Sarmila/GeoWiki-Features huggingface dataset:
(Phoenix was settled shortly afterward, by 1867–68.) The two settlements were 'Hayden's Ferry', named after a ferry service operated by Charles T. Hayden, and 'San Pablo', and were located west and east of Hayden Butte respectively. The ferry became the key river crossing in the area.

Geographic entities mentioned:
surface_form: Hayden Butte
instance_of: Mountain
countries: United States
coordinates: lat: 33.428175
lon: -111.93611111111
The ferry became the key river crossing in the area. The Tempe Irrigating Canal Company was soon established by William Kirkland and James McKinney to provide water for alfalfa, wheat, barley, oats, and cotton. Pioneer Darrell Duppa is credited with suggesting Tempe's name, adopted in 1879, after comparing the Salt River valley near a -tall butte, to the Vale of Tempe near Mount Olympus in Greece.

Geographic entities mentioned:
surface_form: Vale of Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Tempe is generally flat, except for Tempe Butte or Hayden Butte (generally known as A-Mountain for Arizona State University's &quot;A&quot; logo located on its south face), located next to Sun Devil Stadium, Twin Buttes and Bell Butte on the western edge of Tempe, and the buttes within Papago Park at northwest corner of Tempe. Elevation ranges from at Tempe Town Lake to atop Hayden Butte. Climate.

Geographic entities mentioned:
surface_form: Tempe Butte
instance_of: Mountain
countries: United States
coordinates: lat: 33.428175
lon: -111.93611111111
surface_form: Papago Park
instance_of: Landform
countries: United States
coordinates: lat: 33.451889
lon: -111.944361
The City of Tempe estimated that 2.7 million people visited the lake in 2013. Papago Park and Tempe Butte Desert Preserves offer hiking, mountain and road biking, rock climbing, disc golf, and equestrian activities. Tempe is also home to the annual Ironman Triathlon, which takes place in late November.

Geographic entities mentioned:
surface_form: Papago Park
instance_of: Landform
countries: United States
coordinates: lat: 33.451889
lon: -111.944361
surface_form: Tempe Butte
instance_of: Mountain
countries: United States
coordinates: lat: 33.428175
lon: -111.93611111111
Tempe is also home to the annual Ironman Triathlon, which takes place in late November. Tempe has more than 50 neighborhood and community parks, including Kiwanis Park, Tempe Beach Park and Tempe Sports Complex. Kiwanis Park contains Kiwanis Lake, the only indoor wave pool in the Phoenix area, a gymnasium, a batting range, tennis courts, a fitness center, and classroom programs. Government.

Geographic entities mentioned:
surface_form: Kiwanis Lake
instance_of: Lake
countries: United States
coordinates: lat: 33.373905555556
lon: -111.93901111111
SS Norman. The &quot;Norman&quot; was a bulk freighter; its wreck in Lake Huron (also designated 20UH018) was listed on the National Register of Historic Places in 2016. Description. The &quot;Norman&quot; had an overall length of 296.5 feet, a 40.4 foot beam, 21 foot hold depth, and a gross tonnage of 2,304 tons.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
While the Portolá expedition was exploring Alta California, they arrived at San Carpóforo Canyon near present-day San Simeon on September 13, 1769. Unable to penetrate the difficult terrain along the coast, they detoured inland through the San Antonio and Salinas Valleys before arriving at Monterey Bay, where they founded Monterey and named it the provincial capital.

Geographic entities mentioned:
surface_form: Salinas Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.7654
lon: -121.7918
Frank A. Perret. Frank Alvord Perret (2 August 1867 in Hartford, Connecticut &ndash; January 12, 1943 in New York City) was an American entrepreneur, inventor, and volcanologist, who was particularly well known for his studies of eruptions of Vesuvius, Kilauea and Mount Pelée. Career as an Engineer.

Geographic entities mentioned:
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
The station was the forerunner of the Hawaiian Volcano Observatory, which was built by Thomas Jaggar the following year. When Mount Pelée on the French Caribbean island of Martinique became active again in 1929, some years after the devastating eruption of 1902 Perret was one of the first scientists on site.

Geographic entities mentioned:
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
The abdomen is whitish and unmarked. Dark bands are present on the caudal fin. Potentially misidentified species. Several species of puffers inhabit the waters of the &quot;Indian River Lagoon&quot; (IRL). In addition to &quot;S. testudineus&quot;, three other Florida puffer species belong to the genus &quot;Sphoeroides&quot; are found in the IRL. These include: the northern puffer, &quot;S.

