Sarmila/GeoWiki-Features huggingface dataset:
Leah Peak is a mountain summit located on the eastern shore of Maligne Lake in Jasper National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Samson Peak, to the north. __NOTOC__
History. Leah Peak was named by Mary Schäffer in her expedition through the area in 1908 to find Maligne Lake. She also named nearby Samson Peak. Leah Beaver was the wife of Samson Beaver.

Geographic entities mentioned:
surface_form: maligne lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.664444444444
lon: -117.53361111111
surface_form: leah peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.71222222222222
lon: -117.55388888888889
Climate. Based on the Köppen climate classification, Leah Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Leah Peak drains west into Maligne Lake, thence into the Maligne River which is a tributary of the Athabasca River.

Geographic entities mentioned:
surface_form: maligne lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.664444444444
lon: -117.53361111111
surface_form: athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
surface_form: athabasca
instance_of: Mountain
countries: Canada
coordinates: lat: 52.18055555555556
lon: -117.20166666666667
surface_form: leah peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.71222222222222
lon: -117.55388888888889
Leah Peak. Leah Peak is a mountain summit located on the eastern shore of Maligne Lake in Jasper National Park, in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Samson Peak, to the north. __NOTOC__
History. Leah Peak was named by Mary Schäffer in her expedition through the area in 1908 to find Maligne Lake. She also named nearby Samson Peak.

Geographic entities mentioned:
surface_form: leah peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.71222222222222
lon: -117.55388888888889
Samson visited the lake with his father at the age of 14, and 16 years later he drew the map from memory when he met Mary at Elliott Barnes' cabin on the Kootenay Plains in the Saskatchewan Valley. The first ascent of Leah Peak was made in 1926 by R. Ecaubert and J. Weber. The mountain's name became official in 1956 by the Geographical Names Board of Canada. Climate.

Geographic entities mentioned:
surface_form: leah peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.71222222222222
lon: -117.55388888888889
The first ascent of Leah Peak was made in 1926 by R. Ecaubert and J. Weber. The mountain's name became official in 1956 by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Leah Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: leah peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.71222222222222
lon: -117.55388888888889
The first ascent of Leah Peak was made in 1926 by R. Ecaubert and J. Weber. The mountain's name became official in 1956 by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Leah Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Ancharius griseus. &quot;Ancharius griseus&quot; is a species of catfish of family Anchariidae. It inhabits the Onilahy River basin of western Madagascar. &quot;A. griseus&quot; reaches about SL.

Geographic entities mentioned:
surface_form: Onilahy River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -23.566666666667
lon: 43.75
List of lakes of Wisconsin. There are over 15,000 lakes in Wisconsin. Of these, about 40 percent have been named. Excluding Lake Michigan and Lake Superior, Lake Winnebago is the largest lake by area, largest by volume and the lake with the longest shoreline. The deepest lake is Wazee Lake, at 350 feet (107 meters). The deepest natural lake is Green Lake, at 237 feet (72 meters).

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
surface_form: Lake Winnebago
instance_of: Lake
countries: United States
coordinates: lat: 44.0169756
lon: -88.4095327
There are over 15,000 lakes in Wisconsin. Of these, about 40 percent have been named. Excluding Lake Michigan and Lake Superior, Lake Winnebago is the largest lake by area, largest by volume and the lake with the longest shoreline. The deepest lake is Wazee Lake, at 350 feet (107 meters). The deepest natural lake is Green Lake, at 237 feet (72 meters). The largest man-made lake is Petenwell Lake.

Geographic entities mentioned:
surface_form: Wazee Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.29
lon: -90.723
After completion of the dam, the river flooded and several smaller lakes rose and became connected as one large lake. The lake lies on the border of Nord-Fron Municipality, Sør-Fron Municipality and Øystre Slidre Municipality. Water enters from the nearby lake Vinstre to the west. The lake sits at an elevation of above sea level.

Geographic entities mentioned:
surface_form: Vinstre
instance_of: Lake
countries: Norway
coordinates: lat: 61.316666666667
lon: 8.9666666666667
The lake is located about southwest of the town of Vinstra and about northeast of the village of Beitostølen. The lake marks the northwestern boundary of Langsua National Park. Names. Since the completion of the dam and the flooding of the area, the new lake has been referred to as &quot;Vinstervatna&quot;, after the nearby lake Vinstre which flows into this lake.

Geographic entities mentioned:
surface_form: Vinstre
instance_of: Lake
countries: Norway
coordinates: lat: 61.316666666667
lon: 8.9666666666667
In rifting, the equivalent structure is a graben, although the bounding faults are normal rather than reverse in type. Examples of this type of basin include the Cul-de-Sac depression in Haiti and Issyk-Kul in the Tian Shan mountains in Kyrgyzstan.

