Sarmila/GeoWiki-Features huggingface dataset:
These winds are strongest at places where canyons, such as Deep Creek Canyon, open into the valley. In the Warner Valley, frost is common until late spring and begins again in early fall. As a result, the growing season in the valley is limited to about 100 days. The Warner Valley gets most of its rain in May and June, while the summer and fall months tend to be very dry.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Warner Valley gets most of its rain in May and June, while the summer and fall months tend to be very dry. The winter snowfall in the valley bottom is generally very light; however, winter temperatures can get very cold. The higher plateau country above the valley usually gets several feet of snow and the higher peaks can get much more.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The winter snowfall in the valley bottom is generally very light; however, winter temperatures can get very cold. The higher plateau country above the valley usually gets several feet of snow and the higher peaks can get much more. In most years, the high peaks have snow on them from early fall until mid-summer. This snowpack feeds the streams that drain into the valley. Ecology.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The higher plateau country above the valley usually gets several feet of snow and the higher peaks can get much more. In most years, the high peaks have snow on them from early fall until mid-summer. This snowpack feeds the streams that drain into the valley. Ecology. The Warner Valley provides a number of unique animal habitats.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
This snowpack feeds the streams that drain into the valley. Ecology. The Warner Valley provides a number of unique animal habitats. These include lake, marsh, riparian, grasslands, sage steppe, dry forest, and rimrock. They range in elevation from approximately above sea level at the valley floor to over at the summit of Warner Peak. Marsh grasses are common along the lake shores.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: warner peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.459722222222
lon: -119.74166666667
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Marsh grasses are common along the lake shores. In the riparian areas, wild roses, choke cherry, wild plum, cottonwood, and willow are found. Beyond the wetlands, the valley becomes quite dry. Much of the North Warner Valley is semi-desert, where dwarf sagebrush, greasewood, and Western Juniper are the dominant vegetation.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Beyond the wetlands, the valley becomes quite dry. Much of the North Warner Valley is semi-desert, where dwarf sagebrush, greasewood, and Western Juniper are the dominant vegetation. The valley’s wildlife includes common high desert mammal species, resident birds, and migrant waterfowl. There are forty-two mammal species that live in the Warner Valley-Hart Mountain area.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
In the valley’s riparian areas, dusky flycatchers, yellow warblers, orange-crowned warblers, house wrens, and spotted towhees are common in the summer months. In the sage steppes and grasslands, summer residents include horned larks, Brewer's sparrows, vesper sparrows, common ravens, sage thrashers, sagebrush sparrows, black-throated sparrows, and greater sage grouse.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
In the rimrock areas, there are chukars, rock wrens, canyon wrens, cliff swallows, and barn swallows. The valley also hosts mountain chickadees, Cassin's finches, black-headed grosbeaks, green-tailed towhees, yellow-rumped warblers, MacGillivray's warblers, mountain bluebirds, white-headed woodpeckers, and flammulated owls.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
History. Native Americans used the Warner Valley for thousands of years before the first Europeans arrived. The valley has scores of petroglyphs, some estimated to be 12,000 years old. The Greaser Petroglyph Site, in the South Warner Valley, is listed on the National Register of Historic Places.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The valley has scores of petroglyphs, some estimated to be 12,000 years old. The Greaser Petroglyph Site, in the South Warner Valley, is listed on the National Register of Historic Places. The first European explorer to enter the valley was probably John Work, who headed a Hudson's Bay Company trapping expedition in 1832.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
While it is not certain that he visited the valley, he was in the area and left a description of a &quot;valley of lakes&quot; that correspond closely to the Warner Valley. The next explorer to arrive in the valley was Captain John C. Fremont, who led a party through the valley in December 1843. Fremont named it Christmas Valley since his party spent Christmas Day camped near Hart Lake.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
In 1864, Lieutenant Colonel C. S. Drew of the 1st Oregon Cavalry visited the valley while on a long-range reconnaissance patrol. Drew named the valley in honor of Warner, who he believed had been killed there. In 1865, the Army decided it needed a fort in the Warner Valley to facilitate the interdiction of Indian raiding parties passing through the area.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The winter snowfall in the valley bottom is generally very light; however, winter temperatures can get very cold. The higher plateau country above the valley usually gets several feet of snow and the higher peaks can get much more. In most years, the high peaks have snow on them from early fall until mid-summer. This snowpack feeds the streams that drain into the valley. Ecology.