Geographic entities mentioned:
surface_form: Indian River Lagoon
instance_of: Body of water
countries: United States
coordinates: lat: 28.05527778
lon: -80.57611111
Having become colonel on 31 March 1915, towards the end of April he assumed command of the 4th Infantry Regiment &quot;Piemonte&quot; of the &quot;Piemonte&quot; Infantry Brigade, which shortly before the declaration of war on the Austro-Hungarian Empire was deployed in the Fella sector, in Carnia.

Geographic entities mentioned:
surface_form: Carnia
instance_of: Valley
countries: Italy
coordinates: lat: 46.39444444
lon: 12.77416667
Later in 1993, a stretch of 3 km from Mevaram to Ayathil was completed and 1.5 km Ayathil-Kallumthazham stretch was completed in 1999 and the remaining Kallumthazham-Kavanad stretch completed in 2019. This stretch includes three bridges, five culverts, one vehicle underpass, and five major intersections, and needs to pass over the Ashtamudi Lake.

Geographic entities mentioned:
surface_form: Ashtamudi Lake
instance_of: Lake
countries: India
coordinates: lat: 8.9833333333333
lon: 76.6
In 2007 a Holland Marsh Drainage System Joint Municipal Board was created in response to a crisis of maintenance of the Holland Marsh Drainage System. The Holland River flows through the middle of the southernmost Holland Marsh polder and eventually flows out to Lake Simcoe. Geographically, the area is north of the Oak Ridges Moraine.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
In 2007 a Holland Marsh Drainage System Joint Municipal Board was created in response to a crisis of maintenance of the Holland Marsh Drainage System. The Holland River flows through the middle of the southernmost Holland Marsh polder and eventually flows out to Lake Simcoe. Geographically, the area is north of the Oak Ridges Moraine.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Croatia's Goran Ivanišević and Goran Prpić and Argentina's Javier Frana and Christian Miniussi won the bronze medals, which were both countries' first medals in the event. The tournament was held at the Vall d'Hebron complex on Montjuïc, Barcelona, Spain from 30 July to 7 August 1992.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
The name of New Year Lake was changed into Crook's Lake in the Geographic Names Information System (GNIS) in 1966 after a local rancher sent a note to the Board on Geographic Names, in which he wrote that the lake was called &quot;Crooks Lake&quot; ever since a battle took place in 1867 near the lake between General George Crook and the Northern Paiute.

Geographic entities mentioned:
surface_form: battle
instance_of: Watercourse
countries: United States
coordinates: lat: 44.9266
lon: -93.0291
surface_form: new year lake
instance_of: Lake
countries: United States
coordinates: lat: 41.753806
lon: -119.950447
New Year Lake. New Year Lake is a lake in the Hays Canyon Range of northwestern Washoe County, Nevada, US, at elevation. Explorer John C. Frémont passed New Year Lake on December 26, 1843 during his second expedition; it was included, unnamed, on the map he created after the expedition in 1845.

Geographic entities mentioned:
surface_form: new year lake
instance_of: Lake
countries: United States
coordinates: lat: 41.753806
lon: -119.950447
The name change was reversed in 1989 because the name &quot;New Year Lake&quot; was used historically. &quot;Crooks Lake&quot; is listed as a variant name together with Roops Lake.

Geographic entities mentioned:
surface_form: new year lake
instance_of: Lake
countries: United States
coordinates: lat: 41.753806
lon: -119.950447
Cold Pike. Cold Pike is a fell in the English Lake District. It is a satellite of Crinkle Crags and stands above the Upper Duddon Valley. Topography. When travelling clockwise, Crinkle Crags is the last of the high cirque of fells forming the head of upper Eskdale. It sends out a trio of ridges to the south, running parallel like the prongs of a trident.

Geographic entities mentioned:
surface_form: Duddon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
It sends out a trio of ridges to the south, running parallel like the prongs of a trident. Working from the west these ridges culminate in Hard Knott, Little Stand and Cold Pike. The Cold Pike ridge begins indistinctly in an area of rocky knolls and small tarns beneath the Fifth Crinkle.

Geographic entities mentioned:
surface_form: Hard Knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.410539
lon: -3.186436
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
To the east across a wide low col is Pike of Blisco, a conical fell with its footing firmly in Langdale. The source of the River Duddon flows south from this col, curving westward around the foot of Wrynose Breast. To the north is Red Tarn, a feeder via Oxendale of Great Langdale Beck. Red Tarn is an elongated pool whose stony bed can be seen through clear shallow waters, reputed to hold trout.

