hill also have names with Tahltan roots that were adopted on January 2, 1980.

Geographic entities mentioned:
surface_form: Outcast Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.39
lon: -130.774
surface_form: wetalth ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.2275
lon: -130.786
surface_form: arctic lake plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
surface_form: exile hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3783
lon: -130.825
surface_form: tadekho hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
The cone is surrounded by Mess Creek valley to the west, Wetalth Ridge and Little Arctic Lake to the east, Tadekho Hill to the northeast, Exile Hill to the north and Arctic Lake to the south. Between Nahta Cone and Tadekho Hill is Nahta Creek which flows west through a valley into Mess Creek, a northwest-flowing tributary of the Stikine River.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: tadekho hill
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3503
lon: -130.785
Nahta Cone. Nahta Cone is a small cinder cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and lies near the northern edge of the Arctic Lake Plateau, a glacially scored plateau of the Tahltan Highland which in turn extends along the western side of the Stikine Plateau.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: cinder cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9717
lon: -123.007
It has an elevation of and lies near the northern edge of the Arctic Lake Plateau, a glacially scored plateau of the Tahltan Highland which in turn extends along the western side of the Stikine Plateau. The cone is about south-southeast of the community of Telegraph Creek and lies in the southwestern corner of Mount Edziza Provincial Park, one of the largest provincial parks in British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Nahta Cone lies in the southwestern corner of Mount Edziza Provincial Park about south-southeast of the community of Telegraph Creek. With an area of, Mount Edziza Provincial Park is one of the largest provincial parks in British Columbia and was established in 1972 to showcase the volcanic landscape.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Several other features on the Arctic Lake Plateau such as Wetalth Ridge, Outcast Hill, Exile Hill and Tadekho Hill also have names with Tahltan roots that were adopted on January 2, 1980. In his 1992 report &quot;The Late Cenozoic Mount Edziza Volcanic Complex, British Columbia&quot;, Jack Souther gave Nahta Cone the numeronym &quot;AL-1&quot;. Accessibility.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Nahta Cone. Nahta Cone is a small cinder cone in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of and lies near the northern edge of the Arctic Lake Plateau, a glacially scored plateau of the Tahltan Highland which in turn extends along the western side of the Stikine Plateau.

Geographic entities mentioned:
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
Between Nahta Cone and Tadekho Hill is Nahta Creek which flows west through a valley into Mess Creek, a northwest-flowing tributary of the Stikine River. Nahta Cone lies in the southwestern corner of Mount Edziza Provincial Park about south-southeast of the community of Telegraph Creek.

Geographic entities mentioned:
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Five tiny hawaiite conelets consisting of black and brick-red scoria blocks comprise Nahta Cone; the hawaiite contains phenocrysts of olivine and plagioclase. Nahta Cone is somewhat older than The Ash Pit in the Mess Lake Lava Field which may be the youngest cinder cone of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
Nahta Cone is somewhat older than The Ash Pit in the Mess Lake Lava Field which may be the youngest cinder cone of the Mount Edziza volcanic complex. Nahta Cone was the source of air-fall tephra and a roughly long lava flow which extends northerly and then westerly into the head of Nahta Creek.

Geographic entities mentioned:
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
Accessibility. Nahta Cone can be accessed by float plane or helicopter, both of which are available for charter at the communities of Iskut and Dease Lake. Arctic Lake about south of Natha Cone and Little Arctic Lake about east of Nahta Cone are large enough to be used by float-equipped aircraft.

Geographic entities mentioned:
surface_form: nahta cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3083
lon: -130.821
Accessibility. Nahta Cone can be accessed by float plane or helicopter, both of which are available for charter at the communities of Iskut and Dease Lake. Arctic Lake about south of Natha Cone and Little Arctic Lake about east of Nahta Cone are large enough to be used by float-equipped aircraft.

Geographic entities mentioned:
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
It is situated on the German Wine Route, approx. 5 km south of Neustadt an der Weinstraße. Maikammer is the seat of the &quot;Verbandsgemeinde&quot; Maikammer. Location. Maikammer lies at elevations from 120 to 300 m at the foot of the Kalmit, the highest mountain in the Palatine Forest (673 m), in a landscape dominated by vineyards.

Geographic entities mentioned:
surface_form: Kalmit
instance_of: Mountain
countries: Germany
coordinates: lat: 49.318888888889
lon: 8.0827777777778
The name appears as a competitor with the names of the lagoons of Manguaba, (&quot;the southern lagoon&quot;), and Mundaú, (&quot;the northern lagoon&quot;), already in the 16th century, when settlements were founded near the Alagoa do Norte and the Alagoa do Sul, the Alagoas, with the inclusion of the rest of the lagoons in the area. The suffix is characteristic of Brazil:,,, and later.

Geographic entities mentioned:
surface_form: Manguaba
instance_of: Lake
countries: Brazil
coordinates: lat: -9.68333
lon: -35.9
surface_form: Mundaú
instance_of: Lake
countries: Brazil
coordinates: lat: -9.63333
lon: -35.78333
Personal life. Lemann married twice and has six children, three with his first wife and three with his second wife Susanna. He usually shares his time between São Paulo, Rapperswil-Jona on Lake Zurich, where his family lives, and St. Louis, Missouri. In 1994, he suffered a heart attack at age 54. In 1999, several gunmen attempted to kidnap his children on their way to school.

Geographic entities mentioned:
surface_form: Lake Zurich
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2475
lon: 8.6775
or 4,160 m) is a mountain range of the Pennine Alps with its highest peak of the same name (but also called &quot;Breithorn (Western Summit)&quot;), located on the border between Switzerland and Italy. It lies on the main chain of the Alps, approximately halfway between the Matterhorn and Monte Rosa and east of the Theodul Pass.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
It lies on the main chain of the Alps, approximately halfway between the Matterhorn and Monte Rosa and east of the Theodul Pass. Most of the massif is glaciated and includes several subsidiary peaks, all located east of the main summit: the Central Breithorn, the western Breithorn Twin (or Eastern Breithorn), the Gendarm (or eastern Breithorn Twin) and the Roccia Nera.

Geographic entities mentioned:
surface_form: Central Breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.93888889
lon: 7.75638889
surface_form: western Breithorn Twin (or Eastern Breithorn)
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.93722222
lon: 7.76722222
surface_form: Roccia Nera
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.9325
lon: 7.77527778
surface_form: central breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.93888889
lon: 7.75638889
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
surface_form: eastern breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.93722222
lon: 7.76722222
surface_form: eastern breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.93722222
lon: 7.76722222
surface_form: roccia nera
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.9325
lon: 7.77527778
The Breithorn is considered the most easily climbed 4,000 m Alpine peak. This is due to the Klein Matterhorn cable car which takes climbers to over 3,820 m (12,700 ft) from Zermatt for a starting point. The standard route (SSW flank) is from the Italian side of the mountain (the south side) and continues over a glacial plateau before climbing to the summit on a 35 degree snow slope.

Geographic entities mentioned:
surface_form: Klein Matterhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.938333333333
lon: 7.7297222222222
Breithorn. The Breithorn (German for literally &quot;broad horn&quot;; 13,661 ft. or 4,160 m) is a mountain range of the Pennine Alps with its highest peak of the same name (but also called &quot;Breithorn (Western Summit)&quot;), located on the border between Switzerland and Italy.

Geographic entities mentioned:
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
Most of the massif is glaciated and includes several subsidiary peaks, all located east of the main summit: the Central Breithorn, the western Breithorn Twin (or Eastern Breithorn), the Gendarm (or eastern Breithorn Twin) and the Roccia Nera. The main summit is sometimes distinguished by the name &quot;Western Breithorn&quot; (,).

Geographic entities mentioned:
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
However, inexperienced mountaineers may run into severe difficulty if caution is not taken near cornices or in bad weather. For experienced climbers wanting more of a challenge, the half traverse of the Breithorn crest is another option. The Breithorn was first climbed in 1813 by Henry Maynard (climber), Joseph-Marie Couttet, Jean Gras, Jean-Baptiste Erin and Jean-Jacques Erin.