Geographic entities mentioned:
surface_form: high peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45
lon: -70.4
The Warner Lakes formed in the valley bottom after the faulting stopped. The Warner Valley is bounded by high escarpment walls on the east and west. The main line of perpendicular displacement is along the foot of the cliffs to the east of the Warner Lakes. This scarp feature is known as Hart Mountain. The main cliff face of Hart Mountain towers above the valley floor.

Geographic entities mentioned:
surface_form: warner lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
Drew named the valley in honor of Warner, who he believed had been killed there. In 1865, the Army decided it needed a fort in the Warner Valley to facilitate the interdiction of Indian raiding parties passing through the area. Army scouts selected a site along Honey Creek on the west side of the Warner Lakes. In 1866, a detachment from Fort Boise was sent to establish the fort.

Geographic entities mentioned:
surface_form: warner lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
Much of the valley is public land administered by the Bureau of Land Management. These public lands offer numerous recreational opportunities including hunting, fishing, bird watching, wildlife viewing, boating, and camping. However, some of these activities are dependent on the water level of the Warner Lakes, which can fluctuate dramatically.

Geographic entities mentioned:
surface_form: warner lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 42.4499
lon: -119.851
Warner Peak is the highest point on Hart Mountain. The summit is above sea level. The valley floor is occupied by a chain of lakes known collectively as the Warner Lakes. The entire valley was once covered by a single vast lake; however, the water level gradually receded, leaving a chain of lakes at the low spots with marshland between the lakes.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
In 1866, a detachment from Fort Boise was sent to establish the fort. The soldiers arrived on the east side of the lakes in late summer. Unable to cross the chain of lakes and marshes, the soldiers built a winter camp on the east side of the lakes. The camp was sited poorly and the men had a very difficult winter. In February 1867, General George Crook visited the Warner Valley outpost.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
The commune lies in the southwestern reaches of the Transylvanian Plateau, on the banks of the river Sebeș. It is located in the southern part of Alba County, south of Sebeș and south of the county seat, Alba Iulia. Săsciori is crossed by national road Transalpina (DN67C), which starts in Sebeș and runs due south over the Parâng Mountains to Novaci, in Gorj County.

Geographic entities mentioned:
surface_form: Transylvanian Plateau
instance_of: Plateau
countries: Romania
coordinates: lat: 46.5
lon: 24.5
It is in the Rural Municipality of Saltcoats No. 213 and adjacent to the town of Saltcoats. At, it is a small lake with a regional park at its southern end and public trails along the eastern shore. The outflow is from the southern end and it flows north-west where it meets up with Yorkton Creek. Recreation. Saltcoats & District Regional Park is at the southern end of Anderson Lake.

Geographic entities mentioned:
surface_form: Yorkton Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 51.3833
lon: -102.53426
Anderson Lake (Saskatchewan). Anderson Lake, also known as Saltcoats Lake, is a lake in the Canadian province of Saskatchewan. It is in the Rural Municipality of Saltcoats No. 213 and adjacent to the town of Saltcoats. At, it is a small lake with a regional park at its southern end and public trails along the eastern shore.

Geographic entities mentioned:
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.73441
lon: -63.86179
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7266
lon: -63.6197
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.73
lon: -125.19861
surface_form: anderson lake (saskatchewan)
instance_of: Lake
countries: Canada
coordinates: lat: 51.03333
lon: -102.15047
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.6333
lon: -122.417
Anderson Lake (Saskatchewan). Anderson Lake, also known as Saltcoats Lake, is a lake in the Canadian province of Saskatchewan. It is in the Rural Municipality of Saltcoats No. 213 and adjacent to the town of Saltcoats. At, it is a small lake with a regional park at its southern end and public trails along the eastern shore.

Geographic entities mentioned:
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.73441
lon: -63.86179
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7266
lon: -63.6197
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.73
lon: -125.19861
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.03333
lon: -102.15047
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.6333
lon: -122.417
The outflow is from the southern end and it flows north-west where it meets up with Yorkton Creek. Recreation. Saltcoats & District Regional Park is at the southern end of Anderson Lake. The park is accessed from Saltcoats and Highway 16. Some of the amenities include camping, boating, swimming, and picnicking. There is lake access via a dock in the park.