Geographic entities mentioned:
surface_form: Great Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
surface_form: red tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.528333333333
lon: -3.0086111111111
Each has a cairn, the highest being a fine example. The top is an excellent place from which to survey Crinkle Crags, the Langdale Pikes, and the northern end of the Coniston Fells across Wrynose Bottom; there is a fine distant prospect of the Pennines above Windermere, and Morecambe Bay above the Duddon Valley. Ascents.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
surface_form: Duddon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
Cold Pike can be reached easily via Red Tarn from the carpark at the summit of Wrynose Pass. It can also be climbed (less easily) from Great Langdale. More ‘honest’ walkers beginning in the south may wish to start from Little Langdale or Wrynose Bottom, first ascending Wrynose Pass. A direct route from Wrynose Bottom is also possible although pathless, skirting around the left of the crags.

Geographic entities mentioned:
surface_form: Little Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
Beyond the summit the ridge continues for another south eastward before falling steeply over the many tiered crags of Wrynose Breast. Wrynose Breast stands above the nascent Duddon and the Wrynose Pass road, which provides the only vehicular link between central Lakeland and the Duddon Valley.

Geographic entities mentioned:
surface_form: duddon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: duddon valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
To the west of Cold Pike is the Gaitscale Beck, the watercourse separating it from Little Stand. To the east across a wide low col is Pike of Blisco, a conical fell with its footing firmly in Langdale. The source of the River Duddon flows south from this col, curving westward around the foot of Wrynose Breast. To the north is Red Tarn, a feeder via Oxendale of Great Langdale Beck.

Geographic entities mentioned:
surface_form: duddon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: river duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
A direct route from Wrynose Bottom is also possible although pathless, skirting around the left of the crags. A consideration here is that the Duddon will need to be forded when starting out. Cold Pike is often seen as a worthwhile detour &quot;en route&quot; to Crinkle Crags.

Geographic entities mentioned:
surface_form: duddon
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.297688888889
lon: -3.2347888888889
surface_form: duddon
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 54.4155
lon: -3.1156
The Cold Pike ridge begins indistinctly in an area of rocky knolls and small tarns beneath the Fifth Crinkle. Gradually gaining definition it descends to a broad grassy saddle before rising again to the summit plateau of Cold Pike. To the north of the saddle is Great Knott at. This top is considered by most guidebooks to be a subsidiary of Crinkle Crags rather than the nearer Cold Pike.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: the saddle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.162395
lon: -5.414721
To the west of Cold Pike is the Gaitscale Beck, the watercourse separating it from Little Stand. To the east across a wide low col is Pike of Blisco, a conical fell with its footing firmly in Langdale. The source of the River Duddon flows south from this col, curving westward around the foot of Wrynose Breast. To the north is Red Tarn, a feeder via Oxendale of Great Langdale Beck.

Geographic entities mentioned:
surface_form: pike of blisco
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.427980555556
lon: -3.1251888888889
It is a satellite of Crinkle Crags and stands above the Upper Duddon Valley. Topography. When travelling clockwise, Crinkle Crags is the last of the high cirque of fells forming the head of upper Eskdale. It sends out a trio of ridges to the south, running parallel like the prongs of a trident. Working from the west these ridges culminate in Hard Knott, Little Stand and Cold Pike.

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
Cold Pike. Cold Pike is a fell in the English Lake District. It is a satellite of Crinkle Crags and stands above the Upper Duddon Valley. Topography. When travelling clockwise, Crinkle Crags is the last of the high cirque of fells forming the head of upper Eskdale. It sends out a trio of ridges to the south, running parallel like the prongs of a trident.

Geographic entities mentioned:
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
Working from the west these ridges culminate in Hard Knott, Little Stand and Cold Pike. The Cold Pike ridge begins indistinctly in an area of rocky knolls and small tarns beneath the Fifth Crinkle. Gradually gaining definition it descends to a broad grassy saddle before rising again to the summit plateau of Cold Pike. To the north of the saddle is Great Knott at.

Geographic entities mentioned:
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
To the north of the saddle is Great Knott at. This top is considered by most guidebooks to be a subsidiary of Crinkle Crags rather than the nearer Cold Pike. Beyond the summit the ridge continues for another south eastward before falling steeply over the many tiered crags of Wrynose Breast.

Geographic entities mentioned:
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
Together with Hardknott Pass to the west, Wrynose is the latest incarnation of the Roman road from Ambleside to the port of Ravenglass. To the west of Cold Pike is the Gaitscale Beck, the watercourse separating it from Little Stand. To the east across a wide low col is Pike of Blisco, a conical fell with its footing firmly in Langdale.

Geographic entities mentioned:
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
It was worked from 1860 to 1875 but never achieved commercial success. Summit. The summit plateau of Cold Pike has three widely separated summits, all of which are listed as nuttalls. The lower two are unnamed on Ordnance Survey maps, but are generally referred to as Cold Pike West Top and Cold Pike Far West Top.