Geographic entities mentioned:
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
surface_form: breithorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.941111111111
lon: 7.7472222222222
Pedu Lake. Pedu Lake (Malay: &quot;Tasik Pedu&quot;) is a man-made lake located in Padang Terap District, Kedah, Malaysia. It covers an area of 75 km².

Geographic entities mentioned:
surface_form: pedu
instance_of: Lake
countries: Malaysia
coordinates: lat: 6.2471083333333
lon: 100.81295
Pedu Lake. Pedu Lake (Malay: &quot;Tasik Pedu&quot;) is a man-made lake located in Padang Terap District, Kedah, Malaysia. It covers an area of 75 km².

Geographic entities mentioned:
surface_form: pedu
instance_of: Lake
countries: Malaysia
coordinates: lat: 6.2471083333333
lon: 100.81295
surface_form: tasik pedu
instance_of: Lake
countries: Malaysia
coordinates: lat: 6.2471083333333
lon: 100.81295
surface_form: pedu
instance_of: Lake
countries: Malaysia
coordinates: lat: 6.2471083333333
lon: 100.81295
Architecture. The only substantial remains of very early viharas are in the rock-cut complexes, mostly in north India, the Deccan in particular, but this is an accident of survival. Originally structural viharas of stone or brick would probably have been at least as common everywhere, and the norm in the south.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
At the time of his death the firm had in all about eighty such depots on the shipping routes to India, China, South Africa, and South America. About 1868 the firm had acquired its first colliery, that of Pentre, Rhondda, to which others in the same valley, and in the Ogmore and Neath valleys, were later added. Large colliery interests were also acquired elsewhere.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
In 1914 his fortune was estimated at 30 million marks. In 1897 he joined the Society of Friends. In 1882 he married Ida Brandeis-Weikersheim (1860–1912), a daughter of the Viennese wholesaler, banker and British consul Salomon Brandeis-Weikersheim (1813–1877) in Vienna. Huldschinsky had a villa built on the Großer Wannsee in 1890/1891, which at that time had the address Friedrich-Karl-Straße 19.

Geographic entities mentioned:
surface_form: Großer Wannsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.4275
lon: 13.173055555556
Many buildings survive from the Dutch and British period of occupation. Cave temples. The earliest evidence of cave temples is found in the temple complexes of Mihintale. A unique feature in these caves was the use of a drip ledge carved along the top edge of the rock ceiling which stopped rainwater running into the cave. With time, doors, windows and walls of brick or stone were added.

Geographic entities mentioned:
surface_form: Mihintale
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 8.350594
lon: 80.516945
Moe Pond. Moe Pond is a small man-made lake in Otsego County, New York, located north-west of Cooperstown. Moe Pond drains south via Willow Brook, which flows into Otsego Lake. Mount Ovis is located east and Hannah's Hill is located southeast of Moe Pond. The pond was named for Henry Allen Moe, a past member of the New York State Historical Association. Moe Pond was created in 1939.

Geographic entities mentioned:
surface_form: Mount Ovis
instance_of: Mountain
countries: United States
coordinates: lat: 42.718138
lon: -74.939117
surface_form: Hannah's Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.707164
lon: -74.934783
surface_form: moe pond
instance_of: Lake
countries: United States
coordinates: lat: 42.717662
lon: -74.945119
Moe Pond. Moe Pond is a small man-made lake in Otsego County, New York, located north-west of Cooperstown. Moe Pond drains south via Willow Brook, which flows into Otsego Lake. Mount Ovis is located east and Hannah's Hill is located southeast of Moe Pond. The pond was named for Henry Allen Moe, a past member of the New York State Historical Association. Moe Pond was created in 1939.

Geographic entities mentioned:
surface_form: moe pond
instance_of: Lake
countries: United States
coordinates: lat: 42.717662
lon: -74.945119
Mount Ovis is located east and Hannah's Hill is located southeast of Moe Pond. The pond was named for Henry Allen Moe, a past member of the New York State Historical Association. Moe Pond was created in 1939. The pond and surrounding area is currently privately owned by the State University of New York at Oneonta (SUNY Oneonta), which uses it for educational and research purposes only.

Geographic entities mentioned:
surface_form: moe pond
instance_of: Lake
countries: United States
coordinates: lat: 42.717662
lon: -74.945119
Situ Gintung. Situ Gintung (Sundanese, &quot;Lake Gintung&quot;) is an artificial lake near to the town of Cirendeu (pronounced) in the city of South Tangerang, Indonesia. It was formed by a dam up to high which was built by Dutch colonial authorities in 1933. The dam failed on 27 March 2009, draining the lake, with resulting floods killing at least 100 people. History.

Geographic entities mentioned:
surface_form: situ gintung
instance_of: Lake
countries: Indonesia
coordinates: lat: -6.3053
lon: 106.7622
The creek's corridor extends across the Aboriginal Land Councils of Deerubbin and Gandangara. From northwest to southeast, the creek crosses roads such as Prospect Highway, Gipps Road, Cumberland Highway, Fairfield Road, The Horsley Drive, Fairfield Street, Vine Street, Hume Highway and then meanders parallel of Henry Lawson Drive as it heads south to Chipping Norton Lake (Dhurawal Bay).

Geographic entities mentioned:
surface_form: Chipping Norton Lake
instance_of: Lake
countries: Australia
coordinates: lat: -33.90301
lon: 150.95831
The summit is a broad, rounded detrital ridge, with its highest point marked by a metal cross placed by the Savigliano section of the CAI in 2014. From the summit, there is a close and detailed view of the western slope of the Monviso group, with particular prominence given to the, the Visolotto, the Punta Gastaldi, and the ridge descending from the Monviso summit to the Punta Caprera.

Geographic entities mentioned:
surface_form: Visolotto
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6757451
lon: 7.0853457
surface_form: Punta Gastaldi
instance_of: Mountain
countries: Italy
France
coordinates: lat: 44.6808
lon: 7.07639
Punta Tre Chiosis. The Punta Tre Chiosis (3,080 m) is a mountain in the Cottian Alps, located in the commune of Pontechianale in the upper Valle Varaita. Characteristics. It is entirely within the municipal territory of Pontechianale, on the ridge that separates the Vallone di Vallanta to the east from the Valle Varaita di Chianale to the west.

Geographic entities mentioned:
surface_form: valle varaita
instance_of: Valley
countries: Italy
coordinates: lat: 44.58
lon: 7.1
surface_form: punta tre chiosis
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6611
lon: 7.04806
The Punta Tre Chiosis (3,080 m) is a mountain in the Cottian Alps, located in the commune of Pontechianale in the upper Valle Varaita. Characteristics. It is entirely within the municipal territory of Pontechianale, on the ridge that separates the Vallone di Vallanta to the east from the Valle Varaita di Chianale to the west. The ridge branches off from the main Alpine watershed at the.

Geographic entities mentioned:
surface_form: valle varaita
instance_of: Valley
countries: Italy
coordinates: lat: 44.58
lon: 7.1
Punta Tre Chiosis. The Punta Tre Chiosis (3,080 m) is a mountain in the Cottian Alps, located in the commune of Pontechianale in the upper Valle Varaita. Characteristics. It is entirely within the municipal territory of Pontechianale, on the ridge that separates the Vallone di Vallanta to the east from the Valle Varaita di Chianale to the west.

Geographic entities mentioned:
surface_form: punta tre chiosis
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6611
lon: 7.04806
Here, it turns sharply south, forms a wide arc with concavity to the west, and, with a general south-southwest direction, reaches the summit of Punta Tre Chiosis at 3,080 m, the highest point of the Vallanta-Chianale ridge.

Geographic entities mentioned:
surface_form: punta tre chiosis
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6611
lon: 7.04806
T'uru Pampa. T'uru Pampa (Quechua for polished, slippery, also spelled &quot;Thuru Pampa&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Chuquisaca Department, Azurduy Province, Tarvita Municipality. T'uru Pampa lies at the Rumi Jich'asqa River, southwest of Llusk'a.

Geographic entities mentioned:
surface_form: Llusk'a
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.7627
lon: -64.5908
surface_form: llusk'a
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.7627
lon: -64.5908
T'uru Pampa. T'uru Pampa (Quechua for polished, slippery, also spelled &quot;Thuru Pampa&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Chuquisaca Department, Azurduy Province, Tarvita Municipality. T'uru Pampa lies at the Rumi Jich'asqa River, southwest of Llusk'a.

Geographic entities mentioned:
surface_form: t'uru pampa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.77972222
lon: -64.61666667
T'uru Pampa. T'uru Pampa (Quechua for polished, slippery, also spelled &quot;Thuru Pampa&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Chuquisaca Department, Azurduy Province, Tarvita Municipality. T'uru Pampa lies at the Rumi Jich'asqa River, southwest of Llusk'a.

Geographic entities mentioned:
surface_form: t'uru pampa
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.77972222
lon: -64.61666667
surface_form: thuru
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.9628
lon: -66.4364
Especially the widespread convergent evolution seen in anoles living in the Greater Antilles has attracted the attention of scientists, and resulted in comparisons with the Darwin's finches of the Galápagos Islands, lemurs of Madagascar and cichlid fish in the African Great Lakes. Ecomorphs and origin.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
In others with few records, like the Neblina anole, this is not the case. It was initially known from six 1980s specimens from the remote Neblina highlands in Venezuela, but when the Brazilian part of these highlands were visited in 2017 it was discovered that the species was locally abundant. Some species are easily overlooked, even if common.

Geographic entities mentioned:
surface_form: Neblina highlands
instance_of: Mountain
countries: Brazil
Venezuela
coordinates: lat: 0.88638889
lon: -65.98944444
Eulachon was probably the most important non-salmonid resource fished. Eulachon oil was an important trade item. There was a major aboriginal trail, or grease trail, linking the lower Skeena River and Douglas Channel. It ran through the Ecstall Valley, along the river, by Ecstall Lake, over a pass to the Quaal River valley, and down that river to the Kitkiata Inlet of Douglas Channel.

Geographic entities mentioned:
surface_form: Douglas Channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.666666666667
lon: -129.13333333333
surface_form: douglas channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.666666666667
lon: -129.13333333333
Ecstall River. The Ecstall River is a tributary of the Skeena River in the province of British Columbia, Canada. It originates in the Kitimat Ranges, and flows about to the lower tidal reach of the Skeena River at Port Essington, about southeast of Prince Rupert, southwest of Terrace, and northwest of Kitimat.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
Its drainage basin covers about and contains the largest blocks of unlogged land on the north coast of British Columbia, although large-scale industrial logging operations, both active and proposed, have been occurring in the watershed since the 1980s. The name &quot;Ecstall&quot; comes from a Tsimshian word meaning &quot;something from the side&quot; or &quot;a tributary&quot;.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The floodplains and alluvial areas support large spruce, hemlock, and deciduous trees, with an understory consisting principally of salmonberry, ferns, and devil's club. The floodplain above Muddy Creek is one of the richest and most diverse ecosystems on the northern coast of British Columbia. Industrial logging in the Ecstall River's valley began in the 1980s.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Eulachon oil was an important trade item. There was a major aboriginal trail, or grease trail, linking the lower Skeena River and Douglas Channel. It ran through the Ecstall Valley, along the river, by Ecstall Lake, over a pass to the Quaal River valley, and down that river to the Kitkiata Inlet of Douglas Channel. There are two hydroelectric projects in the Ecstall River's watershed.

Geographic entities mentioned:
surface_form: douglas channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.666666666667
lon: -129.13333333333
Turning north the river flows along the east edge of the Ecstall-Sparkling Conservancy and the Ecstall-Spoksuut Conservancy. More tributaries join the Ecstall as it flows north, including Johnston Creek, Red Gulch Creek, Sparkling Creek, Muddy Creek, Big Falls Creek, Madeline Creek, McKnight Creek, Hayward Creek, Cuthbert Creek, and McDonald Creek.

Geographic entities mentioned:
surface_form: johnston creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.2458
lon: -115.841
Ecstall River. The Ecstall River is a tributary of the Skeena River in the province of British Columbia, Canada. It originates in the Kitimat Ranges, and flows about to the lower tidal reach of the Skeena River at Port Essington, about southeast of Prince Rupert, southwest of Terrace, and northwest of Kitimat.

Geographic entities mentioned:
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
It ran through the Ecstall Valley, along the river, by Ecstall Lake, over a pass to the Quaal River valley, and down that river to the Kitkiata Inlet of Douglas Channel. There are two hydroelectric projects in the Ecstall River's watershed. The Falls River Project was built in the 1930s and acquired by BC Hydro in 1964.

Geographic entities mentioned:
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
There are two hydroelectric projects in the Ecstall River's watershed. The Falls River Project was built in the 1930s and acquired by BC Hydro in 1964. It consists of a dam, two penstocks, a 7 MW nominal power plant, and of transmission line running along the east side of the Ecstall River, across the Skeena River, and on to Prince Rupert.

Geographic entities mentioned:
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
It consists of a dam near the outlet of Brown Lake and a tunnel to a powerhouse near sea level, which generates 7.2 MW. Electricity is delivered to the BC Hydro power grid via a submarine cable and a connection to the transmission line on the east side of the Ecstall River. Course.

Geographic entities mentioned:
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
The river flows east, then south through the Ecstall Headwaters Conservancy, then bends sharply to the north and northwest, reaching the Skeena River at Port Essington, near the mouth of the Skeena. Ecstall Island is located at the mouth of the Ecstall River, just east of Port Essington.

Geographic entities mentioned:
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
More tributaries join the Ecstall as it flows north, including Johnston Creek, Red Gulch Creek, Sparkling Creek, Muddy Creek, Big Falls Creek, Madeline Creek, McKnight Creek, Hayward Creek, Cuthbert Creek, and McDonald Creek. High peaks near the Ecstall River include Spokshute Mountain, Mount Morrison, Balmoral Peak, Cunningham Peak, Mount Dodge, and Mount Hayward, among many others.

Geographic entities mentioned:
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
surface_form: mount morrison
instance_of: Mountain
countries: Canada
coordinates: lat: 50.83777777777778
lon: -115.47916666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Ecstall River flows through the Indian reserves of Iakvas 68 and Knokmolks 67, of the Tsimshian Lax-kw'alaams First Nation. The Port Essington Indian Reserve, of the Tsimshian Kitsumkalum and Kitselas people, is located near the mouth of the Ecstall River. Natural history.

Geographic entities mentioned:
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
It supports many species of salmonids, including sockeye salmon, coho salmon, chum salmon, Chinook salmon, pink salmon, steelhead trout, rainbow trout, Dolly Varden trout, mountain whitefish, and bull trout. Eulachon, which historically were harvested by Tsimshian people and traded via grease trails, spawn in the tidal portion of the Ecstall River.

Geographic entities mentioned:
surface_form: ecstall river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.15836
lon: -129.94543
The forests of the Ecstall watershed's valley bottoms and slopes up to about are dominated by old growth western hemlock, western red cedar, Sitka spruce, and amabilis fir. Higher elevations are dominated by mountain hemlock and amabilis fir, some spruce, red cedar, and yellow cedar, with an understory mostly composed of Alaska blueberry, false azalea, red huckleberry, and black huckleberry.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: cedar
instance_of: Lake
countries: Canada
coordinates: lat: 53.366666666667
lon: -100
surface_form: cedar
instance_of: Lake
countries: Canada
coordinates: lat: 53.366666666667
lon: -100
The Ecstall River is an important salmon spawning stream. It supports many species of salmonids, including sockeye salmon, coho salmon, chum salmon, Chinook salmon, pink salmon, steelhead trout, rainbow trout, Dolly Varden trout, mountain whitefish, and bull trout.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Port Essington Indian Reserve, of the Tsimshian Kitsumkalum and Kitselas people, is located near the mouth of the Ecstall River. Natural history. The forests of the Ecstall watershed's valley bottoms and slopes up to about are dominated by old growth western hemlock, western red cedar, Sitka spruce, and amabilis fir.

Geographic entities mentioned:
surface_form: cedar
instance_of: Lake
countries: Canada
coordinates: lat: 53.366666666667
lon: -100
São Caetano de Odivelas. São Caetano de Odivelas is a municipality in the state of Pará in the Northern region of Brazil. The municipal seat lies on the left (west) bank of the Barreto River. It contains the Mocapajuba Marine Extractive Reserve, created in 2014.

Geographic entities mentioned:
surface_form: Barreto River
instance_of: Watercourse
countries: Peru
coordinates: lat: -0.702146
lon: -47.995763
Neolamprologus caudopunctatus. &quot;Neolamprologus caudopunctatus&quot; is a species of cichlid endemic to Lake Tanganyika, where it occurs along the Zambian shores. It has a silvery-beige colored body, accented only by a distinctive, goldish-orange dorsal fin and blue eyes. Its tail fin and flanks have pearly spots that are visible if the light hits them at the correct angle.

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 town's history includes evidence of ancient settlements, including the village of Rabat. Artifacts from the Iberian, Roman, Arab, and Christian periods have been discovered. Rafelcofer offers various cultural and natural attractions, including a local museum, El Rabat, and the Mountain of Sant Miquel, as well as various dykes and mills, some dating back to 1849 with Islamic origins.

Geographic entities mentioned:
surface_form: Mountain of Sant Miquel
instance_of: Mountain
countries: Spain
coordinates: lat: 41.923121729
lon: 2.53302886771
The Cornet. The Cornet is a peak on the south side of Pardo Ridge between Muckle Bluff and The Stadium. Located on Elephant Island in the South Shetland Islands of Antarctica, it was named descriptively for its conical shape by the UK Joint Services Expedition, 1970-71.

Geographic entities mentioned:
surface_form: Pardo Ridge
instance_of: Mountain
coordinates: lat: -61.125
lon: -54.883333333333
surface_form: the cornet
instance_of: Mountain
coordinates: lat: -61.1167
lon: -54.7833
The Cornet. The Cornet is a peak on the south side of Pardo Ridge between Muckle Bluff and The Stadium. Located on Elephant Island in the South Shetland Islands of Antarctica, it was named descriptively for its conical shape by the UK Joint Services Expedition, 1970-71.

Geographic entities mentioned:
surface_form: the cornet
instance_of: Mountain
coordinates: lat: -61.1167
lon: -54.7833
Trails at night are normally not as busy as during the day, but there are usually fewer runs available. The trails also tend to be icier than during the day, due to melting and refreezing. Starting in 1997 Planai in Austria has held a World Cup slalom competition at night. A few ski resorts offer opportunities for night skiing wearing personal headlamps, or by the light of the full moon. History.

Geographic entities mentioned:
surface_form: Planai
instance_of: Mountain
countries: Austria
coordinates: lat: 47.392
lon: 13.694
Lava Fork. Lava Fork is a creek in northwestern British Columbia, Canada and the Alaska Panhandle, United States. It lies west of the Unuk River and northwest of Stewart. It flows south from the Lava Lakes across the British Columbia-Alaska border into the Blue River in the extreme northern part of Misty Fjords National Monument.

Geographic entities mentioned:
surface_form: Lava Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 56.4333
lon: -130.9
Its highest peak is Teram Kangri I, 7,462 metres (24,482 feet). Selected peaks of the Siachen Muztagh. The following is a table of the peaks in the Siachen Muztagh which are over 7,200 meters (23,622 feet) in elevation and have over 500 meters (1,524 feet) of topographic prominence.

Geographic entities mentioned:
surface_form: Teram Kangri
instance_of: Mountain
countries: India
Pakistan
coordinates: lat: 35.58
lon: 77.0783
Waqutuyuq (Junín). Waqutuyuq (Quechua &quot;waqutu&quot; a variety of potatoes, &quot;-yuq&quot; a suffix, &quot;the one with the &quot;waqutu&quot;, also spelled &quot;Huajotuyoc&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It is located in the Junín Region, Jauja Province, Pomacancha District.

Geographic entities mentioned:
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
surface_form: waqutuyuq (junín)
instance_of: Mountain
countries: Peru
coordinates: lat: -11.59333333
lon: -75.7
surface_form: waqutuyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -12.904722222222
lon: -75.134722222222
Waqutuyuq (Junín). Waqutuyuq (Quechua &quot;waqutu&quot; a variety of potatoes, &quot;-yuq&quot; a suffix, &quot;the one with the &quot;waqutu&quot;, also spelled &quot;Huajotuyoc&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It is located in the Junín Region, Jauja Province, Pomacancha District.

Geographic entities mentioned:
surface_form: waqutuyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -11.59333333
lon: -75.7
surface_form: waqutuyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -12.904722222222
lon: -75.134722222222
The octagonal frame of the storks, juxtaposed against the rays and scrolls, offers a richness of contrasting shapes and colors”. On November 4, 1922, King Tutankhamun's tomb was discovered in the Valley of the Kings, Egypt. With this discovery, photographs were released to the public portraying the treasures found within the tomb.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
It is number J11 in Laws’ collection and #983 in the Roud Folk Song Index. Historical background. The song is based on the true story of a young ex-soldier from the Glen of Aherlow named Patrick Sheehan who was blinded at the Siege of Sevastopol. Sheehan was later jailed in 1857 for begging in Grafton Street, Dublin, his British army pension having expired after six months.

Geographic entities mentioned:
surface_form: Glen of Aherlow
instance_of: Valley
countries: Ireland
coordinates: lat: 52.419
lon: -8.193
The Bell Canyon drainage is located to the east and parallel to Cañada Gobernadora, and to the south of Trabuco Creek. After Trabuco Creek, it is the second largest tributary of San Juan Creek in terms of length and its watershed area of. Most of Bell Canyon consists of wilderness in the Cleveland National Forest and Ronald W. Caspers Wilderness Park.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: bell canyon
instance_of: Landform
countries: United States
coordinates: lat: 33.5342
lon: -117.555
Drainage. The headwaters of Bell Creek are a fan-shaped network of canyons eroded into the west side of Los Pinos Peak, which lie just a few miles south of the Trabuco Creek headwaters and a few miles north of Hot Spring Canyon, also a tributary of San Juan Creek. The headwaters are in the Trabuco Ranger District of the Cleveland National Forest, about east of Rancho Santa Margarita.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
On the southeast side are Cold Springs and Hot Springs Creek, tributaries of San Juan Creek above Bell Canyon Creek; on the northwest, Trabuco Creek, on the west, Cañada Gobernadora. Most of the Bell Canyon drainage area lies within the Cleveland National Forest in the upper half and the Ronald W.

Geographic entities mentioned:
surface_form: cleveland
instance_of: Mountain
countries: United States
coordinates: lat: 52.822222222222
lon: -169.945
surface_form: bell canyon
instance_of: Landform
countries: United States
coordinates: lat: 33.5342
lon: -117.555
Drainage. The headwaters of Bell Creek are a fan-shaped network of canyons eroded into the west side of Los Pinos Peak, which lie just a few miles south of the Trabuco Creek headwaters and a few miles north of Hot Spring Canyon, also a tributary of San Juan Creek. The headwaters are in the Trabuco Ranger District of the Cleveland National Forest, about east of Rancho Santa Margarita.

Geographic entities mentioned:
surface_form: los pinos peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.6642
lon: -117.471