Geographic entities mentioned:
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.73441
lon: -63.86179
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7266
lon: -63.6197
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.73
lon: -125.19861
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.03333
lon: -102.15047
surface_form: anderson lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.6333
lon: -122.417
Bus. Bus services in the area are operated mainly by Stagecoach Cumbria & North Lancashire & other local companies. Direct services link the town with Windermere and Bowness-on-Windermere via Carnforth, Milnthorpe and Kendal (755), Lancaster with connections to Keswick via Carnforth, Milnthorpe, Kendal, Windermere, Ambleside and Grasmere.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
The main remaining faction of the Shining Path, the Militarized Communist Party of Peru (MPCP), is active in the VRAEM region of Peru, and it has since distanced itself from the Shining Path's legacy in 2018 in order to maintain the support of peasants previously persecuted by the Shining Path.

Geographic entities mentioned:
surface_form: VRAEM region
instance_of: Valley
countries: Peru
coordinates: lat: -11.7
lon: -74
In addition to the MPCP, the Communist Party of Peru – Red Mantaro Base Committee (PCP-CBMR) has been operating in the Mantaro Valley since 2001, while the Communist Party of Peru – Huallaga Regional Committee (PCP-CRH) was active at the Huallaga region from 2004 until Comrade Artemio's capture in 2012. Name.

Geographic entities mentioned:
surface_form: Mantaro Valley
instance_of: Valley
countries: Peru
coordinates: lat: -11.91666667
lon: -75.33333333
This maxim was featured on the masthead of the newspaper of a Shining Path front group. The followers of this group are generally called &quot;senderistas&quot;. Organization. The Shining Path's remnants currently operate in the VRAEM region and primarily comprises two groups and their sub-branches; a paramilitary wing and a political wing.

Geographic entities mentioned:
surface_form: VRAEM region
instance_of: Valley
countries: Peru
coordinates: lat: -11.7
lon: -74
Of these, the Militarized Communist Party of Peru (MPCP) is considered the group's main successor, founded in 1999 by brothers Víctor and Jorge Quispe Palomino after the collapse of &quot;Sendero Rojo&quot;, the faction that had rejected Guzmán's peace treaty. Also active is a faction in the Mantaro Valley since 2001.

Geographic entities mentioned:
surface_form: Mantaro Valley
instance_of: Valley
countries: Peru
coordinates: lat: -11.91666667
lon: -75.33333333
VRAEM stronghold. Into the 2020s, Shining Path has existed in remaining splinter groups. The main remaining group, called the Militarized Communist Party of Peru (MPCP) of about 450 individuals remained in the Valle de los Ríos Apurímac, Ene y Mantaro (VRAEM) region, reportedly making revenue by escorting cocaine traffickers and are reportedly led by two brothers; Víctor and Jorge Quispe Palomino.

Geographic entities mentioned:
surface_form: Valle de los Ríos Apurímac, Ene y Mantaro
instance_of: Valley
countries: Peru
coordinates: lat: -11.7
lon: -74
While there he worked on the case of the unsolved murder victim who has become known as Wych Elm Bella. In 1944 he joined the Freshwater Biological Association (FBA) as Scientific Officer for algology, moving to Windermere with the Association's Fritsch Collection of Freshwater Algae in 1954. He retired in 1978, was appointed Deputy chief scientific officer and then Honorary Advisor to the FBA.

Geographic entities mentioned:
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
Strathearn (disambiguation). s1w8lx1lb3g82a95iwioy4wmw8p2" xml:space="preserve">Strathearn is a place in Scotland.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
Plackweghöhe. The Plackweghöhe (&quot;Plackweg Heights&quot;), whose main summit has hitherto had no official name, is the highest point in the borough of Warstein, the hill ridge of the Plackwald, the North Sauerland Uplands, and the Arnsberg Forest Nature Park in the German state of North Rhine-Westphalia. It is and lies within the counties of Soest and Hochsauerlandkreis.

Geographic entities mentioned:
surface_form: arnsberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.3951
lon: 9.962
surface_form: plackweghöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3953
lon: 8.34603
Plackweghöhe. The Plackweghöhe (&quot;Plackweg Heights&quot;), whose main summit has hitherto had no official name, is the highest point in the borough of Warstein, the hill ridge of the Plackwald, the North Sauerland Uplands, and the Arnsberg Forest Nature Park in the German state of North Rhine-Westphalia. It is and lies within the counties of Soest and Hochsauerlandkreis.