Geographic entities mentioned:
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
Summit. The summit plateau of Cold Pike has three widely separated summits, all of which are listed as nuttalls. The lower two are unnamed on Ordnance Survey maps, but are generally referred to as Cold Pike West Top and Cold Pike Far West Top. The true summit is itself one of a series of three outcrops in a mild echoing of Crinkle Crags. Each has a cairn, the highest being a fine example.

Geographic entities mentioned:
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
Ascents. Cold Pike can be reached easily via Red Tarn from the carpark at the summit of Wrynose Pass. It can also be climbed (less easily) from Great Langdale. More ‘honest’ walkers beginning in the south may wish to start from Little Langdale or Wrynose Bottom, first ascending Wrynose Pass.

Geographic entities mentioned:
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
surface_form: red tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.528333333333
lon: -3.0086111111111
A direct route from Wrynose Bottom is also possible although pathless, skirting around the left of the crags. A consideration here is that the Duddon will need to be forded when starting out. Cold Pike is often seen as a worthwhile detour &quot;en route&quot; to Crinkle Crags.

Geographic entities mentioned:
surface_form: cold pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.421
lon: -3.134
Ascents. Cold Pike can be reached easily via Red Tarn from the carpark at the summit of Wrynose Pass. It can also be climbed (less easily) from Great Langdale. More ‘honest’ walkers beginning in the south may wish to start from Little Langdale or Wrynose Bottom, first ascending Wrynose Pass.

Geographic entities mentioned:
surface_form: great langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
To the north is Red Tarn, a feeder via Oxendale of Great Langdale Beck. Red Tarn is an elongated pool whose stony bed can be seen through clear shallow waters, reputed to hold trout. It forms a focal point for walkers as the wide path from the summit of Wrynose Pass down to Stool End runs beside it, a further path branching off across the outflow to Crinkle Crags. Geology.

Geographic entities mentioned:
surface_form: red tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.528333333333
lon: -3.0086111111111
Geology. The fell top is composed of dacite lava flows with the volcaniclastic sandstones and tuffs of the Blisco Member outcropping to the south. The main Red Tarn path was originally made to serve Red Crag Mine. This consists of a series of pits and trial borings for iron, concentrated about north of the tarn. It was worked from 1860 to 1875 but never achieved commercial success. Summit.

Geographic entities mentioned:
surface_form: red tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.528333333333
lon: -3.0086111111111
István Rosztóczy. István Rosztóczy (17 November 1942 in Budapest, Hungary – 27 October 1993 in Mount Fuji, Gotemba, Japan) was a Hungarian microbiologist, medical researcher, blood donor organizer, who devoted his life to research and science. Life. He graduated from the Gábor Bethlen Secondary Grammar School at Hódmezővásárhely in 1960.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
He is known for interferon, especially the mechanism of the
priming effect of interferon, then interleukin-6 and tumor necrosis factor. He was a devoted hiker and made his last trip in Mount Fuji, Japan when he was wounded mortally while climbing down the mountain in the time of the International Society for Interferon and Cytokine Research (ISICR) Meeting in Tokyo.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
There are a number of inspection hatches and electric cabinets on the inclines, which are presumably connected with the power station infrastructure. To the north-west, on the other side of Moelwyn Mawr, lies the Croesor Quarry, where extraction of slate ceased in 1930.

Geographic entities mentioned:
surface_form: Moelwyn Mawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.983688888889
lon: -4.0004388888889
A fest'<nowiki/>&quot; and &quot;<nowiki/>'mela'<nowiki/>&quot; is held annually on this day on the premises. Grotto. &quot;St. Paula (347 – 404 A.D.), a Roman Senator's widow and her daughter Eustochium were living an austere life in Rome when St. Jerome (341 – 420 A.D.) came there from Palestine in 383 A.D.

Geographic entities mentioned:
surface_form: Nitrain
instance_of: Valley
countries: Egypt
coordinates: lat: 30.416666666667
lon: 30.333333333333
Grave of Motoori Norinaga (Mount Yamamuro). After Motoori died, he was buried on the summit of Mount Yamamuro behind the temple of Myōraki-ji in Matsusaka. The grave was situated to overlook the town on Matsusaka, and the hills of Mikawa and Mount Fuji in the distance across Ise Bay and is inscribed with a poem from the &quot;Man'yōshū&quot;.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
It is in the south of the island. Þjórsá is a glacier river and has its source on the glacier Hofsjökull. It flows out through narrow gorges in the highlands of Iceland. Further downstream, another river, the Tungnaá, flows into it (see also Háifoss), before it enters the lowlands. There it passes the valley of Þjórsárdalur (Thjorsardalur) where the historical farm of Stöng is located.

Geographic entities mentioned:
surface_form: highlands of Iceland
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.84
lon: -18.11
It flows out through narrow gorges in the highlands of Iceland. Further downstream, another river, the Tungnaá, flows into it (see also Háifoss), before it enters the lowlands. There it passes the valley of Þjórsárdalur (Thjorsardalur) where the historical farm of Stöng is located. In the lowlands it flows along the eastern border of the Great Þjórsá Lava.

Geographic entities mentioned:
surface_form: Þjórsárdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 64.106105
lon: -19.904852
It heads first southeastwards, parallel to the upper course of the Kauylzhyr river that flows a little to the south, to the northwest of lake Shalkar. In its middle course the river bends eastwards and in its final stretch it bends northeastwards, entering lake Tebez from the southwest. The Bolgasyn usually reaches its highest level for a few weeks in March and April when the snows melt.

Geographic entities mentioned:
surface_form: Tebez
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 48.2107
lon: 59.68155
This section was renamed in an effort to revitalize, or mask the social stigma attached to this high-crime section of the city. The same was done in the adjacent section west of the Chattahoochee River by the Cobb county commission, which named it Veterans Memorial Parkway through Mableton and Austell. South Carolina.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Early years. Orchardson was born in Edinburgh, where his father was engaged in business. &quot;Orchardson&quot; is a variation of &quot;Urquhartson&quot;, the name of a Highland sept settled on Loch Ness, from which the painter is descended.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
Barbodes. &quot;Barbodes&quot; is a genus of small to medium-sized cyprinid fish native to tropical Asia. The majority of the species are from Southeast Asia. Many species are threatened and some from the Philippines (Lake Lanao) are already extinct. A survey carried out in 1992 only found three of the endemic &quot;Barbodes&quot; species, and only two (&quot;Barbodes lindog&quot; and &quot;B.

Geographic entities mentioned:
surface_form: Lake Lanao
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
Wonderland Trail Shelters. The Wonderland Trail is an approximately hiking trail that circumnavigates Mount Rainier in Mount Rainier National Park, Washington, United States. The trail goes over many ridges of Mount Rainier for a cumulative of elevation gain. The trail was built in 1915.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Sunset Park Trail Shelter. The Sunset Park Trail Shelter was built in 1931 at Golden Lakes in the Sunset Park portion of Mount Rainier National Park. The rustic log structure provides shelter for hikers on the Wonderland Trail that encircles Mount Rainier. The Sunset Park shelter is built in a saltbox shape, with a porch spanning the width of the front.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
The narrow canyon at Saint-Maurice facilitated both trade and defense. The bridge over the Rhone was built around the 12th century and was the first bridge upstream of Lake Geneva after the Roman bridge of Massongex (2 km downstream Saint-Maurice). The fortifications in the canyon was gradually expanded in 1831, 1848, 1859 and finally in 1892.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
In Jerusalem, they were received by Melania the Younger, a famous ascetic whom Peter had met earlier in Constantinople and who might have inspired him to follow her. Melania bestowed upon them the monastic garb in a ceremony in the Anastasis and they became monks at her monastery on the Mount of Olives under their new names Peter and John.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
The range borders to the north with the Colli Albani, to the south-east with the Amaseno Valley, to the south with the Monti Ausoni and to the west with the Pontinian Plain. The highest peak is the Monte Semprevisa (1,536 m). The name derives probably from the Latin &quot;lapis&quot; (stone), referring to the mountains’ limestone rocks. In ancient times, the area was settled by the Volsci.

Geographic entities mentioned:
surface_form: Monte Semprevisa
instance_of: Mountain
countries: Italy
coordinates: lat: 41.569918
lon: 13.091769
Sacramento was named after the Sacramento River, which forms its western border. The river was named by Spanish cavalry officer Gabriel Moraga for the Santisimo Sacramento (Most Holy Sacrament), referring to the Catholic Eucharist. Before the arrival of Europeans, the Nisenan Native American tribe inhabited the Sacramento Valley area.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
The first European in the state of California was conquistador Juan Rodriguez Cabrillo, a Portuguese explorer sailing on behalf of the Spanish Empire, in 1542; later explorers included Sir Francis Drake and Sebastián Vizcaíno. However, no explorer had yet discovered the Sacramento Valley region nor the Golden Gate strait, which would remain undiscovered until, respectively, 1808 and 1623.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Stetson Pond (Pembroke, Massachusetts). Stetson Pond is a warm water pond in Pembroke, Massachusetts. The average depth is and the maximum depth is. The pond is characterized by brown water with a transparency of five feet. Access to the pond is provided by a dirt launch located off Plymouth Street, near Route 36.

Geographic entities mentioned:
surface_form: stetson pond (pembroke, massachusetts)
instance_of: Lake
countries: United States
coordinates: lat: 42.0292
lon: -70.8278
Stetson Pond (Pembroke, Massachusetts). Stetson Pond is a warm water pond in Pembroke, Massachusetts. The average depth is and the maximum depth is. The pond is characterized by brown water with a transparency of five feet. Access to the pond is provided by a dirt launch located off Plymouth Street, near Route 36.

Geographic entities mentioned:
surface_form: stetson pond
instance_of: Lake
countries: United States
coordinates: lat: 42.0292
lon: -70.8278
The city mayor estimates the preferred option of renovation to cost around USD 25.6 million. Kaimana Beach. Adjacent to the south of the Natatorium lies Kaimana Beach, a popular destination for the resident Honolulu population of the Kaimuki, Manoa, Diamond Head and other surrounding communities. Kaimana is a sandy beach lined with palms with a lifeguard tower, showers and public parking.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
It is a long and narrow fjord lined with high mountains rising steeply from the shore. Hannah Island, a small island, lies in the area of its mouth by the Kennedy Channel, Cape Bryan is on the western side of the mouth and Cape Maynard on the northeastern. This fjord is located northeast of Washington Land, at the northern end of Daugaard-Jensen Land.

Geographic entities mentioned:
surface_form: Kennedy Channel
instance_of: Watercourse
countries: Canada
Greenland
coordinates: lat: 80.9167
lon: -66.5
The Ice-Maiden. &quot;The Ice-Maiden&quot; (, or in contemporary Danish) is an 1861 literary fairy tale by the Danish writer Hans Christian Andersen. The first English translation was published by King and Baird in 1863. The story, set in Switzerland, was inspired by a local legend about the Île de Peilz, a small island in Lake Geneva, which is also the setting of its denouement. Summary.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Ashburn, Ontario. Ashburn is a hamlet in the town of Whitby, Durham Region, Ontario, Canada, located approximately 15 kilometres north of the town core, and centred on the intersection of Ashburn Road and Myrtle Road. It is a rural settlement area on the Oak Ridges Moraine, situated on the headwaters of the Lynde Creek watershed and part of Ontario's protected Golden Horseshoe Greenbelt. History.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
In 1869, Ashburn had a population between 100 and 250, with a stage coach to Uxbridge and Whitby, daily mail, an Orange Society (No. 176), three stores, two hotels and several blacksmiths and wagonmakers. Between 1870 and 1872, a railway was built from Port Whitby on Lake Ontario to Port Perry on Lake Scugog, crossing Myrtle Road two kilometres east of Ashburn.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
However, her attraction to him persists, making her struggle to do so: &quot;All this time I've been playin' your side / I could've done better shit with my life.&quot; She tells herself that if she continued to stay, she would feel more &quot;fucked up&quot;. &quot;TwoAM&quot; was produced by ThankGod4Cody, Carter Lang, and Scum, and it was recorded in Lang's cottage near Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
According to the 2021 census, it had 43 inhabitants. The village is about 9 km west of Nafpaktos. It is located at the foot of a northeastern foothill of Klokova and is on the right bank of the creek named Varia. In the vicinity toward the south is the ancient city of Molykreio, where an ancient temple is located. History.

Geographic entities mentioned:
surface_form: Klokova
instance_of: Mountain
countries: Greece
coordinates: lat: 38.360277777778
lon: 21.681666666667
state of Virginia. The original Native American name for the ridge is unknown. Geography. The mountain bisects the Shenandoah Valley just east of Strasburg in Shenandoah County in the north, to its highest peak east of Harrisonburg in Rockingham County in the south. The mountain is divided into northern and southern sections, divided by the New Market Gap.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The ridges of the northern section converge at New Market Gap. The southern section consists of a series of closely gathered ridges, separated by precipitous creek gorges. On the eastern side of the mountain range lie the Page Valley and the Blue Ridge Mountains. On the western side lie the North-Central Shenandoah Valley and the Great North Mountain of the Alleghany Mountains. Recreation.

Geographic entities mentioned:
surface_form: Page Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.7497
lon: -78.3992
The ridges of the northern section converge at New Market Gap. The southern section consists of a series of closely gathered ridges, separated by precipitous creek gorges. On the eastern side of the mountain range lie the Page Valley and the Blue Ridge Mountains. On the western side lie the North-Central Shenandoah Valley and the Great North Mountain of the Alleghany Mountains. Recreation.

Geographic entities mentioned:
surface_form: Great North Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0356
lon: -78.5675
surface_form: shenandoah
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The mountain is divided into northern and southern sections, divided by the New Market Gap. The northern section consists of 3 roughly parallel ridges, forming 2 valleys. The wider, main valley, is called Fort Valley, while the smaller one is known as Little Fort Valley. The ridges of the northern section converge at New Market Gap.