Geographic entities mentioned:
surface_form: Issyk-Kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
It was established in 1943 and its main purpose is for municipal and industrial usage. Location. Churchill Dam lies east-southeast of Kareedouw, south of the path of the Langkloof Valley (R62 road), and on the northern slopes of the Kareedouw Mountains. The dam is 100 km west of Gqeberha, at 34° 00' S, 24° 29' E. Dimension.

Geographic entities mentioned:
surface_form: Langkloof
instance_of: Valley
countries: South Africa
coordinates: lat: -33.825
lon: 23.857777777778
Vicuna Peak. Vicuna Peak, or Vicuña Peak, is a granitic horn located in the North Cascades of southwestern British Columbia, Canada. It is situated northwest of Coquihalla Summit, northeast of Alpaca Peak, and southwest of Guanaco Peak, its nearest higher peak, by a mere one metre.

Geographic entities mentioned:
surface_form: Alpaca Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.6497
lon: -121.1717
surface_form: Guanaco Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.6623
lon: -121.1442
Vicuna Peak. Vicuna Peak, or Vicuña Peak, is a granitic horn located in the North Cascades of southwestern British Columbia, Canada. It is situated northwest of Coquihalla Summit, northeast of Alpaca Peak, and southwest of Guanaco Peak, its nearest higher peak, by a mere one metre.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: vicuna peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.64972
lon: -121.15253
It is situated northwest of Coquihalla Summit, northeast of Alpaca Peak, and southwest of Guanaco Peak, its nearest higher peak, by a mere one metre. Precipitation runoff from the peak drains west into headwaters of the East Anderson River, or east into headwaters of the Coldwater River.

Geographic entities mentioned:
surface_form: coldwater river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.735
lon: -79.6508
surface_form: coldwater river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.4681
lon: -84.7881
Vicuna Peak. Vicuna Peak, or Vicuña Peak, is a granitic horn located in the North Cascades of southwestern British Columbia, Canada. It is situated northwest of Coquihalla Summit, northeast of Alpaca Peak, and southwest of Guanaco Peak, its nearest higher peak, by a mere one metre.

Geographic entities mentioned:
surface_form: vicuna peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.64972
lon: -121.15253
Climate. Based on the Köppen climate classification, Vicuna Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Range where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: vicuna peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.64972
lon: -121.15253
As a result, the Cascade Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for climbing Vicuna Peak.

Geographic entities mentioned:
surface_form: vicuna peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.64972
lon: -121.15253
Precipitation runoff from the peak drains west into headwaters of the East Anderson River, or east into headwaters of the Coldwater River. The mountain was named for the vicuña, as part of the animal names theme for several other nearby peaks that were submitted by Philip Kubik of the 1974 first ascent party.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain was named for the vicuña, as part of the animal names theme for several other nearby peaks that were submitted by Philip Kubik of the 1974 first ascent party. The mountain's name was officially adopted on February 5, 1976, by the Geographical Names Board of Canada. Geology. The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The westernmost and largest of the lakes, Lake Copais, was drained in the 19th century to make way for a large tract of fertile agricultural land, divided into plots. The ancient Bronze-age community on its northwestern shore, Orchomenos, is now a modern city at the edge of the farmland.

Geographic entities mentioned:
surface_form: Lake Copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
surface_form: copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
surface_form: lake copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
The ancient Bronze-age community on its northwestern shore, Orchomenos, is now a modern city at the edge of the farmland. The Cephissos River descending from Phocis to enter Copais has been rerouted through it to enter Lake Yliki from the north. Lake Yliki and Lake Paralimni are part of the water supply of the city of Athens, which houses one-third of the population of Greece.

Geographic entities mentioned:
surface_form: Lake Yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
surface_form: copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
surface_form: yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
surface_form: yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
surface_form: lake yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
surface_form: lake yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
Paralimni, a lake in the NE to SW direction, is locked by mountains for most of its length. Ptoion, a mountain range on its north shore, which separates it from the Gulf of Euboea, descends to the water's edge in slopes and cliffs, especially since the expansion of surface area. If there was once an ancient track, it must have been many feet lower.

Geographic entities mentioned:
surface_form: Ptoion
instance_of: Mountain
countries: Greece
coordinates: lat: 38.48111111
lon: 23.32777778
If there was once an ancient track, it must have been many feet lower. In a similar case, although not quite as severe, are the foothills of Messapio, which come down to a somewhat lesser length on the south side. Today there is not even a mule track, but then, there is no point in one. The main highway to the south leads from the plain of Thebes to the coast through a pass in Messapio.

Geographic entities mentioned:
surface_form: Messapio
instance_of: Mountain
countries: Greece
coordinates: lat: 38.45
lon: 23.45
surface_form: messapio
instance_of: Mountain
countries: Greece
coordinates: lat: 38.45
lon: 23.45
The lakes are unusual in that they were all connected by underground streams called katabothra. These caves, beginning as sinkholes, are a feature of karst, or limestone topography. Limestone erodes easily. Examples of former katabothra can be visited in Copais. Most are on the eastern side. Many are associated with prehistoric settlements.

Geographic entities mentioned:
surface_form: copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
Drainig Copais altered the hydrology. The large amount of flood waters formerly stored by Copais could no longer collect there but must be passed on to Yliki and Paralimni. The elevation of the surface of Yliki having been at now rose to, average figures, with a concomitant increase of surface area from to.

Geographic entities mentioned:
surface_form: copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
surface_form: yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
Topography. Any consideration of the topographic features of the three lakes must take into consideration the draining of Copais and concomitant expansion in depth and area of Yliki and Paralimni. The latter not only erased tracks and roads, and made the land non-arable and unbuildable, but rendered any possible archaeological evidence inaccessible, at least temporarily.

Geographic entities mentioned:
surface_form: copais
instance_of: Lake
countries: Greece
coordinates: lat: 38.45
lon: 23.05
surface_form: yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
The large amount of flood waters formerly stored by Copais could no longer collect there but must be passed on to Yliki and Paralimni. The elevation of the surface of Yliki having been at now rose to, average figures, with a concomitant increase of surface area from to. The surface of Paralimni rose from to with an increase in surface area from to more or less.

Geographic entities mentioned:
surface_form: yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
The surface of Paralimni rose from to with an increase in surface area from to more or less. The east-west length of the lake expanded from to, and the width by. The rise in Lake Yliki at first appeared to be a threat to the geological stability of the region. A canal was planned between Lake Yliki and Paralimni, the Mouriki Channel, and was excavated down to an elevation of.

Geographic entities mentioned:
surface_form: yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
surface_form: lake yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
A canal was planned between Lake Yliki and Paralimni, the Mouriki Channel, and was excavated down to an elevation of. The realization that even in flood the lake level would never rise to that elevation stopped work on the channel, which is visible as a controlled waterway on the Yliki side but in fact dries out further on and does not go through to Paralimni.

Geographic entities mentioned:
surface_form: yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
The realization that even in flood the lake level would never rise to that elevation stopped work on the channel, which is visible as a controlled waterway on the Yliki side but in fact dries out further on and does not go through to Paralimni. During construction on Yliki the main katabothron between the two lakes was blocked. The water levels are now independent.

Geographic entities mentioned:
surface_form: yliki
instance_of: Lake
countries: Greece
coordinates: lat: 38.4
lon: 23.26666667
The Anthedon region to the northeast was isolated on the coast by the mountains enclosing Paralimni. The plain of Thebes extended northward to the bridge between Hyliki and Paralimni, passing first through Mouriki. Ecology of Paralimni. Both Yliki and Paralimni, fringed by wetlands, are home to rare species of fish and birds. They are mainly protected areas.

Geographic entities mentioned:
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
They were basically unaffected by the glaciers of the Pleistocene, or Ice Age, and must have preceded them. So far the only evidence of glaciers in Greece are the cirque features of the Pindus Mountains, of which Parnassus, a purely limestine peak, is an offshoot. Parnassus does have a cave glacier, but that may have developed by ordinary wintering.

Geographic entities mentioned:
surface_form: parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
surface_form: parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
In a similar case, although not quite as severe, are the foothills of Messapio, which come down to a somewhat lesser length on the south side. Today there is not even a mule track, but then, there is no point in one. The main highway to the south leads from the plain of Thebes to the coast through a pass in Messapio. Demography.

Geographic entities mentioned:
surface_form: messapio
instance_of: Mountain
countries: Greece
coordinates: lat: 38.45
lon: 23.45
Lake Paralimni. Lake Paralimni (, &quot;Limne Paralimni&quot;, Latinised as &quot;Lacus Paralimnus&quot;), formerly named Lake Ougria, Latinized to Uggria, is the easternmost of an east-west sequence of three ancient lakes in Central Greece that divided the mountains of Phocis from the plains of southern Boeotia on the east and the northern plains of Boeotia from the southern on the west.

Geographic entities mentioned:
surface_form: lake ougria
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
surface_form: lake paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
surface_form: ougria
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
Lake Paralimni. Lake Paralimni (, &quot;Limne Paralimni&quot;, Latinised as &quot;Lacus Paralimnus&quot;), formerly named Lake Ougria, Latinized to Uggria, is the easternmost of an east-west sequence of three ancient lakes in Central Greece that divided the mountains of Phocis from the plains of southern Boeotia on the east and the northern plains of Boeotia from the southern on the west.

Geographic entities mentioned:
surface_form: lake paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
The locality is called Palaiometochi, within the village of Pyrgos (termed Paralimni Pyrgos by Farinetti to distinguish it from all the other villages of that name). It seems clear that first, the three-lakes region was settled anciently, before the arrival of the Greeks, and second, that an ancient road along the south shore of Paralimni connected all the villages.

Geographic entities mentioned:
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
The Cephissos River descending from Phocis to enter Copais has been rerouted through it to enter Lake Yliki from the north. Lake Yliki and Lake Paralimni are part of the water supply of the city of Athens, which houses one-third of the population of Greece. Hydrology of the three lakes. The three lakes were never connected by surface channels. They each settled into their own distinct beds.

Geographic entities mentioned:
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
The three lakes were never connected by surface channels. They each settled into their own distinct beds. Significant bridges of hilly terrain separate them, and divide Paralimni from the Gulf of Euboea. The lakes are unusual in that they were all connected by underground streams called katabothra. These caves, beginning as sinkholes, are a feature of karst, or limestone topography.

Geographic entities mentioned:
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
Paralimni was left hanging independently over the Gulf of Euboea. The separating land bridge is across, elevation. One artificial tunnel replaces the former katabothron, now blocked, connecting Paralimni with the Gulf. It is high up and serves to drain the lake when the water level becomes high. The connection of both lakes to the Athens aqueduct solved all the hydrologic problems.

Geographic entities mentioned:
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
It includes the walled Homeric city of Anthedon. Closer to the lake was a settlement now unknown with an acropolis also dating to the Neolithic. The locality is called Palaiometochi, within the village of Pyrgos (termed Paralimni Pyrgos by Farinetti to distinguish it from all the other villages of that name).

Geographic entities mentioned:
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
It seems clear that first, the three-lakes region was settled anciently, before the arrival of the Greeks, and second, that an ancient road along the south shore of Paralimni connected all the villages. The west end of Lake Paralimni merges into the plain of Thebes. The mountains of Boeotia divide it into clusters of towns within which communication was easy, but outside of which, not.

Geographic entities mentioned:
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
The Copais region to the northwest was under the domination of Orchomenos. The Anthedon region to the northeast was isolated on the coast by the mountains enclosing Paralimni. The plain of Thebes extended northward to the bridge between Hyliki and Paralimni, passing first through Mouriki. Ecology of Paralimni.

Geographic entities mentioned:
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
The Copais region to the northwest was under the domination of Orchomenos. The Anthedon region to the northeast was isolated on the coast by the mountains enclosing Paralimni. The plain of Thebes extended northward to the bridge between Hyliki and Paralimni, passing first through Mouriki. Ecology of Paralimni.

Geographic entities mentioned:
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
surface_form: paralimni
instance_of: Lake
countries: Greece
coordinates: lat: 38.4603
lon: 23.3516
Season one. The first season of 6 episodes of 60 minutes each, released in 1984, was directed by Damiano Damiani and scored by Riz Ortolani. The episodes were filmed at locations in Rome and the Sicilian city of Trapani, and the scenes in the mountains and on the lake were shot in Horgen and Lake Geneva, Switzerland.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
In 2012, ACCO Brands merged with MeadWestvaco, which also had other personal organizer products, including At-A-Glance and Day Runner; to eliminate redundancies, corporate heads decided to shut down Day-Timers' historical Lehigh Valley-based headquarters, leading to the loss of 300 jobs there, and shifted Day-Timer product operations to corporate facilities in New York, Ohio, and Illinois.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
This was another blow to the Lehigh Valley economy, which had previously undergone major factory closings from Mack Trucks, Ingersoll Rand, and other historically Lehigh Valley-based companies. The market for paper-based personal organizers and calendars remains, and Day-Timer continue to publish these products.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Newnata, Arkansas. Newnata is an unincorporated community in Stone County, Arkansas, United States. It is in the Ozark Mountains region of the northern part of the state and is near the town of Mountain View. Overview.

Geographic entities mentioned:
surface_form: Ozark Mountains
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
The monastery is currently under renovation. Queen Catherine of Bosnia sought refuge from the Ottomans in Kozograd, royal summer-residence in the mountains near Fojnica at the time, before making her way to Rome. Fojnica also has a spa center with thermal water, Reumal Fojnica. The Prokoško Lake is located in the west of the municipality.

Geographic entities mentioned:
surface_form: Prokoško Lake
instance_of: Lake
countries: Bosnia and Herzegovina
coordinates: lat: 43.95722222
lon: 17.75472222
But it unfolds smoothly, thanks to Greg Chwerchak's focused direction. And the water down on Barnegat Inlet Island looks oddly idyllic on film. &quot;Greetings From the Shore&quot; is well-acted, including by newcomer Shaw, who has an appealing, wide-eyed innocence reminiscent of a young Meg Ryan. This is a two-hankie weeper that doesn't really earn its tears.

Geographic entities mentioned:
surface_form: Barnegat Inlet
instance_of: Landform
countries: United States
coordinates: lat: 39.76666667
lon: -74.10333333
Thomas's son Siophanes is resurrected and returns with tales of heavenly geography he traveled while dead; the astonished denizens of the city convert en masse, and Thomas makes Siophanes their bishop. Thomas travels back to the Mount of Olives via cloud, and re-enacts the story of Doubting Thomas where he demands to see the risen Jesus and touch his wounds.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
The Autumn&quot;, &quot;Evening sun&quot;, &quot;Landscape&quot; by Nikolai Timkov, &quot;Gurzuf&quot; by Mikhail Trufanov, &quot;Spring in Turkmenistan&quot; by Mikhail Trufanov, &quot;Evening&quot;, &quot;A Winter&quot;, &quot;Venice&quot; by Boris Ugarov, &quot;Autumn&quot;, &quot;Street in Staraya Ladoga&quot;, &quot;Last snow&quot;, &quot;Staraya Ladoga&quot; by Ivan Varichev, &quot;Spring on the Angara River&quot; by Anatoli Vasiliev, &quot;Volkhov River&quot;, &quot;Flowering Bird Cherry&quot;, &quot;Winter window&quot;, &quot;Twilight&quot; by Vecheslav Zagonek, &quot;October in Crimea&quot;, &quot;Lake Ritsa&quot;, &quot;Early spring&quot; by Elena Zhukova, and others.

Geographic entities mentioned:
surface_form: Lake Ritsa
instance_of: Lake
countries: Georgia
Republic of Abkhazia
coordinates: lat: 43.4811
lon: 40.5415
History. Turlough Hill was first conceived by Dermot O'Riordan, Deputy Chief Engineer in the ESB's Civil Engineering Department. In 1964, ESB engineers visited several locations in the Wicklow Mountains, digging trial pits and boreholes, looking for suitable sites for a pumped-storage station.

Geographic entities mentioned:
surface_form: Turlough Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.0242
lon: -6.41639
A shortlist of three proposals was drawn up by O'Riordan: an artificial upper reservoir at the summit of Tonduff mountain with an artificial lower reservoir in the Glencree valley; an upper reservoir using Lough Ouler, a natural corrie lake near the summit of Tonelagee mountain, with an artificial lower reservoir in the Glenmacnass valley; and an artificial upper reservoir at Turlough Hill with Lough Nahanagan as lower reservoir.

Geographic entities mentioned:
surface_form: Glencree
instance_of: Valley
countries: Ireland
coordinates: lat: 53.17
lon: -6.23
surface_form: Tonelagee
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.053605555556
lon: -6.3821722222222
Chile Route 27. Chile Route 27 (Ruta 27 CH) is a main road in the northern portion of Chile. It runs from San Pedro de Atacama to Paso de Jama. A short road off Route 27 heads north to Portezuelo del Cajón. Another adjacent road leads to Llano de Chajnantor Observatory, reaching maximum altitude of.

Geographic entities mentioned:
surface_form: Paso de Jama
instance_of: Mountain
countries: Chile
coordinates: lat: -23.2375
lon: -67.07638889
Copadichromis sp. 'Virginalis Kajose'. &quot;Copadichromis&quot; sp. 'Virginalis Kajose' is a formally undescribed species of freshwater fish in the family Cichlidae. It is found in Malawi, Mozambique, and Tanzania, primarily in Lake Malawi. It is also present in the adjoining, extremely shallow and recently formed Lake Malombe.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
It is found in Malawi, Mozambique, and Tanzania, primarily in Lake Malawi. It is also present in the adjoining, extremely shallow and recently formed Lake Malombe. It is abundant in parts of Lake Malawi and in Lake Malombe as well, in shallow waters, and has been a regionally important species for fisheries in both lakes.