Geographic entities mentioned:
surface_form: plackweghöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3953
lon: 8.34603
Natural regions. The Plackweghöhe belongs to the major unit group of the Süder Uplands (Np. 33) and the major unit of the North Sauerland Uplands (334) as part of the &quot;Plackweghöhe (Plackwald)&quot; sub-unit (334.5). Name. The name &quot;Plackweghöhe&quot; does not just cover the hill itself, but a ridge along the old trading route of the Plackweg.

Geographic entities mentioned:
surface_form: plackweghöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3953
lon: 8.34603
surface_form: plackweghöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3953
lon: 8.34603
The term does not relate explicitly to the highest point, but to the entire, roughly 20-km-long ridgeline of the North Sauerland scarp on the Ruhr-Möhne watershed between the hills of &quot;Großer Berg&quot; (476.0 m) in the west and the &quot;Großen Storchschnabel&quot; (ca. 516.7 m) in the east, along which ridgeline the Plackweg runs.

Geographic entities mentioned:
surface_form: großer berg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.9759
lon: 14.7995
It resulted in 247 exchanges of bancos (land surrounded by bends in the river that became segregated by a cutoff often by the rapid erosion of the river channel) between the two nations from 1910 to 1976. Most of them were in the Lower Rio Grande Valley, the Presidio Valley and the El Paso-Juarez Valley. In 1927, the convention was applied to the short international border on the Colorado River.

Geographic entities mentioned:
surface_form: Lower Rio Grande Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 26.22
lon: -98.12
Human use. The continuation of Lake Yalpug in the south is Lake Kuhurlui. Between these lakes in the 70s of the 20th century, a dam, which were built to protect the areas adjacent to the river from flooding and regulate the water level in the lakes (in the interests of agriculture). along which The Izmail-Reni road was built along the dam.

Geographic entities mentioned:
surface_form: Lake Kuhurlui
instance_of: Lake
countries: Ukraine
coordinates: lat: 45.3
lon: 28.66666667
surface_form: lake kuhurlui
instance_of: Lake
countries: Ukraine
coordinates: lat: 45.3
lon: 28.66666667
Lake Yalpuh. Yalpuh () is a freshwater lake located in the southern Ukrainian oblast of Odesa. The largest natural lake in Ukraine. Yalpug is located in a temperate climate zone with warm summers and cold winters. The water level in the lake fluctuates seasonally: minimum in winter and autumn, maximum in spring and summer.

Geographic entities mentioned:
surface_form: lake yalpuh
instance_of: Lake
countries: Ukraine
coordinates: lat: 45.416666666667
lon: 28.616666666667
Yalpug is located in a temperate climate zone with warm summers and cold winters. The water level in the lake fluctuates seasonally: minimum in winter and autumn, maximum in spring and summer. Through Lake Kugurluy, rivers and straits, the lake are connected to the Danube. Lake Yalpug is home to up to 40 species of fish, many of which are of commercial importance.

Geographic entities mentioned:
surface_form: kugurluy
instance_of: Lake
countries: Ukraine
coordinates: lat: 45.3
lon: 28.66666667
The largest town on Yalpuh's shores is Bolhrad at its northernmost point. Larger villages include Vynohradivka to the north, Kotlovyna to the west and Ozerne on its southeastern shore. It covers an area of 149 km², has an average depth of about two metres, a maximum depth of 5.5 metres and, at its southernmost point, adjoins Lake Kugurluy. Two rivers, Yalpug and Karasulak, flow into the lake.

Geographic entities mentioned:
surface_form: kugurluy
instance_of: Lake
countries: Ukraine
coordinates: lat: 45.3
lon: 28.66666667
The amplitude of the water level fluctuation in the lake is up to 360 cm. Through Lake Kugurluy, rivers and straits, the lake are connected to the Danube. During heavy floods, Danube water flows through these straits into Kugurluy and Yalpug. The Yalpug River flows into the lake at an altitude of 2.0 m above sea level. Flora and fauna.

