Sarmila/GeoWiki-Features huggingface dataset:
For instance, the name of the mount &quot;Parnassos&quot; in Greece has been interpreted as the Luwian &quot;parna-&quot; ('house') attached to the possessive suffix &quot;-ssa-&quot;. Both Hittite and Luwian texts also attest a place-name &quot;Parnassa&quot;, which could be related. Philologist Martin L.

Geographic entities mentioned:
surface_form: &quot;Parnassos&quot;
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
Along the valley floor lies a chain of large and small saline lakes, which are generally shallow, with a saucer-shaped depth profile. The largest of these lakes are Böön Tsagaan Lake and Orog Lake. Water levels vary considerably in size both seasonally and from year to year, and some lakes may dry out completely in certain years.

Geographic entities mentioned:
surface_form: Böön Tsagaan Lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.5961
lon: 99.142
surface_form: Orog Lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.055
lon: 100.70472222222
The fish fauna includes species of Oreoleuciscus and Thymallus brevirostris endemic to the western Mongolia. The valley was first explored scientifically by the geographer Nikolay Przhevalsky. In 1998, the whole valley region (including Böön Tsagaan Lake, Taatsiin Tsagaan Lake, and Orog Lake) was designated a Ramsar site of international importance.

Geographic entities mentioned:
surface_form: Böön Tsagaan Lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.5961
lon: 99.142
surface_form: Taatsiin Tsagaan Lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.156
lon: 101.4689
surface_form: Orog Lake
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.055
lon: 100.70472222222
Valley of the Lakes. The Valley of the Lakes () is an intermontane depression located in southwestern Mongolia, separating the Khangai and Govi-Altai mountains. The valley stretches 500 km long, has a width of approximately 100 km, and is located at altitudes ranging between 1000 and 1400 meters above sea level.

Geographic entities mentioned:
surface_form: valley of the lakes
instance_of: Valley
countries: Mongolia
coordinates: lat: 45.3167
lon: 99.9667
The campaign into Manchuria in 1387 was ultimately successful, but the commanding general, Feng Sheng, was replaced by Lan Yu. In the 1388 campaign, Lan Yu's army of 200,000 decisively defeated the Mongols at the Songhua River and Buir Lake. The Chinese captured 73,000 Mongol warriors, including the Mongol crown prince and his younger brother.

Geographic entities mentioned:
surface_form: Buir Lake
instance_of: Lake
countries: Mongolia
People's Republic of China
coordinates: lat: 47.806944444444
lon: 117.69222222222
Soon after her arrival in the turnover port of Rota, &quot;America&quot; participated in a NATO exercise, &quot;Open Gate&quot;, before entering the Mediterranean. Passing the Pillars of Hercules on 3 May, the ship entered into the eastern Mediterranean in support of Operation &quot;Fluid Drive&quot;, a contingency operation for the evacuation of non-combatants from war-torn Lebanon.

Geographic entities mentioned:
surface_form: Pillars of Hercules
instance_of: Landform
countries: Morocco
Spain
Gibraltar
coordinates: lat: 36
lon: -5.35
The rest of the year the regiment was deployed on Monte Sober, at Vrtojba, and again on Markov Hrib. In 1917 the regiment fought in the Tenth Battle of the Isonzo and was then deployed on the Banjšice Plateau, where the regiment fought in the Eleventh Battle of the Isonzo.

Geographic entities mentioned:
surface_form: Banjšice Plateau
instance_of: Plateau
countries: Slovenia
coordinates: lat: 46.04905
lon: 13.69995
Abitibi River. The Abitibi River is a river in northeastern Ontario, Canada, which flows northwest from Lake Abitibi to join the Moose River which empties into James Bay. This river is long, and descends. It is the ninth longest river in Ontario, Behind the Ottawa River (1,271km), St.

Geographic entities mentioned:
surface_form: Lake Abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
Cherry Lake (South Dakota). Cherry Lake is a lake in South Dakota, in the United States. The lake was named for the abundant growth of chokecherries at the site.

Geographic entities mentioned:
surface_form: cherry lake (south dakota)
instance_of: Lake
countries: United States
coordinates: lat: 44.545629
lon: -97.5253618
Cherry Lake (South Dakota). Cherry Lake is a lake in South Dakota, in the United States. The lake was named for the abundant growth of chokecherries at the site.

Geographic entities mentioned:
surface_form: cherry lake
instance_of: Lake
countries: United States
coordinates: lat: 44.545629
lon: -97.5253618
Rural Municipality of Gimli. The Rural Municipality of Gimli is a rural municipality located in the Interlake Region of south-central Manitoba, Canada, on the western shore of Lake Winnipeg. It is about north of the provincial capital Winnipeg. The rural municipality's population in the 2016 Canadian Census was 6,181, making it the 12th largest rural municipality by population.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
The Town of Winnipeg Beach lies adjacent to its southeast corner, on the shores of Lake Winnipeg, between it and the Rural Municipality of St. Andrews to the south. History. The Rural Municipality of Gimli was first settled by a large group of Icelandic settlers who arrived in New Iceland on Lake Winnipeg in the 1870s.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Glassy Mountain (Georgia). Glassy Mountain is a mountain in the Chattahoochee National Forest in Rabun County, Georgia, with its USGS GNIS summit at, which is AMSL. It is bypassed on its northern flank by a major two-lane highway that carries U.S. Route 76 and Georgia State Route 2 east and west.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: glassy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.8456
lon: -83.5006
surface_form: chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
surface_form: glassy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.9008
lon: -82.6592
Glassy Mountain (Georgia). Glassy Mountain is a mountain in the Chattahoochee National Forest in Rabun County, Georgia, with its USGS GNIS summit at, which is AMSL. It is bypassed on its northern flank by a major two-lane highway that carries U.S. Route 76 and Georgia State Route 2 east and west.

Geographic entities mentioned:
surface_form: glassy mountain (georgia)
instance_of: Mountain
countries: United States
coordinates: lat: 34.8456
lon: -83.5006
surface_form: glassy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.9008
lon: -82.6592
A radio tower and a fire lookout tower are both located atop the mountain. The fire tower was built at Glassy Mountain in 1941. The forest service added a residence and garage in the 1960s.

Geographic entities mentioned:
surface_form: glassy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.8456
lon: -83.5006
surface_form: glassy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.9008
lon: -82.6592
Route 76 and Georgia State Route 2 east and west. It is also the location of NOAA Weather Radio station KXI81, which serves nearby Clayton, Georgia (to the east-northeast), Lake Burton (to the west and southwest), and adjacent areas of northeast Georgia, upstate South Carolina, and western North Carolina. A radio tower and a fire lookout tower are both located atop the mountain.

Geographic entities mentioned:
surface_form: lake burton
instance_of: Lake
countries: United States
coordinates: lat: 34.8269
lon: -83.5551
Ilave. Ilave, also known as Illawi, is the capital city of the Ilave District in El Collao Province, in the Puno Region of Peru. According to the projection of the 2012 census, it has 57,366 inhabitants. It is located on the Ilave River and west from Lake Titicaca.

Geographic entities mentioned:
surface_form: Ilave River
instance_of: Watercourse
countries: Peru
coordinates: lat: -16.000277777778
lon: -69.443055555556
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325
Saddleback Junior. Saddleback Junior is a mountain located in Franklin County, Maine. Saddleback Junior is flanked to the southwest by Saddleback Horn, and to the northeast by Poplar Ridge. The mountain is on the south border of the U.S. Navy Survival Escape and Evasion Training Facility (USSEAETF).

Geographic entities mentioned:
surface_form: Saddleback Horn
instance_of: Mountain
countries: United States
coordinates: lat: 44.951333333333
lon: -70.487166666667
surface_form: saddleback junior
instance_of: Mountain
countries: United States
coordinates: lat: 44.95815
lon: -70.457783333333
The east and south sides of Saddleback Jr. drain into Hardy Stream, then into Orbeton Stream, and the Sandy River, another tributary of the Kennebec. The Appalachian Trail, a National Scenic Trail from Georgia to Maine, runs across the summit of Saddleback Junior, between Saddleback and Spaulding Mountain.

Geographic entities mentioned:
surface_form: Spaulding Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.003
lon: -70.3335
surface_form: saddleback junior
instance_of: Mountain
countries: United States
coordinates: lat: 44.95815
lon: -70.457783333333
Saddleback Junior. Saddleback Junior is a mountain located in Franklin County, Maine. Saddleback Junior is flanked to the southwest by Saddleback Horn, and to the northeast by Poplar Ridge. The mountain is on the south border of the U.S. Navy Survival Escape and Evasion Training Facility (USSEAETF).

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: saddleback junior
instance_of: Mountain
countries: United States
coordinates: lat: 44.95815
lon: -70.457783333333
Navy Survival Escape and Evasion Training Facility (USSEAETF). Saddleback Junior stands within the watershed of the Kennebec River, which drains into the Gulf of Maine. The northeast and northwest sides of Saddleback Jr. drain into Redington Stream, then into the South Branch of the Dead River, and the Kennebec River. The east and south sides of Saddleback Jr.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
Saddleback Junior. Saddleback Junior is a mountain located in Franklin County, Maine. Saddleback Junior is flanked to the southwest by Saddleback Horn, and to the northeast by Poplar Ridge. The mountain is on the south border of the U.S. Navy Survival Escape and Evasion Training Facility (USSEAETF).

Geographic entities mentioned:
surface_form: saddleback junior
instance_of: Mountain
countries: United States
coordinates: lat: 44.95815
lon: -70.457783333333
The mountain is on the south border of the U.S. Navy Survival Escape and Evasion Training Facility (USSEAETF). Saddleback Junior stands within the watershed of the Kennebec River, which drains into the Gulf of Maine. The northeast and northwest sides of Saddleback Jr. drain into Redington Stream, then into the South Branch of the Dead River, and the Kennebec River.

Geographic entities mentioned:
surface_form: saddleback junior
instance_of: Mountain
countries: United States
coordinates: lat: 44.95815
lon: -70.457783333333
Oum Er-Rbia has six dams, the most important of which is Al Massira Dam. Its most important tributaries are the El-Abid River, the Tessaoute River, and the Lakhdar River. According to scholars, the original Berber common name of the river is Wansifen and was only changed recently, circa 16th or 17th century, and a nearby village called Oum Rabia might have influenced this change.

Geographic entities mentioned:
surface_form: El-Abid River
instance_of: Watercourse
countries: Morocco
coordinates: lat: 32.29017
lon: -7.05175
Three main plutons are present. The oldest and most extensive is an irregularly-zoned pluton composed of quartz diorite at the margins, grading inward through granodiorite to a small core of granite. This pluton is exposed on both sides of Chilliwack Lake, a narrow north–south trending lake in the Cascade Mountains.

Geographic entities mentioned:
surface_form: Chilliwack Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.05694444444445
lon: -121.41388888888889
This pluton is exposed on both sides of Chilliwack Lake, a narrow north–south trending lake in the Cascade Mountains. Two younger plutons, consisting of nearly homogeneous leucocratic biotite quartz monzonite, are situated north of Chilliwack Lake and east of Slesse Mountain. Coquihalla Volcanic Complex.

Geographic entities mentioned:
surface_form: Slesse Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.0256
lon: -121.592
It comprises volcanic and intrusive rocks that are calc-alkaline felsic to intermediate in composition. Coquihalla Mountain, the highest summit of the Bedded Range with an elevation of, is a major preserved stratovolcano and represents one of the few remaining Miocene volcanoes in southwestern British Columbia.

Geographic entities mentioned:
surface_form: Coquihalla Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.525
lon: -121.06
A large stock, composed of pyroxene diorite and biotite-pyroxene quartz diorite, forms the present base of Coquihalla Mountain. Mount Barr Plutonic Complex. South of the Fraser River at Wahleach Lake is the Mount Barr Plutonic Complex. Named after Mount Barr in the Skagit Range of the Cascade Mountains, this plutonic complex ranges in age from 21 to 16 million years old.

Geographic entities mentioned:
surface_form: Wahleach Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.2333
lon: -121.617
Mount Barr Plutonic Complex. South of the Fraser River at Wahleach Lake is the Mount Barr Plutonic Complex. Named after Mount Barr in the Skagit Range of the Cascade Mountains, this plutonic complex ranges in age from 21 to 16 million years old. It consists of at least four plutons.

Geographic entities mentioned:
surface_form: Mount Barr
instance_of: Mountain
countries: Canada
coordinates: lat: 49.2636
lon: -121.56
Because of its heterogeneity, it is only occasionally grouped as part of the Mount Barr Plutonic Complex. Crevasse Crag Volcanic Complex. About southeast of Lillooet Lake is the Crevasse Crag Volcanic Complex. It is about 16 million years old, situated on the summit of a glaciated mountain ridge made of Late Cretaceous and younger intrusive rocks.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
Southern segment. Three principal volcanoes comprise the southern segment along with several smaller edifies. The largest and youngest principal volcano, Mount Garibaldi, is a dissected stratovolcano that began its formation 250,000 years ago. This eruptive period built a broad composite cone made of dacite and breccia.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
After reaching its maximum extent the Cheekye Glacier and Cordilleran Ice Sheet were covered with volcanic ash and fragmental debris from Garibaldi. This period of growth began with the eruption of the Atwell Peak plug dome about 13,000 years ago from a ridge surrounded by the ice sheet. As the plug dome grew, massive sheets of broken lava crumbled as talus down its sides.

Geographic entities mentioned:
surface_form: Atwell Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8411
lon: -123.009
Later volcanism occurred from Dalton Dome, which forms Garibaldi's western summit. Lava flows mantled the landslide headwall on Garibaldi's western flank. Around the same time, a voluminous dacite lava flow from Opal Cone travelled down Ring Creek on Garibaldi's southeastern flank without encountering any residual glacial ice.

Geographic entities mentioned:
surface_form: Opal Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 49.8272
lon: -122.971
After the ice sheet had retreated from higher elevations, andesite eruptions from a satellite vent created a small lava dome on Price's northern flank. Possibly contemporaneous volcanism occurred at Clinker Peak about 10,000 years ago with the eruption of two hornblende-biotite andesite lava flows. They are both over thick and long, extending to the northwest and southwest.

Geographic entities mentioned:
surface_form: Clinker Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.93
lon: -123.04
This was the last eruptive activity at Mount Price. The Black Tusk, the oldest and most striking of the three principal volcanoes, is the glacially dissected remains of a stratovolcano that formed between 1.3  and 1.1 million years ago. Eruptions produced hornblende andesite lava flows and lithic tuffs. Prolonged erosion destroyed the original cone.

Geographic entities mentioned:
surface_form: The Black Tusk
instance_of: Mountain
countries: Canada
coordinates: lat: 49.97527777777778
lon: -123.04277777777777
A long lava flow, ranging from basalt to mugearite, issued from the base of the cone and travelled in a north-trending U-shaped valley on the eastern flank of The Black Tusk. The Monmouth Creek complex on the west side of the Squamish River mouth is a prominent and enigmatic edifice composed of basaltic andesite and dacite of unknown age.

Geographic entities mentioned:
surface_form: Monmouth Creek complex
instance_of: Mountain
countries: Canada
coordinates: lat: 49.6939
lon: -123.197
The most elevated lava flows and spines are composed of dacite. Along the northeastern shore of Howe Sound is a small outcrop of volcanic rock known as the Watts Point volcanic centre. It is the southernmost volcano in the Garibaldi Volcanic Belt, comprising about of hornblende, pyroxene and sparsely porphyritic dacite lava and breccia.

Geographic entities mentioned:
surface_form: Watts Point volcanic centre
instance_of: Mountain
countries: Canada
coordinates: lat: 49.65
lon: -123.21
Subsequent activity 0.3–0.2 million years ago began with the eruption of a dacite lava flow into the Shovelnose Creek valley. This resulted in the formation of two small lava domes. Mount Fee is a long and wide spine of rhyodacite situated on a mountain ridge east of the Squamish River. Like Mount Cayley, it predates the appearance of the Cordilleran Ice Sheet.

Geographic entities mentioned:
surface_form: Mount Fee
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0831
lon: -123.25
Like Mount Cayley, it predates the appearance of the Cordilleran Ice Sheet. Other volcanoes in the central segment, such as Slag Hill, Ember Ridge, Cauldron Dome, Pali Dome and Ring Mountain, were formed when lava came into contact with the Cordilleran Ice Sheet. They are similar in structure to tuyas, displaying oversteepened ice-contact margins.

Geographic entities mentioned:
surface_form: Slag Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1834
lon: -123.3
surface_form: Cauldron Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1556
lon: -123.319
surface_form: Pali Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 50.136944444444
lon: -123.30694444444
They are similar in structure to tuyas, displaying oversteepened ice-contact margins. At least two sequences of basaltic andesite lava flows are deposited south of Tricouni Peak. One of these sequences, known as Tricouni Southwest, creates a cliff on the eastern side of a north–south trending channel with a depth of adjacent to the High Falls Creek mouth.

Geographic entities mentioned:
surface_form: Tricouni Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6317
lon: -123.504
At least two sequences of basaltic andesite lava flows are deposited south of Tricouni Peak. One of these sequences, known as Tricouni Southwest, creates a cliff on the eastern side of a north–south trending channel with a depth of adjacent to the High Falls Creek mouth. The eastern flank of the lava flow, outside the High Falls Creek channel, has a more constant structure.

Geographic entities mentioned:
surface_form: High Falls Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.93298
lon: -123.31943
As a result, the western portion of the lava flow records glaciation during a period when the eastern slopes were free from glacial ice. Tricouni Southeast, the other volcanic sequence south of Tricouni Peak, consists of at least four andesite or dacite lava flows that outcrop as several small cliffs and bluffs on extensively vegetated flanks.

Geographic entities mentioned:
surface_form: Tricouni Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.6317
lon: -123.504
The mafic, intermediate and felsic volcanic rocks comprising Meager were erupted from at least eight volcanic vents. Extending north of the Mount Meager massif almost to the Interior Plateau are the Bridge River Cones. This group of small volcanoes on the upper Bridge River includes stratovolcanoes, volcanic plugs and lava flows.

Geographic entities mentioned:
surface_form: Interior Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
surface_form: Bridge River Cones
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8
lon: -123.4
At least two volcanoes and one volcanic group may have formed as a result of Canadian Cascade Arc volcanism. The oldest feature, the Franklin Glacier Complex, is a deeply eroded long and wide geological structure with an elevation of over. It consists of dikes and subvolcanic intrusions overlain by tuffs, dacite breccia and eroded remains of a thick sequence of hornblende andesite lava flows.

Geographic entities mentioned:
surface_form: Franklin Glacier Complex
instance_of: Mountain
countries: Canada
coordinates: lat: 51.3333
lon: -125.4
This indicates that the Franklin Glacier Complex can be considered part of the Pemberton Volcanic Belt or the Garibaldi Volcanic Belt. About north-northwest of the Franklin Glacier Complex is the deeply dissected Silverthrone Caldera. It is wide, with steep slopes extending from near sea level to a maximum elevation of.

Geographic entities mentioned:
surface_form: Silverthrone Caldera
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4333
lon: -126.3
In some places, the basal breccia has been welded together by intense volcanic heat. Subsequent activity 750,000 to 400,000 years ago constructed rhyolite, dacite and andesite lava domes, breccia and lava flows. Mount Silverthrone, a volcanic peak associated with the Silverthrone Caldera, consists of overlapping andesite and rhyolite lava domes that were formed during this eruptive period.

Geographic entities mentioned:
surface_form: Mount Silverthrone
instance_of: Mountain
countries: Canada
coordinates: lat: 51.51777777777778
lon: -126.11333333333333
Its formation might have also resulted from other tectonic processes that are currently not understood. Swindle Island contains a high symmetrical cinder cone on its southern shoreline. This volcano, known as Kitasu Hill, comprises tephra and volcanic bombs. Its summit contains a volcanic crater that is breached to the east.

Geographic entities mentioned:
surface_form: Kitasu Hill
instance_of: Mountain
countries: Canada
coordinates: lat: 52.5
lon: -128.73
The fort contained a chapel and mission house. Queen Anne donated a set of communion silver and sent two missionaries to the colony. In return, she asked Tejonihokarawa for help in settling Palatine Germans, Protestant refugees then working at English camps in the Hudson Valley in present-day Dutchess County. They had left the Palatine because of French invasions related to religious wars.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Course and system. The Dodder rises on the northern slopes of Kippure in the Wicklow Mountains and is formed from several streams. The headwaters flow from Kippure Ridge, and include, and are often mapped solely as, Tromanallison (Allison's Brook), which is then joined by Mareen's Brook, including the Cataract of the Brown Rowan, and then the combined flow meeting the Cot and Slade Brooks.

Geographic entities mentioned:
surface_form: Kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
The headwaters flow from Kippure Ridge, and include, and are often mapped solely as, Tromanallison (Allison's Brook), which is then joined by Mareen's Brook, including the Cataract of the Brown Rowan, and then the combined flow meeting the Cot and Slade Brooks. In the river's valley at Glenasmole are the two Bohernabreena Reservoirs, a major part of the Dublin water supply system.

Geographic entities mentioned:
surface_form: Glenasmole
instance_of: Valley
countries: Ireland
coordinates: lat: 53.23301
lon: -6.356268
Hurricane Charley (often spelt &quot;Charlie&quot; in Ireland) passed south of the country on 25 August 1986. In 24 hours, 200mm (almost 8 inches) of rain poured down on Kippure Mountain while 100mm fell on Dublin causing heavy river flooding, including the Dodder in many places, and hardship and loss were experienced.

Geographic entities mentioned:
surface_form: Kippure
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.169397
lon: -6.338322
Morey Peak. Morey Peak is a mountain summit with an elevation of 3123 meters (10246 ft), with a prominence of 51 meters. It is located in the Hot Creek Range in the state of Nevada, United States. Geography. The past volcanic activity in the area has formed many steep and cliffs and gullies across the summit. The mountains near Morey Peak are composed out of quartz latite and rhyolite intrusives.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: morey peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.627777777778
lon: -116.28805555556
Morey Peak. Morey Peak is a mountain summit with an elevation of 3123 meters (10246 ft), with a prominence of 51 meters. It is located in the Hot Creek Range in the state of Nevada, United States. Geography. The past volcanic activity in the area has formed many steep and cliffs and gullies across the summit. The mountains near Morey Peak are composed out of quartz latite and rhyolite intrusives.

Geographic entities mentioned:
surface_form: morey peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.627777777778
lon: -116.28805555556
It is located in the Hot Creek Range in the state of Nevada, United States. Geography. The past volcanic activity in the area has formed many steep and cliffs and gullies across the summit. The mountains near Morey Peak are composed out of quartz latite and rhyolite intrusives. Most of which come from the Oligocene epoch, estimated to be between 25 - 30 million years ago. Flora and fauna.

Geographic entities mentioned:
surface_form: morey peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.627777777778
lon: -116.28805555556
Most of which come from the Oligocene epoch, estimated to be between 25 - 30 million years ago. Flora and fauna. Most flowers in Hot Creek Range around Morey Peak can typically be found in wetter areas like near streams. Such are Irises, Lupines, Wild roses, primroses, scarlet columbines, palmer penstemons, purple penstemons, red penstemons, and lavender.

Geographic entities mentioned:
surface_form: morey peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.627777777778
lon: -116.28805555556
state of Alaska. Green, as a political newcomer, was elected to the Alaska Senate in 1994, defeating a 22-year Democratic incumbent in a district representing most of the population of the Matanuska-Susitna Borough. Two Democratic members of the Alaska House of Representatives, also from the Matanuska-Susitna Valley, were defeated in the same election.

Geographic entities mentioned:
surface_form: Matanuska-Susitna Valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
Csobánc. Csobánc is a hill in the Tapolca Basin, Hungary. Geography and environment. Csobánc is one of the highlights of the region. Similar to the other hills in the area, it is of volcanic origin. These hills are witness hills. The expression originates from the fact that these hills “witnessed” the decrease of the land surface level during volcanic activity millions of years ago.

Geographic entities mentioned:
surface_form: csobánc
instance_of: Mountain
countries: Hungary
coordinates: lat: 46.87138889
lon: 17.50416667
They preserve the original surface since the Pliocene period. Protected natural assets. Csobánc is one of the unique and peculiar monadnocks of Tapolca Basin. It is a result of basalt volcanism 3.5 million years ago. Numerous rare habitats in need of protection have been preserved due to the relatively secluded and undisturbed area.

Geographic entities mentioned:
surface_form: csobánc
instance_of: Mountain
countries: Hungary
coordinates: lat: 46.87138889
lon: 17.50416667
Csobánc is one of the unique and peculiar monadnocks of Tapolca Basin. It is a result of basalt volcanism 3.5 million years ago. Numerous rare habitats in need of protection have been preserved due to the relatively secluded and undisturbed area. The natural assets of Csobánc granted the hill increased protection from the Balaton Uplands National Park and the Bakony-Balaton Geopark. Rock grasses.

Geographic entities mentioned:
surface_form: csobánc
instance_of: Mountain
countries: Hungary
coordinates: lat: 46.87138889
lon: 17.50416667
surface_form: balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
surface_form: balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Castle ruins. The castle has been attacked by the Turks between 1554 and 1567. Construction works began in 1255 for the first time. The Italian Rátóti Gyulaffy family owned the castle for more than 40 years. Csobánc fell under numerous unsuccessful Turkish sieges in the 16th century. In 1669 the Esterházy family took control over the castle.

Geographic entities mentioned:
surface_form: csobánc
instance_of: Mountain
countries: Hungary
coordinates: lat: 46.87138889
lon: 17.50416667
The castle was first destroyed in the 18th century. The Foundation for the Castle of Csobánc from the neighbouring village Gyulakeszi makes efforts to reconstruct the ruins of the castle. Cultural and historical programs such as riding shows, mediaeval knights in period dresses, Turkish belly dance etc. are offered to raise fund.

Geographic entities mentioned:
surface_form: csobánc
instance_of: Mountain
countries: Hungary
coordinates: lat: 46.87138889
lon: 17.50416667
Hiking and geocaching are also popular activities around the area. References in literature. Poet - literary historian István Péter NÉMETH from Tapolca wrote several poems and articles on Csobánc, including “Greeting from Csobánc”, and “The Requiem of Csobánc”.

Geographic entities mentioned:
surface_form: csobánc
instance_of: Mountain
countries: Hungary
coordinates: lat: 46.87138889
lon: 17.50416667
surface_form: csobánc
instance_of: Mountain
countries: Hungary
coordinates: lat: 46.87138889
lon: 17.50416667
surface_form: csobánc
instance_of: Mountain
countries: Hungary
coordinates: lat: 46.87138889
lon: 17.50416667
Of the nineteen years spent in Papua more than five of those he lived in Papuan villages. His fieldwork consisted of seven major studies: Vailala (Purari Delta); Orokaiva (Northern Division); Keraki (Morehead River); Koiari (Central Division); Elena (Gulf Division); Foi (Lake Kutubu), and Keveri (Eastern Division) in addition to smaller field studies in about a dozen other societies.

Geographic entities mentioned:
surface_form: Lake Kutubu
instance_of: Lake
countries: Papua New Guinea
coordinates: lat: -6.4
lon: 143.33333333333
Huber Woods Park. Huber Woods Park is a county park located in the community of Locust, Middletown Township, New Jersey. The park, run by the Monmouth County Park System is situated in the Navesink Highlands and is primarily made up of preserved woodland and farmlands formerly owned by the Huber family.

Geographic entities mentioned:
surface_form: Navesink Highlands
instance_of: Mountain
countries: United States
coordinates: lat: 40.3996
lon: -74.0365
The garage of the Huber house, which was turned into a reptile center during the 1990s, was renovated in 2019. Description. The park is situated on a cuesta ridge in the Navesink Highlands, and consists of rolling pasture and woodlands. Although the park in the past was equally divided between pasture and woodlands, today the park is rewilding, and four-fifths of the park has reverted to woodland.

Geographic entities mentioned:
surface_form: Navesink Highlands
instance_of: Mountain
countries: United States
coordinates: lat: 40.3996
lon: -74.0365
&quot;Big Red Machine&quot; is the debut studio album by American musicians Aaron Dessner and Justin Vernon as Big Red Machine. Dessner is most famous for being a founding member, instrumentalist, songwriter, and producer for The National, and Vernon for being the founding member and frontman of Bon Iver. The majority of the album was recorded in Dessner's shed studio in the Hudson Valley.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
After being delayed for about a year in Massawa, Rassam at last received permission from the Emperor to enter his realm. Due to rebellions in Tigray Province, Rassam was forced to follow a circuitous route taking him to Kassala, then to Metemma along the western shore of Lake Tana before finally meeting with Emperor Tewodros in northern Gojjam.

Geographic entities mentioned:
surface_form: Lake Tana
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12
lon: 37.25
Their lands lay within the Yakima Rivers (in Yakama: &quot;Tapteal&quot; – ″rapids″ because of the waterfalls at Prosser, Washington) watershed and for the most part east of the Cascade Range, to the south along the northern tributaries of the Columbia River (in Yakama: &quot;Nch'i-Wána&quot; – ″great river″) (here the Yakama bands frequently lived in bilingual villages together with Southern/Columbia River Sahaptin-speaking bands: Umatilla, Skin-pah/Skin, Tenino/Warm Springs), to the southwest along the Lower Snake River and Columbia River (here the Yakama bands lived also in bilingual villages together with Lower Snake River Sahaptin-speaking local groups of Chamnapam/Chem-na-pum, Wauyukma and Naxiyampam), to the northeast their tribal territories ranged up to the Wenatchee River (because of frequently intermarriages some of the originally Interior Salish-speaking Wenatchi bands switched to Sahaptin as first language), in the north to the lakes of Cle Elum Lake (after the Upper Yakama / Kittitas name &quot;Tie-el-Lum&quot;, meaning &quot;swift water&quot;, referring to the Cle Elum River), Kachess Lake (&quot;more fish&quot;) and Keechelus Lake (&quot;few fish&quot;) at the headwaters of the Yakima River (with the directly northwest living Coast-Salish-speaking Snoqualmie the Yakama bands kept family ties), in the west across the Cascade Range to the headwaters of the Cowlitz River (shch'il), Lewis River ((wl'ɫt'kh) and White Salmon River (where there were also family ties with Coast-Salish-speaking Lower Cowlitz and Upper Chinookan/Kiksht-speaking Wasco-Wishram).

Geographic entities mentioned:
surface_form: Cle Elum Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.282
lon: -121.107
surface_form: Kachess Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.307795
lon: -121.232403
surface_form: Keechelus Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.34777777777778
lon: -121.36888888888889
McBain is best known for originating the phrase &quot;Living Constitution,&quot; the subject of his 1927 book of the same name. He wrote, &quot;However unchanging the form, it is the peculiar virtue of our bills of rights that their substance has changed and is changing.&quot;
He also wrote, &quot;The Constitution of the United States was not handed down on Mount Sinai by the Lord God of Hosts.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
The Army of the Northwest was commanded by Colonel Edward &quot;Alleghany&quot; Johnson and had been ordered to secure a major roadway through the Appalachian Mountains known as the Staunton and Parkersburg Turnpike. Johnson ordered the construction of fortifications and breastworks at a high point along the turnpike on top of Shenandoah Mountain, which is in the U.S.

Geographic entities mentioned:
surface_form: Shenandoah Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5097
lon: -79.1842
Lee to order Johnson to take his forces east to better protect the strategic city of Staunton, as well as the Shenandoah Valley.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Hyperolius frontalis. &quot;Hyperolius frontalis&quot; is a species of frog in the family Hyperoliidae. It is found in the eastern Democratic Republic of the Congo, from northwest of Mount Rwenzori, south to west of Lake Kivu, extending into extreme south-western Uganda in the Bwindi Forest. Common names Bushoho reed frog and white-snouted reed frog have been coined for this species. Description.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
The first phase connecting Guwahati to Mandalay will eventually be extended to Cambodia and Vietnam under Mekong-Ganga Cooperation within the wider framework of Asian Highway Network. This is aimed at creating a new economic zone ranging from Kolkata on the Bay of Bengal to Ho Chi Minh City on the South China Sea. Kaladan Multi-modal Transit Route.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Mountaineering. Six months after the 900-mile walk to Lands End Croucher climbed the Jungfrau and the Mönch mountains in Switzerland and in 1972 he scaled the treacherous west flank of the Eiger. Two years later he also conquered the Matterhorn. He has climbed many other mountains, including peaks in the Himalayas.

Geographic entities mentioned:
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
surface_form: Mönch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.558333333333
lon: 7.9972222222222
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
Mountaineering. Six months after the 900-mile walk to Lands End Croucher climbed the Jungfrau and the Mönch mountains in Switzerland and in 1972 he scaled the treacherous west flank of the Eiger. Two years later he also conquered the Matterhorn. He has climbed many other mountains, including peaks in the Himalayas.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
Dancing Lady Mountain. Dancing Lady Mountain is a summit in Glacier County, Montana, in the United States and it is located within Glacier National Park. Dancing Lady is derived from a Blackfoot-language name. The mountain's former name of Squaw Mountain was changed due to ongoing controversy over the term &quot;squaw&quot;.

Geographic entities mentioned:
surface_form: squaw mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.271944444444
lon: -111.61638888889
Dancing Lady Mountain. Dancing Lady Mountain is a summit in Glacier County, Montana, in the United States and it is located within Glacier National Park. Dancing Lady is derived from a Blackfoot-language name. The mountain's former name of Squaw Mountain was changed due to ongoing controversy over the term &quot;squaw&quot;.

Geographic entities mentioned:
surface_form: lady mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.254156
lon: -112.9668554
surface_form: dancing lady mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.42444444
lon: -113.31166667
Chäserrugg (or &quot;Käserrugg&quot;) is a mountain in Wildhaus-Alt St. Johann municipality, Toggenburg, canton of St. Gallen, Switzerland, rising to 2,262 m. It is the easternmost of the &quot;seven peaks&quot; of the Churfirsten, the other six being, running east to west, Hinterrugg (2,306 m),
Schibenstoll (2,234 m), Zuestoll (2,235 m), Brisi (2,279 m), Frümsel (2,263 m), Selun (2,205 m).

Geographic entities mentioned:
surface_form: Hinterrugg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.153666666667
lon: 9.3048333333333
surface_form: Schibenstoll
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.155
lon: 9.29527778
surface_form: Zuestoll
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.1544
lon: 9.28583
surface_form: Brisi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.153222222222
lon: 9.2773333333333
surface_form: Frümsel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.1525
lon: 9.26555556
surface_form: Selun
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.15277778
lon: 9.25555556
surface_form: frümsel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.1525
lon: 9.26555556
surface_form: hinterrugg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.153666666667
lon: 9.3048333333333
surface_form: brisi
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.153666666667
lon: 9.3048333333333
It is the easternmost of the &quot;seven peaks&quot; of the Churfirsten, the other six being, running east to west, Hinterrugg (2,306 m),
Schibenstoll (2,234 m), Zuestoll (2,235 m), Brisi (2,279 m), Frümsel (2,263 m), Selun (2,205 m). In spite of its being counted among the &quot;seven peaks&quot;, it has a modest prominence of just 14 m, forming part of the ridge ascending to Hinterrugg.

Geographic entities mentioned:
surface_form: Hinterrugg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.153666666667
lon: 9.3048333333333
surface_form: hinterrugg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.153666666667
lon: 9.3048333333333
Chäserrugg. Chäserrugg (or &quot;Käserrugg&quot;) is a mountain in Wildhaus-Alt St. Johann municipality, Toggenburg, canton of St. Gallen, Switzerland, rising to 2,262 m.

Geographic entities mentioned:
surface_form: chäserrugg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.155
lon: 9.3127777777778
The mountain's name translates to &quot;cheesemaker's ridge&quot; and is properly the name of the ridge ascending towards it from the north, beginning at &quot;Ruggschöpf&quot; at about 1,800 m and was only transferred to the &quot;peak&quot; when the &quot;seven Churfirsten&quot; were systematized in the late 19th or early 20th century; in the 19th century, there was also a fashion of etymologizing the name of the Churfirsten range as &quot;Kurfürsten&quot; &quot;prince-electors&quot;, which occasionally inspired a name variant &quot;Kaiserruck&quot; &quot;emperor's back&quot; for Chäserrugg.

Geographic entities mentioned:
surface_form: chäserrugg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.155
lon: 9.3127777777778
While flying the P-51, he scored his first aerial victory on December 5, when he shot down a Focke-Wulf Fw 190 and damaged another Fw 190 northeast of Berlin. On January 14, 1945, 356th FG's P-51s encountered 15 to 20 Fw 190s, southwest of Dümmer Lake. During the aerial battle, Burdick shot down two Fw 190s and damaged another two.

Geographic entities mentioned:
surface_form: Dümmer Lake
instance_of: Lake
countries: Germany
coordinates: lat: 52.5
lon: 8.35
Kaptol, Požega-Slavonia County. Kaptol is a village and a municipality in central Slavonia, Croatia. It is located on the slopes of Papuk mountain, east of Velika and northeast of Požega. In the 2011 census, 97% were Croats.

Geographic entities mentioned:
surface_form: Papuk
instance_of: Mountain
countries: Croatia
coordinates: lat: 45.533333333333
lon: 17.65
Many electrical lines were blown down and a number of roofs were damaged. A tornado touched down near Stratford and numerous funnel clouds were reported. Demise. The bow echo system then crossed over Lake Erie and dissipated over Western Pennsylvania (including metro Pittsburgh) at around 2 A.M. EDT on July 8.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
In 2018, the population of the island was 1,100. The island is very rocky and mountainous. The highest point on the island is the tall mountain Komagaksla on the southern shore of the island. The coastline is very jagged and has numerous fjords that cut inland from the open ocean. The island is surrounded by the Norwegian Sea on the north and the Sørøysundet strait to the south.

Geographic entities mentioned:
surface_form: Komagaksla
instance_of: Mountain
countries: Norway
coordinates: lat: 70.540555555556
lon: 22.881388888889
Khao Chang. Khao Chang (เขาช้าง), is a 45 m high hill in Phang Nga Province, Thailand. It is in Phang Nga town behind city hall. Located within the compound of Wat Phra Paht Phra Chim temple, at the base of a mountain, is &quot;Phung Chang Cave&quot;, also known as 'Elephant Belly Cave.' This cave is notable for its stalactites and stalagmites formations.

Geographic entities mentioned:
surface_form: เขาช้าง
instance_of: Mountain
countries: Thailand
coordinates: lat: 8.4516666666667
lon: 98.517222222222
surface_form: khao chang
instance_of: Mountain
countries: Thailand
coordinates: lat: 8.4516666666667
lon: 98.517222222222
Khao Chang. Khao Chang (เขาช้าง), is a 45 m high hill in Phang Nga Province, Thailand. It is in Phang Nga town behind city hall. Located within the compound of Wat Phra Paht Phra Chim temple, at the base of a mountain, is &quot;Phung Chang Cave&quot;, also known as 'Elephant Belly Cave.' This cave is notable for its stalactites and stalagmites formations.

Geographic entities mentioned:
surface_form: khao chang
instance_of: Mountain
countries: Thailand
coordinates: lat: 8.4516666666667
lon: 98.517222222222
Certain areas of the cave are permanently flooded, but they remain accessible to visitors via boat. Symbolism. In the cultural context of Phang Nga, Khao Chang holds significant symbolic value. Its towering shape resembles a crouched elephant, a feature that has led to its inclusion in the provincial seal of Phang Nga.

Geographic entities mentioned:
surface_form: khao chang
instance_of: Mountain
countries: Thailand
coordinates: lat: 8.4516666666667
lon: 98.517222222222
Velence. Velence is a town in the county of Fejér, Hungary, on the shore of Lake Velence. Its name is the same in Hungarian as that of the Italian city of Venice, though they are suffixed differently: &quot;in Velence&quot; is &quot;Velencén&quot;, while &quot;Velencében&quot; refers to the Italian city (Magyar Angol Nagyszótár, Akadémiai Kiadó. See Hungarian grammar for details).

Geographic entities mentioned:
surface_form: Lake Velence
instance_of: Lake
countries: Hungary
coordinates: lat: 47.208333333333
lon: 18.6
Pointe de Chésery. The Pointe de Chésery is a mountain in the Chablais Alps on the Swiss-French border.

Geographic entities mentioned:
surface_form: pointe de chésery
instance_of: Mountain
countries: Switzerland
France
coordinates: lat: 46.203611111111
lon: 6.8033333333333