Geographic entities mentioned:
surface_form: fort valley
instance_of: Valley
countries: United States
coordinates: lat: 38.825
lon: -78.435
surface_form: fort valley
instance_of: Valley
countries: United States
coordinates: lat: 38.825
lon: -78.435
Recreation. Most of the range is part of the Lee Ranger District of the George Washington National Forest and contains the Elizabeth Furnace and Camp Roosevelt recreational areas. The Potomac Appalachian Trail Club maintains the Massanutten Trail as well as several other hiking trails in the forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Massanutten Mountain. Massanutten Mountain is a synclinal ridge in the Ridge-and-Valley Appalachians, located in the U.S. state of Virginia. The original Native American name for the ridge is unknown. Geography. The mountain bisects the Shenandoah Valley just east of Strasburg in Shenandoah County in the north, to its highest peak east of Harrisonburg in Rockingham County in the south.

Geographic entities mentioned:
surface_form: massanutten mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
Most of the range is part of the Lee Ranger District of the George Washington National Forest and contains the Elizabeth Furnace and Camp Roosevelt recreational areas. The Potomac Appalachian Trail Club maintains the Massanutten Trail as well as several other hiking trails in the forest. Signal Knob, a former Civil War signal station on the northern peak of the mountain, is a popular destination.

Geographic entities mentioned:
surface_form: massanutten
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
Signal Knob, a former Civil War signal station on the northern peak of the mountain, is a popular destination. The forest service also maintains several ATV trails. In 1971, the Massanutten Mountain ski lodge and four-season resort village was established near the southern peak. The private resort has nearly doubled in size since Great Eastern Resorts bought it in 1995. Flora and fauna.

Geographic entities mentioned:
surface_form: massanutten mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
The private resort has nearly doubled in size since Great Eastern Resorts bought it in 1995. Flora and fauna. Wildlife on Massanutten includes black bear, coyotes, wild turkeys, white-tailed deer, timber rattlesnake, and luna moths. Significant flora includes mayapple, bluets, wild lupine, cardinal flower, and pinxter flower. Geology.

Geographic entities mentioned:
surface_form: massanutten
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
Geology. The geology of the Massanutten Mountains is dominated by Silurian Massanutten Sandstone, a lateral equivalent of the Tuscarora Formation in the Appalachian Mountains to the west, overlying the Ordovician Martinsburg Formation. Erosion of the Martinsburg shale in some areas of the mountain caused the sandstone to break and slide to form talus slopes.

Geographic entities mentioned:
surface_form: massanutten
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
surface_form: massanutten
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
Erosion of the Martinsburg shale in some areas of the mountain caused the sandstone to break and slide to form talus slopes. The Massanutten Sandstone is folded in a synclinorium, and it outcrops at the ridge tops.

Geographic entities mentioned:
surface_form: massanutten
instance_of: Mountain
countries: United States
coordinates: lat: 38.643
lon: -78.612
Personal life. San Giacomo has been married twice. Her first marriage (1990–1998) was to actor Cameron Dye, with whom she had a son, Mason, who was born with cerebral palsy. In 2000, she remarried, to actor Matt Adler. She is a cousin of Torry Castellano, former drummer of the rock group The Donnas. She lives in the San Fernando Valley, California. Philanthropy.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
As with much of the United Kingdom, the coldest month is January, while the warmest month is July. Altitude affects average temperature results, with the Severn Valley to the south and the Peak District to the north of The Midlands contributing to the average climate figures for the region. Notable people. Fred Jordan (1922–2002), folk singer, died in a residential home at Ditton Priors.

Geographic entities mentioned:
surface_form: Severn Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.5
lon: -2.33333
bholua&quot; subsp. &quot;emeiensis&quot; is distinguished from subsp. &quot;bholua&quot; by obtuse leaves, shorter oblong involucral bracts (up to 7 mm rather than 18 mm), and shorter calyx lobes (3–5 mm rather than 5–7 mm). It has reddish fruit. It is found in forests and forest margins at altitudes of 800–1100 m in Mount Emei and Pingshan county in Sichuan, China. Distribution. &quot;D.

Geographic entities mentioned:
surface_form: Mount Emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
In the 8th century BC in central-southern Italy, for example, Latins were settled in the west from which the Romans would later emerge, Sabines in the upper Tiber Valley, Umbrians in the north-east, Samnites in the south, Oscans and others shared the Italian peninsula with two other main ethnic groups: Etruscans to the north, and Greeks to the south.

Geographic entities mentioned:
surface_form: Tiber Valley
instance_of: Valley
countries: Italy
coordinates: lat: 42.133333333333
lon: 12.583333333333
In 2019, Philippa R. Alvarez and Marco Duretto published a paper suggesting that the plants previously known as &quot;A. correifolia&quot; occurring in Queensland and those on the Northern Tablelands of New South Wales were different species. They gave those in Queensland the name &quot;Asterolasia sola&quot; and those on the Northern Tablelands &quot;A. exasperata&quot;.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
Bonnetia bolivarensis. &quot;Bonnetia bolivarensis&quot; is a species of flowering plant in the Bonnetiaceae family. It is found only in Venezuela, known only from a single locality in the summit savanna of Ptari-tepui, in Canaima National Park in Bolívar.

Geographic entities mentioned:
surface_form: Ptari-tepui
instance_of: Mountain
countries: Venezuela
coordinates: lat: 5.7669444444444
lon: -61.811111111111
Sweeney Mountains. The Sweeney Mountains () are a group of mountains of moderate height and about extent, located north of the Hauberg Mountains in eastern Ellsworth Land, Antarctica. Location. The Sweeney Mountains are in the southeast of Ellsworth Land.

Geographic entities mentioned:
surface_form: Ellsworth Land
instance_of: Plateau
coordinates: lat: -75.5
lon: -80
Location. The Sweeney Mountains are in the southeast of Ellsworth Land. They are east of the Merrick Mountains, northeast of the Behrendt Mountains, north of the Hauberg Mountains, northwest of the Wilkins Mountains and west of the Scaife Mountains. The region to the north, extending to the English Coast, is largely featureless.

Geographic entities mentioned:
surface_form: Ellsworth Land
instance_of: Plateau
coordinates: lat: -75.5
lon: -80
His daughter Rosebud Yellow Robe persuaded her father to perform the part after being assured by Burden that the film would contain &quot;an honest depiction of Native American life.&quot; Upon this assurance, Yellow Robe changed his mind and traveled to Arnprior and Lake Temagami in Ontario, Canada, to shoot the film.

Geographic entities mentioned:
surface_form: Lake Temagami
instance_of: Lake
countries: Canada
coordinates: lat: 46.95
lon: -80.0833
Lake Waramaug. Lake Waramaug is a lake occupying parts of the towns of Kent, Warren and Washington in Litchfield County, Connecticut, United States, approximately north of Danbury. The lake is named after Chief Waramaug, who wintered in the area surrounding Lake Waramaug. Description. Although natural in origin, the surface elevation of the lake has been raised by a small concrete and masonry dam.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake waramaug
instance_of: Lake
countries: United States
coordinates: lat: 41.698055555556
lon: -73.361111111111
Plans for the new boat launch were developed in 2006, and the new facility was opened in 2008. In 2010, the Town of Washington separately completed major reconstruction of the adjacent, Hitherto Forlorn Town Beach at Lake Waramaug, which may be used only by Washington residents and their guests.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake waramaug
instance_of: Lake
countries: United States
coordinates: lat: 41.698055555556
lon: -73.361111111111
Lake Waramaug. Lake Waramaug is a lake occupying parts of the towns of Kent, Warren and Washington in Litchfield County, Connecticut, United States, approximately north of Danbury. The lake is named after Chief Waramaug, who wintered in the area surrounding Lake Waramaug. Description. Although natural in origin, the surface elevation of the lake has been raised by a small concrete and masonry dam.

Geographic entities mentioned:
surface_form: lake waramaug
instance_of: Lake
countries: United States
coordinates: lat: 41.698055555556
lon: -73.361111111111
The surface area of the lake is approximately. The lake has a maximum depth of, an average depth of, and contains approximately of water. The lake is fed by Sucker Brook (Lake Waramaug Brook), numerous small streams, and groundwater that enters through the lake bottom. Drainage from Waramaug Lake flows southward into the East Aspetuck River.

Geographic entities mentioned:
surface_form: lake waramaug
instance_of: Lake
countries: United States
coordinates: lat: 41.698055555556
lon: -73.361111111111
Wetlands and water bodies comprise approximately 10 percent () of the watershed, while the remaining 16 percent () of the area is low-density residential housing and commercial and agricultural land. The shoreline development of Lake Waramaug is moderate and includes houses, seasonal cottages, and boat houses, with few commercial establishments.

Geographic entities mentioned:
surface_form: lake waramaug
instance_of: Lake
countries: United States
coordinates: lat: 41.698055555556
lon: -73.361111111111
The shoreline development of Lake Waramaug is moderate and includes houses, seasonal cottages, and boat houses, with few commercial establishments. Public access to the lake is available only within Lake Waramaug State Park, which is located at the northwestern end of the lake. Outside park boundaries, the shoreline is privately owned.

Geographic entities mentioned:
surface_form: lake waramaug
instance_of: Lake
countries: United States
coordinates: lat: 41.698055555556
lon: -73.361111111111