Geographic entities mentioned:
surface_form: kugurluy
instance_of: Lake
countries: Ukraine
coordinates: lat: 45.3
lon: 28.66666667
along which The Izmail-Reni road was built along the dam. After the construction of the dam, the water exchange between Lake Yalpug and Kugurluy decreased by almost a third. The territory around the lake is covered with vineyards, orchards and agricultural fields. Agricultural enterprises of the Bolgrad and Izmail districts of the Odessa region use the lake water for their needs.

Geographic entities mentioned:
surface_form: kugurluy
instance_of: Lake
countries: Ukraine
coordinates: lat: 45.3
lon: 28.66666667
The Vynogradivka Landscape Reserve of Local Significance is located in the Bolgrad district of the Odessa region, near the villages of Vynogradivka and Vladycheny, which protects areas of steppe with plants from the Red Book of Ukraine. In the summer of 2020, the Odesa regional administration announced the creation of a project for a landscape national park on lakes Kugurluy and Yalpug.

Geographic entities mentioned:
surface_form: kugurluy
instance_of: Lake
countries: Ukraine
coordinates: lat: 45.3
lon: 28.66666667
Jim Dreyer. Jim Dreyer (born August 16, 1963), self described as The Shark, is an ultra marathon swimmer. Career. Dreyer completed a 41-hour swim across Lake Michigan in 1998. He failed to repeat the swim in 2023. He failed to complete the route once again the next year due to a his GPS running low on power. He towed a 906 kg worth of bricks for 35 kilometers from Canada to Detroit in 2013.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Career. Dreyer completed a 41-hour swim across Lake Michigan in 1998. He failed to repeat the swim in 2023. He failed to complete the route once again the next year due to a his GPS running low on power. He towed a 906 kg worth of bricks for 35 kilometers from Canada to Detroit in 2013. The swim, which took place in Lake St. Clair, took 54 hours to complete.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
Geography. Lago di Comabbio is a lake in the Province of Varese, Lombardy, Italy. At an elevation of, its surface area is. Once it was part of Lake Varese, but now the two lakes are connected just by an artificial channel, which is even one of its greatest emissaries. Wildlife. In the lake, it is forbidden to use motor boats, and thanks to this the growth of the wildlife was possible.

Geographic entities mentioned:
surface_form: Lake Varese
instance_of: Lake
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.7333333333333
Experts thinks that in the next years the fauna of this lake will be in serious danger, because of the most likely arrival of one of the most lethal predators in northern Italy: the Wels catfish. Who is yet causing serious problems in other lakes and rivers in northern Italy such as: Lake Maggiore, Lake Iseo and also in Po River.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
surface_form: Lake Iseo
instance_of: Lake
countries: Italy
coordinates: lat: 45.711666666667
lon: 10.071944444444
Lago di Comabbio. Geography. Lago di Comabbio is a lake in the Province of Varese, Lombardy, Italy. At an elevation of, its surface area is. Once it was part of Lake Varese, but now the two lakes are connected just by an artificial channel, which is even one of its greatest emissaries. Wildlife.

Geographic entities mentioned:
surface_form: lago di comabbio
instance_of: Lake
countries: Italy
coordinates: lat: 45.761944
lon: 8.691389
Transmission Gully. The Transmission Gully is a gully in Wellington, it is also a chain of steep-sided, isolated valleys in the Wellington Region of New Zealand, runs approximately north–south between the Kāpiti Coast and Tawa, through hills east of Porirua. The gully's name comes from the 110,000-volt transmission line that formerly ran through it.

Geographic entities mentioned:
surface_form: transmission gully
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.05
lon: 174.93
The gully's name comes from the 110,000-volt transmission line that formerly ran through it. The line, built in 1924, linked Wellington to the Mangahao hydroelectric station near Shannon, and later to the wider North Island transmission grid. Despite lying mostly within the boundaries of Porirua City, Transmission Gully is sparsely populated, and most of the land is farmland, forest, or scrub.

Geographic entities mentioned:
surface_form: transmission gully
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.05
lon: 174.93
Despite lying mostly within the boundaries of Porirua City, Transmission Gully is sparsely populated, and most of the land is farmland, forest, or scrub. There are some areas with lifestyle blocks, particularly near Pāuatahanui, and Transmission Gully is also home to Battle Hill Farm Forest Park.

Geographic entities mentioned:
surface_form: transmission gully
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.05
lon: 174.93
The 1879 proposal for a Haywards–Plimmerton Line railway route north from Wellington envisaged using these valleys; the line was never built. The Transmission Gully Motorway running through the gully was opened in March 2022. It is part of State Highway 1 and was constructed as part of the 2008-2017 National Government's Roads of National Significance package.

Geographic entities mentioned:
surface_form: transmission gully
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.05
lon: 174.93
It will not, however, offer any access to the gully itself, as only a single interchange providing access to Paekākāriki exists between Pāuatahanui and Mackays Crossing. Apart from the motorway, the only other road access through Transmission Gully is the narrow and winding Paekākāriki Hill Road.

Geographic entities mentioned:
surface_form: transmission gully
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.05
lon: 174.93
Apart from the motorway, the only other road access through Transmission Gully is the narrow and winding Paekākāriki Hill Road. Beginning at Paekākāriki, it travels up and over the western ridge of Transmission Gully, and then gradually descends the western bank along most of the length of the gully to Pāuatahanui.

Geographic entities mentioned:
surface_form: transmission gully
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.05
lon: 174.93
Mt. Fuji Station. is a railway station on the Fujikyuko Line in the city of Fujiyoshida, Yamanashi, Japan, operated by the private railway operator Fuji Kyuko (Fujikyu). The station is located at an altitude of. This is one of the gateway stations to Mount Fuji and Fuji Five Lakes, including Lake Kawaguchi and Lake Yamanaka. Lines. Mt.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
surface_form: Fuji Five Lakes
instance_of: Group of lakes
countries: Japan
coordinates: lat: 35.415833333333
lon: 138.87111111111
__TOC__
Setting. The ridge parallels a section of the San Andreas Fault, and features panoramic vistas with trees, meadows, rounded hillsides, Bolinas Lagoon, Tomales Bay, the Olema Valley and the Pacific Ocean. The base of the ridge at the south end includes the community of Stinson Beach, with the ridge rising abruptly from around to over at the highest point.

Geographic entities mentioned:
surface_form: Olema Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.9948
lon: -122.754
Views to the east include lakes and undulating hills, with the ocean to the west, the source of dense fog that sometimes obscures all views and limits visibility to a few feet. A popular site for hiking and biking, Mount Tamalpais, where Bolinas Ridge is located, offers many different trails and paths for visitors.

Geographic entities mentioned:
surface_form: mount tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
surface_form: bolinas ridge
instance_of: Mountain
countries: United States
coordinates: lat: 37.907222222222
lon: -122.62027777778
A popular trail is the Bolinas Ridge Trail which is a loop that connects to Samuel Taylor Park and is about 16.9 kilometers (or 10.5 miles). In terms of weather, the temperature on Mount Tamalpais is fairly cool, generally somewhere between 43°F and 72°F. December through February tend to be the cooler months while June through October tend to be warmer. Flora.

Geographic entities mentioned:
surface_form: mount tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
Fauna. There are few animals that have robust communities near Bolinas Ridge, but within Mount Tamalpais State Park, black-tailed deer (Odocoileus hemionus), raccoons (Procyon lotor), and squirrels (Sciuridae) have been known to roam. Additionally there is a plentiful bird population.

Geographic entities mentioned:
surface_form: mount tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
surface_form: bolinas ridge
instance_of: Mountain
countries: United States
coordinates: lat: 37.907222222222
lon: -122.62027777778
Bolinas Ridge. Bolinas Ridge is a north-south ridge in southwestern Marin County, California. Much of the western side of the ridge is protected parkland in the Golden Gate National Recreation Area, and the eastern side is watershed lands of the Marin Municipal Water District. __TOC__
Setting.

Geographic entities mentioned:
surface_form: bolinas ridge
instance_of: Mountain
countries: United States
coordinates: lat: 37.907222222222
lon: -122.62027777778
A popular site for hiking and biking, Mount Tamalpais, where Bolinas Ridge is located, offers many different trails and paths for visitors. A popular trail is the Bolinas Ridge Trail which is a loop that connects to Samuel Taylor Park and is about 16.9 kilometers (or 10.5 miles). In terms of weather, the temperature on Mount Tamalpais is fairly cool, generally somewhere between 43°F and 72°F.

Geographic entities mentioned:
surface_form: bolinas ridge
instance_of: Mountain
countries: United States
coordinates: lat: 37.907222222222
lon: -122.62027777778
Specifically, starting from the Jewell Trail Junction, the Bolinas Ridge area is mostly grasslands until about a quarter of the way down the Bolinas Ridge Trail, where the trail starts to border a forest made up of Douglas fir and some Coast redwoods. Fauna.

Geographic entities mentioned:
surface_form: bolinas ridge
instance_of: Mountain
countries: United States
coordinates: lat: 37.907222222222
lon: -122.62027777778
surface_form: bolinas ridge
instance_of: Mountain
countries: United States
coordinates: lat: 37.907222222222
lon: -122.62027777778
Between 1993 and 1995, he worked in several public functions. Under Laurent Kabila. . He then held the following positions. Role in the peace process of the Great Lakes region. As Commissioner General of the Government responsible for monitoring the peace process in the Great Lakes region he was one of the principal negotiators of the 2002 peace deal. Role in the 2006 election campaign.

Geographic entities mentioned:
surface_form: Great Lakes region
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
By the town of Waren on the northern shore of the lake is the Binnenmüritz, which contains the deepest point of the lake (−31 metres), and only has a narrow strait connecting it to the main basin of Lake Müritz. At the southern shore is the Little Müritz (&quot;Kleine Müritz&quot;) from which the Müritzarm and the Müritzsee branch off further to the south.

Geographic entities mentioned:
surface_form: Binnenmüritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.4325
lon: 12.776944444444
surface_form: binnenmüritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.4325
lon: 12.776944444444
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
But by 1739 the mill reservoir had been lowered by around. In the wake of two adjustments to the Elde and two further changes to the mill impoundment the water level reached its present level of in 1836. Settlements. The largest town on Lake Müritz is Waren (Müritz). Other settlements are (clockwise) Rechlin, Priborn, Vipperow, Ludorf, Müritz, Gotthun, Sietow and Klink.

Geographic entities mentioned:
surface_form: Müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
By the town of Waren on the northern shore of the lake is the Binnenmüritz, which contains the deepest point of the lake (−31 metres), and only has a narrow strait connecting it to the main basin of Lake Müritz. At the southern shore is the Little Müritz (&quot;Kleine Müritz&quot;) from which the Müritzarm and the Müritzsee branch off further to the south.

Geographic entities mentioned:
surface_form: müritzsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.275016666667
lon: 12.663116666667
surface_form: müritzarm
instance_of: Lake
countries: Germany
coordinates: lat: 53.314161111111
lon: 12.685433333333
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
surface_form: kleine müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.330555555556
lon: 12.705555555556
Lake Müritz measures about from north to south and about from east to west; and has a catchment area of about. The Müritz is crossed by the River Elde from south to north and has a link to the Kölpinsee in the west from the Binnenmüritz via the Reeck Canal (also Eldenburg Canal) which is a good two kilometres long.

Geographic entities mentioned:
surface_form: binnenmüritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.4325
lon: 12.776944444444
surface_form: kölpinsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.500833333333
lon: 12.580555555556
Müritz. The Müritz (; from Slavic &quot;little sea&quot;) is a lake in Mecklenburg-Vorpommern, northern Germany. Its area is, which makes it the second largest lake in Germany (after Lake Constance) and the largest lake located entirely within German territory. Its maximum depth is. It is fed and drained by the river Elde.

Geographic entities mentioned:
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
Its maximum depth is. It is fed and drained by the river Elde. Part of the Müritz and adjacent forests and wetlands are protected by the Müritz National Park. The former Müritz district was named after the lake. The biggest towns bordering the lake are Waren (Müritz) and Röbel, both major centres of tourism in the Mecklenburg Lake District.

Geographic entities mentioned:
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
It is fed and drained by the river Elde. Part of the Müritz and adjacent forests and wetlands are protected by the Müritz National Park. The former Müritz district was named after the lake. The biggest towns bordering the lake are Waren (Müritz) and Röbel, both major centres of tourism in the Mecklenburg Lake District. Lake Müritz is part of the Müritz-Elde Waterway, a Class I federal waterway.

Geographic entities mentioned:
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
It is fed and drained by the river Elde. Part of the Müritz and adjacent forests and wetlands are protected by the Müritz National Park. The former Müritz district was named after the lake. The biggest towns bordering the lake are Waren (Müritz) and Röbel, both major centres of tourism in the Mecklenburg Lake District. