Sarmila/GeoWiki-Features huggingface dataset:
Buni. Buni (Khowar,; also spelled Booni) is a town and the headquarters of Upper Chitral District in Khyber Pakhtunkhwa, Pakistan. The high Qaqlasht Meadows, which host a major festival in the region, are situated near the town. Lying near the foothills of the Buni Zom, Buni is located in proximity to glacial lakes due to which the town has faced floodings various times.

Geographic entities mentioned:
surface_form: chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
surface_form: booni
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.272777777777776
lon: 72.25972222222222
surface_form: buni
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.272777777777776
lon: 72.25972222222222
Through the glacial melting followed by heavy monsoon rainfalls, the region was severely affected by the floods during August 2024. Demography. The residents of Buni are primarily Kho people (also known as Chitralis), who speak Khowar, a language widely spoken and understood throughout the Chitral region. Urdu, the national language of Pakistan, is also commonly spoken and understood.

Geographic entities mentioned:
surface_form: chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
surface_form: buni
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.272777777777776
lon: 72.25972222222222
Climate. The climate is considered to be a local Mediterranean climate. During the year, there is abundant rainfall. This climate is considered to be Csa to the Köppen-Geiger climate classification. The average annual temperature in Buni is 15.6 °C. About 418 mm of precipitation falls annually. Educational institutions. There are a number of educational institutions in Booni, which includes;

Geographic entities mentioned:
surface_form: booni
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.272777777777776
lon: 72.25972222222222
Buni. Buni (Khowar,; also spelled Booni) is a town and the headquarters of Upper Chitral District in Khyber Pakhtunkhwa, Pakistan. The high Qaqlasht Meadows, which host a major festival in the region, are situated near the town. Lying near the foothills of the Buni Zom, Buni is located in proximity to glacial lakes due to which the town has faced floodings various times.

Geographic entities mentioned:
surface_form: buni
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.272777777777776
lon: 72.25972222222222
Climate. The climate is considered to be a local Mediterranean climate. During the year, there is abundant rainfall. This climate is considered to be Csa to the Köppen-Geiger climate classification. The average annual temperature in Buni is 15.6 °C. About 418 mm of precipitation falls annually. Educational institutions. There are a number of educational institutions in Booni, which includes;

Geographic entities mentioned:
surface_form: buni
instance_of: Valley
countries: Pakistan
coordinates: lat: 36.272777777777776
lon: 72.25972222222222
Lochrutton Loch. Lochrutton Loch is a large, lowland freshwater loch that lies to the west of Dumfries, Scotland. The loch trends from north to south and is long and at its widest point. It has an average depth of and is at its deepest. The loch was surveyed on 1 May 1905 by James Murray and L. W.

Geographic entities mentioned:
surface_form: lochrutton loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.039
lon: -3.7257
Armenia plans to restore the Soviet-era Yeraskh-Julfa-Meghri-Horadiz rail route, which would not only connect Armenia and Azerbaijan, but would also restore Armenia's railway connection with Iran and Russia. With this project, Armenia could offer new logistic pathways linking the Caspian Sea to the Mediterranean and Black seas through Armenian territory. Gyumri dry port.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Afan Forest Park. The Afan Forest Park (formally and locally known as Afan Argoed Country Park) is a forest park in Britain. It is set in the Afan Valley in Neath Port Talbot, in south Wales. It is well known for its mountain biking and hiking or hillwalking trails. It is situated from Junction 40 of the M4 (the Port Talbot turn). Trails and waymarked walks.

Geographic entities mentioned:
surface_form: afan forest park
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.632802777778
lon: -3.7327583333333
Afan Forest Park. The Afan Forest Park (formally and locally known as Afan Argoed Country Park) is a forest park in Britain. It is set in the Afan Valley in Neath Port Talbot, in south Wales. It is well known for its mountain biking and hiking or hillwalking trails. It is situated from Junction 40 of the M4 (the Port Talbot turn). Trails and waymarked walks.

Geographic entities mentioned:
surface_form: afan forest park
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.632802777778
lon: -3.7327583333333
surface_form: afan argoed
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.632802777778
lon: -3.7327583333333
Kanji Wood. In 2002, Afan Forest Park was officially twinned with the C.W.Nicol Woodland Trust in Kurohime in the Nagano prefecture of Japan. In Afan Forest Park, 'Kanji Wood' was developed on three kanji characters; human, forest and life and landscaped with Japanese trees, shrubs and sculptures. Education and activities.

Geographic entities mentioned:
surface_form: afan forest park
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.632802777778
lon: -3.7327583333333
This is a high level link that connects both The Wall and White's Level. Accommodation. Lists of places to stay in and around the park can be found at the Afan Forest Park website. Media. Afan Forest park was named in the top ten places in the world to &quot;ride before you die&quot; by &quot;What Mountain Bike Magazine&quot;. Other destinations named included Whistler, Canada.

Geographic entities mentioned:
surface_form: afan forest park
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.632802777778
lon: -3.7327583333333
surface_form: afan forest park
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.632802777778
lon: -3.7327583333333
Brachoria. &quot;Brachoria&quot; is a genus of polydesmidan millipedes in the family Xystodesmidae inhabiting the Eastern United States. Also known as the Appalachian mimic millipedes, at least 30 species are known, with highest diversity in the Appalachian Mountains, especially the Cumberland Plateau and Ridge and Valley Province.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Foel Penolau. Foel Penolau is a mountain close to Moel Ysgyfarnogod in Snowdonia, North Wales and is the northernmost summit of the Rhinogydd, and overlooks Llyn Trawsfynydd. From the summit it is possible to see the towns of Porthmadog and Blaenau Ffestiniog.

Geographic entities mentioned:
surface_form: Moel Ysgyfarnogod
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.89115
lon: -3.9961694444444
surface_form: foel penolau
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.894242
lon: -3.990612
Foel Penolau. Foel Penolau is a mountain close to Moel Ysgyfarnogod in Snowdonia, North Wales and is the northernmost summit of the Rhinogydd, and overlooks Llyn Trawsfynydd. From the summit it is possible to see the towns of Porthmadog and Blaenau Ffestiniog.

Geographic entities mentioned:
surface_form: foel penolau
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.894242
lon: -3.990612
From the summit it is possible to see the towns of Porthmadog and Blaenau Ffestiniog. As a result of a revised survey of its topographical prominence, Foel Penolau gained Hewitt and Simms status in December 2018 when its prominence was measured to be above. The top of Foel Penolau is reputed to be one of the rockiest summits in Snowdonia, where hands must be used to attain the summit.

Geographic entities mentioned:
surface_form: foel penolau
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.894242
lon: -3.990612
By 1999, The Weather Channel reached 70 million homes, or 98% of all households that subscribe to cable television. It also provided radio forecasts to more than 250 radio stations and weather information to 52 newspapers. Between 1999 and 2000, TWC aired weather observation reports from Mount Everest using battery-powered sensors.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Following it will reveal expansive views of the Presidential Range and Crawford Notch to the east, and the Twin Range to the west. Biodiversity. As part of the White Mountain Range, Mt. Willey hosts similar wildlife and plant life to the neighboring elevated regions in New Hampshire. The most common trees populating the White Mountain region, and in turn, Mt.

Geographic entities mentioned:
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: mt. willey
instance_of: Mountain
countries: United States
coordinates: lat: 44.1833
lon: -71.4167
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
Biodiversity. As part of the White Mountain Range, Mt. Willey hosts similar wildlife and plant life to the neighboring elevated regions in New Hampshire. The most common trees populating the White Mountain region, and in turn, Mt. Willey, are red spruce, balsam fir, sugar maple, American beech and yellow birch. At higher elevations, balsam fir and red spruce become more populous.

Geographic entities mentioned:
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: mt. willey
instance_of: Mountain
countries: United States
coordinates: lat: 44.1833
lon: -71.4167
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
Mount Willey. Mount Willey is a mountain located in Grafton County, New Hampshire. The mountain is named after Samuel Willey, Jr. (1766–1826) and his family, who in 1825 moved into a house in Crawford Notch. The family was killed a year later in August 1826 during a landslide. Mount Willey is part of the Willey Range of the White Mountains, of which it is the southernmost and second highest.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount willey
instance_of: Mountain
countries: United States
coordinates: lat: 44.1833
lon: -71.4167
The Ethan Pond Trail covers a longer distance and is classified as part of the Appalachian Trail. The Kedron Flume Trail spans a shorter distance and passes through the Kedron Flume waterfall. The Avalon Trail stems North from Mt. Field, and diverges into the A-Z Trail at half its length. The A-Z Trail runs from the Avalon trail to Zealand Hut. Mount Willey Trail.

Geographic entities mentioned:
surface_form: mt. field
instance_of: Mountain
countries: United States
coordinates: lat: 44.1962
lon: -71.4345
The family was killed a year later in August 1826 during a landslide. Mount Willey is part of the Willey Range of the White Mountains, of which it is the southernmost and second highest. It, along with Mount Field, forms the western wall of Crawford Notch. The summit is just outside the Crawford Notch State Park; it is at the northeast corner of the Pemigewasset Wilderness.

Geographic entities mentioned:
surface_form: mount field
instance_of: Mountain
countries: United States
coordinates: lat: 44.1962
lon: -71.4345
Mount Willey. Mount Willey is a mountain located in Grafton County, New Hampshire. The mountain is named after Samuel Willey, Jr. (1766–1826) and his family, who in 1825 moved into a house in Crawford Notch. The family was killed a year later in August 1826 during a landslide. Mount Willey is part of the Willey Range of the White Mountains, of which it is the southernmost and second highest.

Geographic entities mentioned:
surface_form: mount willey
instance_of: Mountain
countries: United States
coordinates: lat: 44.1833
lon: -71.4167
The mountain is named after Samuel Willey, Jr. (1766–1826) and his family, who in 1825 moved into a house in Crawford Notch. The family was killed a year later in August 1826 during a landslide. Mount Willey is part of the Willey Range of the White Mountains, of which it is the southernmost and second highest. It, along with Mount Field, forms the western wall of Crawford Notch.

Geographic entities mentioned:
surface_form: mount willey
instance_of: Mountain
countries: United States
coordinates: lat: 44.1833
lon: -71.4167
Multiple hiking trails span through its area, including a portion of the Appalachian Trail. Higher elevations classify as a spruce-fir forest, hosting natural life commonly found in the White Mountains region. The north and east faces of Mount Willey drain directly into the Saco River, thence into the Gulf of Maine at Saco, Maine.

Geographic entities mentioned:
surface_form: mount willey
instance_of: Mountain
countries: United States
coordinates: lat: 44.1833
lon: -71.4167
Connected Trails. This mountain can be traversed through a multitude of trails connecting over land in the White Mountains Range. Most frequently used is the Mount Willey Trail, which joins with surrounding trail junctions. The Ethan Pond Trail covers a longer distance and is classified as part of the Appalachian Trail.

Geographic entities mentioned:
surface_form: mount willey
instance_of: Mountain
countries: United States
coordinates: lat: 44.1833
lon: -71.4167
Field, and diverges into the A-Z Trail at half its length. The A-Z Trail runs from the Avalon trail to Zealand Hut. Mount Willey Trail. The peak can be reached via the 4.8 mile long Mount Willey Trail, beginning at the Willey Station Road Parking Lot, which branches off from Route 302. It joins with the Ethan Pond Trail and passes through the junction of the A-Z trail.

Geographic entities mentioned:
surface_form: mount willey
instance_of: Mountain
countries: United States
coordinates: lat: 44.1833
lon: -71.4167
District 3. District 3 comprises the cities of Carlsbad, Coronado, Del Mar, Encinitas, Solana Beach and the communities of La Jolla, Little Italy, Midway, Mira Mesa, Mission Beach, Ocean Beach, Pacific Highlands, Point Loma, Rancho Peñasquitos, Sorrento Valley, Torrey Highlands, Pacific Beach, University City, Carmel Valley, Harmony Grove, Rancho Santa Fe, and Elfin Forest.

Geographic entities mentioned:
surface_form: Point Loma
instance_of: Landform
countries: United States
coordinates: lat: 32.67
lon: -117.24194444
surface_form: Pacific Beach
instance_of: Landform
countries: United States
coordinates: lat: 32.797827777778
lon: -117.24031388889
It also had critical levels of fuel and ammunition and did not yet control Székesfehérvár that day, thereby lengthening the German supply lines. The Soviet 1st Mechanized Corps was also deployed to fight the SS, slowing down the German advance which was redirected north-east towards Lake Velence.

Geographic entities mentioned:
surface_form: Lake Velence
instance_of: Lake
countries: Hungary
coordinates: lat: 47.208333333333
lon: 18.6
Together with the first ascent of Mont Mallet in Chamonix’s Grandes Jorasses range, Loppé made over forty ascents of Mont Blanc during his climbing career, which lasted until the late 1890s. Loppé frequently made oil sketches from alpine summits, including a panorama of the view from the summit of Mont Blanc.

Geographic entities mentioned:
surface_form: Mont Mallet
instance_of: Mountain
countries: France
coordinates: lat: 45.86527778
lon: 6.96055556
surface_form: Grandes Jorasses
instance_of: Mountain
countries: Italy
France
coordinates: lat: 45.866666666667
lon: 6.9833333333333
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
The summit is in Washington County, but the mountain extends into Lamoille County as well. Mount Putnam stands within the watershed of the Winooski River, which drains into Lake Champlain, and ultimately into the Gulf of Saint Lawrence in Canada. The north side of Mount Putnam drains into Gold Brook, thence into the Little River and the Winooski River. The west side of Mt.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: mount putnam
instance_of: Mountain
countries: United States
coordinates: lat: 44.4183
lon: -72.6383
surface_form: mount putnam
instance_of: Mountain
countries: United States
coordinates: lat: 42.95305555555556
lon: -112.165
Mount Putnam (Vermont). Mount Putnam is a mountain located on the border between Washington County and Lamoille County, Vermont, in the Putnam State Forest. Mount Putnam, the high point of the Worcester Range, is flanked to the northeast by Mount Worcester, and to the southwest by Mount Hunger. It is the sixth most prominent peak in Vermont.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount putnam
instance_of: Mountain
countries: United States
coordinates: lat: 44.4183
lon: -72.6383
surface_form: mount putnam
instance_of: Mountain
countries: United States
coordinates: lat: 42.95305555555556
lon: -112.165
It is the sixth most prominent peak in Vermont. The summit is in Washington County, but the mountain extends into Lamoille County as well. Mount Putnam stands within the watershed of the Winooski River, which drains into Lake Champlain, and ultimately into the Gulf of Saint Lawrence in Canada.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Mount Putnam (Vermont). Mount Putnam is a mountain located on the border between Washington County and Lamoille County, Vermont, in the Putnam State Forest. Mount Putnam, the high point of the Worcester Range, is flanked to the northeast by Mount Worcester, and to the southwest by Mount Hunger. It is the sixth most prominent peak in Vermont.

Geographic entities mentioned:
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.924722222222
lon: -74.288055555556
surface_form: mount putnam
instance_of: Mountain
countries: United States
coordinates: lat: 44.4183
lon: -72.6383
surface_form: mount putnam
instance_of: Mountain
countries: United States
coordinates: lat: 42.95305555555556
lon: -112.165
surface_form: high point
instance_of: Mountain
countries: United States
coordinates: lat: 41.3209
lon: -74.6616
Mount Putnam (Vermont). Mount Putnam is a mountain located on the border between Washington County and Lamoille County, Vermont, in the Putnam State Forest. Mount Putnam, the high point of the Worcester Range, is flanked to the northeast by Mount Worcester, and to the southwest by Mount Hunger. It is the sixth most prominent peak in Vermont.

Geographic entities mentioned:
surface_form: mount putnam (vermont)
instance_of: Mountain
countries: United States
coordinates: lat: 44.4183
lon: -72.6383
surface_form: mount putnam
instance_of: Mountain
countries: United States
coordinates: lat: 42.95305555555556
lon: -112.165
The summit is in Washington County, but the mountain extends into Lamoille County as well. Mount Putnam stands within the watershed of the Winooski River, which drains into Lake Champlain, and ultimately into the Gulf of Saint Lawrence in Canada. The north side of Mount Putnam drains into Gold Brook, thence into the Little River and the Winooski River. The west side of Mt.

Geographic entities mentioned:
surface_form: mount putnam
instance_of: Mountain
countries: United States
coordinates: lat: 44.4183
lon: -72.6383
surface_form: mount putnam
instance_of: Mountain
countries: United States
coordinates: lat: 42.95305555555556
lon: -112.165
Mount Putnam stands within the watershed of the Winooski River, which drains into Lake Champlain, and ultimately into the Gulf of Saint Lawrence in Canada. The north side of Mount Putnam drains into Gold Brook, thence into the Little River and the Winooski River. The west side of Mt. Putnam drains into Thatcher Brook, and thence into the Winooski. The east side of Mt.

Geographic entities mentioned:
surface_form: mt. putnam
instance_of: Mountain
countries: United States
coordinates: lat: 44.4183
lon: -72.6383
surface_form: mt. putnam
instance_of: Mountain
countries: United States
coordinates: lat: 42.95305555555556
lon: -112.165
The north side of Mount Putnam drains into Gold Brook, thence into the Little River and the Winooski River. The west side of Mt. Putnam drains into Thatcher Brook, and thence into the Winooski. The east side of Mt. Putnam drains into Minister Brook, thence into the North Branch of the Winooski River.

Geographic entities mentioned:
surface_form: mt. putnam
instance_of: Mountain
countries: United States
coordinates: lat: 44.4183
lon: -72.6383
surface_form: mt. putnam
instance_of: Mountain
countries: United States
coordinates: lat: 42.95305555555556
lon: -112.165
Kumtumanje and Musopole were supported by the younger Kanyama Chiume and R. R. Chumia, and these four reinvigorated Congress throughout the Northern Province, opening new branches and building up a substantial following in the towns along Lake Malawi. Chiume, Musopole and Chumia were described by the police as ‘the main driving force’ behind Congress in the Northern Province.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
It then participated in the Kanawha Valley Campaign of 1862. The regiment returned to Tennessee for the Knoxville Campaign. The unit fought in numerous conflicts in the Shenandoah Valley before being disbanded around April 15, 1865. It reported 9 killed, 43 wounded, and 5 missing at Fort Donelson, and 3 killed and 16 wounded at Fayetteville.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Whin Rigg. Whin Rigg is a fell in the English Lake District, situated in the western segment of the national park, south east of the town of Whitehaven. It reaches only a modest altitude of but is part of one of the Lake District’s most dramatic landscapes in that the rugged and impressive Wastwater Screes (also known as &quot;The Screes&quot;) fall from the fells summit to Wast Water over below.

Geographic entities mentioned:
surface_form: Wast Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: wastwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: wast water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Topography and Geology. Whin Rigg is linked to the adjoining fell of Illgill Head, just away at the northern end of The Screes by a path that gives precipitous views down to Wast Water. The Screes are a Site of Special Scientific Interest and are regarded as a classic geological locality and one of the best and most famous examples of screes in Britain.

Geographic entities mentioned:
surface_form: Illgill Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4327
lon: -3.2825694444444
surface_form: illgill head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4327
lon: -3.2825694444444
surface_form: wast water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
Whin Rigg can be climbed either from Nether Wasdale in Wasdale or Eskdale Green in Eskdale using the bridleway which links the two places to attain the western ridge of the fell, there are then of ascent up the ridge to reach the summit. Walkers starting from the Wasdale side can also use the footpath by Greathall Gill as already mentioned. Summit.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
Ascents. The path on the eastern side of Greathall Gill has developed into a popular way up the fell from Nether Wasdale and has become eroded in recent years, it is being monitored so any worsening of the situation can be reversed.

Geographic entities mentioned:
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
Whin Rigg can be climbed either from Nether Wasdale in Wasdale or Eskdale Green in Eskdale using the bridleway which links the two places to attain the western ridge of the fell, there are then of ascent up the ridge to reach the summit. Walkers starting from the Wasdale side can also use the footpath by Greathall Gill as already mentioned. Summit.

Geographic entities mentioned:
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
The escarpment and screes are made up of hard wearing Borrowdale Volcanics rock, however there are areas of less resistant rock which have been eroded and this has led to deep gullies in the cliff face. The cliffs around the summit of Whin Rigg take the form of vertical rock buttresses which are split by the huge Great Gully and C Gully which give precipitous views of Wast Water.

Geographic entities mentioned:
surface_form: wast water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: whin rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.41945780200143
lon: -3.3093011327319037
The gullies are spectacular but are a no go area for walkers, Great Gully has seventeen near vertical pitches and the remains of an aeroplane within it. Apart from The Screes, Whin Rigg has another fine geological feature in Greathall Gill. This is a granite ravine which rises up the fell from where the River Irt flows out of Wast Water to the mark on the fell to the south west of the summit.

Geographic entities mentioned:
surface_form: wast water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
Walkers starting from the Wasdale side can also use the footpath by Greathall Gill as already mentioned. Summit. The highlight of the summit panorama is the view down to Wast Water, and there are good views of the coastal plain and the Isle of Man.

Geographic entities mentioned:
surface_form: wast water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
The Screes are a Site of Special Scientific Interest and are regarded as a classic geological locality and one of the best and most famous examples of screes in Britain. The escarpment and screes are made up of hard wearing Borrowdale Volcanics rock, however there are areas of less resistant rock which have been eroded and this has led to deep gullies in the cliff face.

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
Whin Rigg. Whin Rigg is a fell in the English Lake District, situated in the western segment of the national park, south east of the town of Whitehaven. It reaches only a modest altitude of but is part of one of the Lake District’s most dramatic landscapes in that the rugged and impressive Wastwater Screes (also known as &quot;The Screes&quot;) fall from the fells summit to Wast Water over below.

Geographic entities mentioned:
surface_form: whin rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.41945780200143
lon: -3.3093011327319037
The gullies are spectacular but are a no go area for walkers, Great Gully has seventeen near vertical pitches and the remains of an aeroplane within it. Apart from The Screes, Whin Rigg has another fine geological feature in Greathall Gill. This is a granite ravine which rises up the fell from where the River Irt flows out of Wast Water to the mark on the fell to the south west of the summit.

Geographic entities mentioned:
surface_form: whin rigg
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.41945780200143
lon: -3.3093011327319037
Lake George Scott. Lake George Scott, also called Scott Pond, is a small lake situated on the Tekapo River approximately 3 kilometres downstream of Lake Tekapo, New Zealand. It is a man-made lake formed to divert water from the river into the Tekapo hydro electric canal. The Lake is named after the late George Scott, a former superintendent of the nearby Tekapo A Power Station.

Geographic entities mentioned:
surface_form: Lake Tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
surface_form: lake george scott
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.015277777778
lon: 170.46305555556
surface_form: tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
surface_form: tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
It is a man-made lake formed to divert water from the river into the Tekapo hydro electric canal. The Lake is named after the late George Scott, a former superintendent of the nearby Tekapo A Power Station. The Department of Conservation maintains a walkway to the lake from the Lake Tekapo Township.

Geographic entities mentioned:
surface_form: Lake Tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
surface_form: tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
Lake George Scott. Lake George Scott, also called Scott Pond, is a small lake situated on the Tekapo River approximately 3 kilometres downstream of Lake Tekapo, New Zealand. It is a man-made lake formed to divert water from the river into the Tekapo hydro electric canal. The Lake is named after the late George Scott, a former superintendent of the nearby Tekapo A Power Station.

Geographic entities mentioned:
surface_form: lake george scott
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.015277777778
lon: 170.46305555556
Lake George Scott. Lake George Scott, also called Scott Pond, is a small lake situated on the Tekapo River approximately 3 kilometres downstream of Lake Tekapo, New Zealand. It is a man-made lake formed to divert water from the river into the Tekapo hydro electric canal. The Lake is named after the late George Scott, a former superintendent of the nearby Tekapo A Power Station.

Geographic entities mentioned:
surface_form: tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
It is a man-made lake formed to divert water from the river into the Tekapo hydro electric canal. The Lake is named after the late George Scott, a former superintendent of the nearby Tekapo A Power Station. The Department of Conservation maintains a walkway to the lake from the Lake Tekapo Township.

Geographic entities mentioned:
surface_form: tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
Early life. Murdoch was born in Kirkland Lake, Ontario, a mining community far from Southern Ontario in Timiskaming District. He grew up in nearby Larder Lake and played organized hockey in this area that saw many players go to the NHL, mainly playing on outdoor rinks. He went to the University of Waterloo where he received a double major degree in Mathematics and Physical Education.

Geographic entities mentioned:
surface_form: Larder Lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.085277777777776
lon: -79.64222222222222
Later life and death. While he was proud of his Northeastern Ontario roots, Murdoch and his family spent summers near Lake of the Woods in Northwestern Ontario. In later years, Canmore, Alberta was home, where he was diagnosed in 2019 with Lewy Body Dementia, and died in Calgary, Alberta on August 3, 2023, at the age of 76.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
It is located 36 km from Pakur, the district headquarters. A predominantly hilly area, Pakur district has pockets of plain land. A long but narrow stretch between the Farakka Feeder Canal, located outside the district, and the Sahibganj loop line is very fertile. The Littipara and Amrapara CD blocks are largely covered by the Rajmahal hills. The rest of the district is rolling uplands.

Geographic entities mentioned:
surface_form: Rajmahal hills
instance_of: Mountain
countries: India
coordinates: lat: 25
lon: 87
The Yorkshire Post described the church as boasting some impressive stained glass windows. The church was listed as Grade I in October 1966. Geography. The village sits in the Great Wold Valley and the waters of the winterbourne stream the Gypsey Race flow alongside the main street in the village. The waters of the Gypsey Race have carved a small valley out of the surrounding chalk.

Geographic entities mentioned:
surface_form: Great Wold Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.1385
lon: -0.3835
CR 425 is a short piece of SR 425 as defined in 1945. The route began at SR 426 and followed the entire length of Tuskawilla Road (now inventoried as CR 4281). A crossing of Lake Jesup was never built, but SR 425 began again on the north shore at the south end of Sanford Avenue, finally picking up current CR 425 to end at SR 46.

Geographic entities mentioned:
surface_form: Lake Jesup
instance_of: Lake
countries: United States
coordinates: lat: 28.7272492
lon: -81.2205217
Pic de la Dona. Pic de la Dona is a mountain of Catalonia, Spain. Located in the Pyrenees, it has an elevation of above sea level.

Geographic entities mentioned:
surface_form: pic de la dona
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.43777778
lon: 2.26138889
Cargoes consisted of coal/coke, aggregates, slag, iron ore/oxides, salt, fertilizers, grain products, gypsum, quartzite, and sand. The freighter set several load records on the Great Lakes, including those for wheat and salt. On 28 December 1976, &quot;Algosoo&quot; went aground in Lake St. Clair, which according the United States Coast Guard, was probably caused by ice on the lake.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
In 1995, &quot;Algosoo&quot; damaged its propeller and leaked some oil in the St. Lawrence River. On 23 December 2000 &quot;Algosoo&quot; collided with the Canadian Coast Guard icebreaker while being freed from ice near the Toledo Channel in Lake Erie. On 26 December the freighter arrived for repairs at Hamilton, Ontario. In April 2002, fleetmate went aground in the St.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Sabinus was also close to Benedict of Nursia. Pope Gregory the Great in his &quot;Dialogues&quot; mentions how Benedict, praying atop Monte Cassino, had a vision of the soul of Germanus in the form of a ball of fire being carried to heaven by angels. He later learned that this vision coincided with Germanus's death.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
People began to visit the site, drawn to the scene of devastation, human tragedy and the miraculous survival of the structure itself. As well as boosting a nascent tourist industry in the area, in which the Crawford family had already been playing a significant part, it became a source of inspiration for artists and writers. The peak on the western wall of the notch became known as Mount Willey.

Geographic entities mentioned:
surface_form: Mount Willey
instance_of: Mountain
countries: United States
coordinates: lat: 44.1833
lon: -71.4167
The Tigris serves as the marshes' eastern boundary while the Euphrates serves as its southern boundary. Covering an area of, the marshes consist of reed beds and several permanent lakes including Umm al Binni lake. The Al-Zikri and Hawr Umm Al-Binni lakes are two of the notable lakes and are deep. Hammar.

Geographic entities mentioned:
surface_form: Umm al Binni lake
instance_of: Lake
countries: Iraq
coordinates: lat: 31.241388888889
lon: 47.105833333333
Founding. An Act of the Assembly of Albemarle County established Charlottesville in 1762. Thomas Walker was named its first trustee. It was situated along a trade route called Three Notched Road (present day U.S. Route 250), which led from Richmond to the Great Valley. The town took its name from the British queen Charlotte of Mecklenburg-Strelitz.

Geographic entities mentioned:
surface_form: Great Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
A post office operated at Manzanar from 1911 to 1914. Manzanar was a shipping point for the surrounding apple orchards before the diversion of water through the Los Angeles Aqueduct from the Owens Valley to Los Angeles. During World War II, the area was the location of the Manzanar War Relocation Center, where people of Japanese ancestry were held. Owens Valley Paiute.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Owens Valley Paiute. Manzanar was first inhabited by Native Americans nearly 10,000 years ago. Approximately 1,500 years ago, the area was settled by the Owens Valley Paiute, who ranged across the Owens Valley from Long Valley on the north to Owens Lake on the south, and from the crest of the Sierra Nevada on the west to the Inyo Mountains on the east.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
surface_form: Long Valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
The Owens Valley Paiute hunted and fished, collected pine nuts, and raised crops utilizing irrigation in the Manzanar area. They also traded brown-ware pottery for salt from the Saline Valley, and traded other wares and goods across the Sierra Nevada during the summer and fall.

Geographic entities mentioned:
surface_form: Saline Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.75
lon: -117.81
Tarnica. Tarnica is a peak in the Bieszczady Mountains in southern Poland. Its height is 1,346 metres. It is one of the Polish Crown Peaks. The summit towers 500 metres above the Wołosatka Valley. It can be easily told apart from its neighbours by its distinctive shape. The mountain has two separate summits, one of 1,339 and one of 1,346 metres.

Geographic entities mentioned:
surface_form: tarnica
instance_of: Mountain
countries: Poland
coordinates: lat: 49.069444444444
lon: 22.738055555556
On September 14, 1901, then-Vice President Theodore Roosevelt was at Lake Tear of the Clouds after returning from a hike to the Mount Marcy summit when he received a message informing him that President William McKinley, who had been shot two weeks earlier but was expected to survive, had taken a turn for the worse.

Geographic entities mentioned:
surface_form: Lake Tear of the Clouds
instance_of: Lake
countries: United States
coordinates: lat: 44.1067
lon: -73.9358
surface_form: Mount Marcy
instance_of: Mountain
countries: United States
coordinates: lat: 44.112733333333
lon: -73.923727777778
In 2015, Matilde Borromeo served as chief ambassador for the Milano Winter Show and Fiera Verona Cavalli. Personal life. On 11 June 2011 Borromeo married Antonius zu Fürstenberg, the youngest son of Heinrich Fürst zu Fürstenberg, at Isola Bella, one of the Borromean Islands in Lake Maggiore owned by the Borromeo family. They have two children, Karl Egon and Alexander.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
This occurs in the spring and autumn when the water column becomes uniformly mixed due to temperature-driven density changes
Loch Lomond is long and between wide, with a surface area of. It is the largest lake in Great Britain by surface area; in the United Kingdom, it is surpassed only by Lough Neagh and Lough Erne in Northern Ireland.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
surface_form: neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
surface_form: erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
The total volume of Loch Lomond is, making it the second largest lake in Great Britain, after Loch Ness, by water volume.Due to its considerable depth and latitudinal location, Loch Lomond exhibits thermal stratification during the summer months, with a distinct epilimnion, metalimnion, and hypolimnion forming in deeper areas.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
surface_form: loch lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
surface_form: loch lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
surface_form: lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
surface_form: lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Loch Lomond is a popular leisure destination and is featured in the song &quot;The Bonnie Banks o' Loch Lomond&quot;. The loch is surrounded by hills, including Ben Lomond on the eastern shore, which is in height and the most southerly of the Scottish Munro peaks. A 2005 poll of &quot;Radio Times&quot; readers voted Loch Lomond as the sixth greatest natural wonder in Britain. Etymology.

Geographic entities mentioned:
surface_form: Ben Lomond
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.190293
lon: -4.633009
surface_form: ben lomond
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.190293
lon: -4.633009
surface_form: lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
A 2005 poll of &quot;Radio Times&quot; readers voted Loch Lomond as the sixth greatest natural wonder in Britain. Etymology. Loch Lomond takes its name from the highest peak in the area, Ben Lomond, meaning ‘beacon mountain’ i.e. a site for warning beacons.

Geographic entities mentioned:
surface_form: Ben Lomond
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.190293
lon: -4.633009
surface_form: ben lomond
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.190293
lon: -4.633009
surface_form: lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
The change in rock type can be clearly seen at points around the loch, as it runs across the islands of Inchmurrin, Creinch, Torrinch and Inchcailloch and over the ridge of Conic Hill. The loch's shape and many of its islands follow the line of the HBF separates the ancient metamorphic rocks of the Highlands from the younger sedimentary rocks of the Lowlands.

Geographic entities mentioned:
surface_form: Conic Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.097
lon: -4.5246
surface_form: conic hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.097
lon: -4.5246
Inchmurrin, for example, is the largest island in a body of freshwater in the British Isles. Many of the islands are the remains of harder rocks that withstood the passing of the glaciers; however, as in Loch Tay, several of the islands appear to be crannogs, artificial islands built in prehistoric periods. Flora and fauna.

Geographic entities mentioned:
surface_form: Loch Tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
surface_form: loch tay
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.515555555556
lon: -4.1461111111111
A minor road extends north as far as Rowardennan, a further 11 km away, however beyond this point no road continues along the eastern shore, although there is road access to Inversnaid via another minor road that comes in from Loch Katrine to the east via the northern shore of Loch Arklet.

Geographic entities mentioned:
surface_form: Loch Katrine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.254444444444445
lon: -4.515555555555555
surface_form: loch katrine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.254444444444445
lon: -4.515555555555555
The hydrology and structure of the loch are strongly influenced by its glacial origins and underlying geology. Formed during the last glaciation, the loch occupies a classic glacial trough, carved by ice movement from the Ben Lui region.

Geographic entities mentioned:
surface_form: ben lui
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.397004
lon: -4.810525