Geographic entities mentioned:
surface_form: Lake Malombe
instance_of: Lake
countries: Malawi
coordinates: lat: -14.666666666667
lon: 35.25
The species grows in all the mountainous part of California including the North Coast, the Klamath Ranges, the north and south Coast Ranges, in the Sierra Nevada, the Transverse Ranges, and even in the Warner Mountains and the White Mountains. The southernmost known population is on Mount Pinos in California.

Geographic entities mentioned:
surface_form: Mount Pinos
instance_of: Mountain
countries: United States
coordinates: lat: 34.8116
lon: -119.147
Channel 23 began transmitting on September 9, 1988. In January 1990 they installed a transmitter with 1000 watts in the Irazú volcano. In 1991 a trademark was filed for the name Enlace. In 1992, Channel 23 installed three repeaters in Limón, Santa Elena and Cerro de la Muerte.

Geographic entities mentioned:
surface_form: Cerro de la Muerte
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 9.56666667
lon: -83.75
Stewart formally announced on May 31, 2023, that he intended to resign from Congress to focus on helping take care of his wife's health issues. He resigned on September 15. Early life and education. Stewart was born in Logan, Utah, and grew up on a dairy farm in Cache Valley. His father was a retired Air Force pilot and teacher. His mother, Sybil S.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667
Loch of Mey. Loch of Mey is a loch near the north coast of Caithness, Scotland, and one of the most northern water features of mainland Britain. It lies just to the south of Skarfskerry, and southwest of Harrow.

Geographic entities mentioned:
surface_form: loch of mey
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.6444
lon: -3.25722
This portion of the trail is on private property, so permission is required to visit. Lake De Smet. Lake De Smet occupies a natural undrained basin on the divide between Piney Creek, and one of its tributaries, Boxelder Creek. It is one of several basins in the Buffalo area that were formed by coal seam fires.

Geographic entities mentioned:
surface_form: Lake De Smet
instance_of: Lake
countries: United States
coordinates: lat: 44.478611111111
lon: -106.75222222222
Kongur Glacier. Kongur Glacier (,) is a long glacier draining the northwest slopes of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated northeast of Dalgopol Glacier and southwest of Saparevo Glacier, and flows west of Mount Christi into Drake Passage. Bulgarian early mapping in 2009.

Geographic entities mentioned:
surface_form: Mount Christi
instance_of: Mountain
coordinates: lat: -62.909277777778
lon: -62.400277777778
Location. The falls are located in the lower part of the Reichenbachtal, on the Rychenbach, a tributary (from the south bank) of the Aare. They are some south of the town of Meiringen, and Interlaken. Politically, the falls are within the municipality of Schattenhalb in the canton of Bern. The falls are made accessible by the Reichenbach Funicular.

Geographic entities mentioned:
surface_form: Reichenbachtal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.6799
lon: 8.1494
The majority of the local place names were derived from the Munsee-Lenape, however; places like &quot;Lock-ah Hanna&quot; (Lackawanna or Sand River), &quot;Tunk Hanna Unk&quot; (Tunkhannock or Bend River Place), &quot;Why-ohm Ing&quot; (Wyoming or Food Place), &quot;Min Nees Unk&quot; (Minisink), &quot;Toe-be Hanna&quot; (Tobyhanna or Cool River), &quot;Mesh-op Ing&quot; (Meshoppen), &quot;Why-ah-loose Ing&quot; (Wyalusing), &quot;Schick-shin Ing&quot; (Shickshinny), and &quot;Mawsch Unk&quot; (Bear Place, present-day Jim Thorpe) are examples.

Geographic entities mentioned:
surface_form: Wyoming
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
These settlements eventually led to armed conflict with the Penn proprietors (William Penn's sons, Richard and Thomas, and his grandson, John), who also claimed the land. (See Pennamite Wars). During the American Revolution in 1778, a combined British, Tory, Iroquois, Munsee, and Lenape force attacked the Wyoming Valley settlers on the eastern edge of this region, and killed many of the settlers.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
In the meantime, the Koch fleet occupied Sala and Makaland and proceeded to Dikhowmukh. At several engagements, the Ahoms were routed. The Ahom king alarmed by the continuous setback, took flight for Charaikhorong in Naga Hills. This demoralized the common people, including many nobles and some Ahom princes joined the Koches. Meanwhile, Garhgaon (&quot;the Ahom capital&quot;) was also occupied.

Geographic entities mentioned:
surface_form: Naga Hills
instance_of: Mountain
countries: Myanmar
India
coordinates: lat: 26
lon: 95
Mount Agamenticus. Mount Agamenticus is a high monadnock in the town of York, Maine. The area surrounding the summit is a park reservation which provides habitat for wildlife and a venue for recreation. The greater Agamenticus region covers nearly in the southern Maine towns of Eliot, Ogunquit, South Berwick, Wells and York.

Geographic entities mentioned:
surface_form: mount agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
surface_form: agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
Mount Agamenticus is a high monadnock in the town of York, Maine. The area surrounding the summit is a park reservation which provides habitat for wildlife and a venue for recreation. The greater Agamenticus region covers nearly in the southern Maine towns of Eliot, Ogunquit, South Berwick, Wells and York. Though under high, Mount Agamenticus was historically a noted landmark for sailors.

Geographic entities mentioned:
surface_form: mount agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
surface_form: agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
Though under high, Mount Agamenticus was historically a noted landmark for sailors. Mount Agamenticus is also affectionately known by older locals as &quot;Big A,&quot; the nickname of a ski slope that once operated on its northeast flank, remnants of which can be seen both near the summit and along the trails. A memorial cairn to Mi'kmaq chief St.

Geographic entities mentioned:
surface_form: mount agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
surface_form: agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
Aspinquid (St. Aspenquid) was an alleged Mi'kmaq sachem around whom little is known, including whether he ever even existed. He allegedly was murdered in 1696 and was declared a martyr and buried atop Mount Agamenticus. According to legend, Saint Aspinquid (sometimes &quot;Aspenquid&quot;) was born in May 1588, and after converting to Christianity, spread the gospel to tribes across the continent.

Geographic entities mentioned:
surface_form: mount agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
surface_form: agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
Mount Agamenticus is a high monadnock in the town of York, Maine. The area surrounding the summit is a park reservation which provides habitat for wildlife and a venue for recreation. The greater Agamenticus region covers nearly in the southern Maine towns of Eliot, Ogunquit, South Berwick, Wells and York. Though under high, Mount Agamenticus was historically a noted landmark for sailors.

Geographic entities mentioned:
surface_form: agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
On paper, the mountain's Indian name, &quot;Sassanows,&quot; became &quot;Snadoun Hill.&quot; But many royal recommendations were not retained. Instead, the mountain would assume the general name of the York settlement of 1630, the &quot;Plantation of Agamenticus,&quot; which itself took the Abenaki name for the York River. Plantation of Agamenticus.

Geographic entities mentioned:
surface_form: agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
surface_form: agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
surface_form: agamenticus
instance_of: Mountain
countries: United States
coordinates: lat: 43.223055555556
lon: -70.691944444444
Equestrian statue of Philip Sheridan (Washington, D.C.). &quot;General Philip Sheridan&quot; is a bronze sculpture that honors Civil War general Philip Sheridan. The monument was sculpted by Gutzon Borglum, best known for his design of Mount Rushmore.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
At the behest of Irene, on July 2, 1907, Borglum received a contract to sculpt the memorial. He was a Danish American artist who was greatly influenced by French sculptor Auguste Rodin. Borglum is best known for his carvings at Mount Rushmore and Stone Mountain. The Sheridan sculpture is his only equestrian monument in Washington, D.C.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
surface_form: Stone Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
Most of the inhabitants in Ugunja are Luos. Ugunja is located on the Kisumu-Busia highway, which links Kenya and Uganda. Ugunja town is 72 km north of the nearest city, Kisumu, which sits on the shores of Lake Victoria. The equator is 40 km south of Ugunja town. Rural residents of Ugunja mainly depend on agriculture as their main source of food and income.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
The Clearwater River flows to the west, Raft River to the east, Spahats Creek to the north, and North Thompson River to the south. Raft Mountain is part of the Shuswap Highland. There are five summits in the group and the highest is. Trophy Mountain is the closest summit to the north. Access. The Raft West and Raft Peak Forest Service Roads provide access to the south side of the mountain.

Geographic entities mentioned:
surface_form: Trophy Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7997
lon: -119.876
Raft Mountain. Raft Mountain is a mountain in east-central British Columbia, Canada, located north-east of Clearwater and just outside the south boundary of Wells Gray Provincial Park. The Clearwater River flows to the west, Raft River to the east, Spahats Creek to the north, and North Thompson River to the south. Raft Mountain is part of the Shuswap Highland.

Geographic entities mentioned:
surface_form: raft mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7278
lon: -119.861
Raft Mountain. Raft Mountain is a mountain in east-central British Columbia, Canada, located north-east of Clearwater and just outside the south boundary of Wells Gray Provincial Park. The Clearwater River flows to the west, Raft River to the east, Spahats Creek to the north, and North Thompson River to the south. Raft Mountain is part of the Shuswap Highland.

Geographic entities mentioned:
surface_form: raft mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7278
lon: -119.861
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The Clearwater River flows to the west, Raft River to the east, Spahats Creek to the north, and North Thompson River to the south. Raft Mountain is part of the Shuswap Highland. There are five summits in the group and the highest is. Trophy Mountain is the closest summit to the north. Access. The Raft West and Raft Peak Forest Service Roads provide access to the south side of the mountain.

Geographic entities mentioned:
surface_form: raft mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7278
lon: -119.861
A hike of about 2.5 hours goes up the meadows to the west ridge, then to the summit. An all-day hike crosses the five summits. The north face of Raft Mountain can be reached via Spahats Creek Road which turns east off Clearwater Valley Road (also called Wells Gray Park Road). A good clearance vehicle is recommended, but four-wheel drive should not be necessary.

Geographic entities mentioned:
surface_form: raft mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7278
lon: -119.861
After, watch for the sign &quot;Cirque of Tarns Trail&quot; at the pass. The trail was rebuilt in 2023 and several sections of boardwalk were added by BC Parks. The 2.3 km long trail bypasses Caligata Lake and ends below the Raft Mountain cliffs. Cross-country hiking routes lead from there to the nearby Cirque of Tarns.

Geographic entities mentioned:
surface_form: raft mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7278
lon: -119.861
Cross-country hiking routes lead from there to the nearby Cirque of Tarns. A more rigorous hike ascends to the east ridge of Raft Mountain from where a skyline walk can go in either direction to Raft's multiple summits. Road and hiking directions for both routes are essential and can be found in &quot;Exploring Wells Gray Park&quot; (7th edition).

Geographic entities mentioned:
surface_form: raft mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7278
lon: -119.861
Road and hiking directions for both routes are essential and can be found in &quot;Exploring Wells Gray Park&quot; (7th edition). Groomed cross-country ski trails are located on the lower slopes of Raft Mountain and are maintained by the Wells Gray Outdoors Club. A network of snowmobile trails on Raft Mountain is maintained by the Clearwater Sno-Drifters Club.

Geographic entities mentioned:
surface_form: raft mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7278
lon: -119.861
Groomed cross-country ski trails are located on the lower slopes of Raft Mountain and are maintained by the Wells Gray Outdoors Club. A network of snowmobile trails on Raft Mountain is maintained by the Clearwater Sno-Drifters Club. The group also operates two warming huts near treeline. Naming. The Overlanders expedition to the Cariboo goldfields rafted down the North Thompson River in 1862.

Geographic entities mentioned:
surface_form: raft mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7278
lon: -119.861
elliptica&quot;. The specific epithet (&quot;elliptica&quot;) refers to the shape of the fruit as described by Blakely and McKie. Distribution and habitat. &quot;Eucalyptus elliptica&quot; grows in grassy woodland between the Barrington Tops area and southeastern Queensland, most often in the Bendemeer and Walcha areas.

Geographic entities mentioned:
surface_form: Barrington Tops
instance_of: Landform
countries: Australia
coordinates: lat: -31.94998
lon: 151.52687
By the early 20th century, gold was mined in alluvial deposits spread over the island. At the same time, antimony, copper, iron and tin were thought to be abundant, in addition to asphalt, coal, and petroleum. Deposits of alluvial gold were found in the valley of the Ampoasary River, a tributary of the Mananjary River, about east of Ambositra.

Geographic entities mentioned:
surface_form: Mananjary River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -21.256944444444443
lon: 48.34444444444445
Brent Knoll. Brent Knoll is a hill on the Somerset Levels, in Somerset, England. It is located roughly halfway between Weston-super-Mare and Bridgwater, from the Bristol Channel coast at Burnham-on-Sea. At the foot of the hill are two villages East Brent and Brent Knoll, which takes its name from the hill but was previously called South Brent.

Geographic entities mentioned:
surface_form: brent knoll
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.254
lon: -2.946
Another possibility is that the name of Brent simply derives from the local river, the Brent, which gives its name to a Somerset hundred. Geology. An isolated hill, Brent Knoll is an example of denudation – waters of the Bristol Channel eroded surrounding features leaving just the Blue Lias rocks from the Jurassic period capped with Midford Sands of the Bridport Formation. Travel.

Geographic entities mentioned:
surface_form: brent knoll
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.254
lon: -2.946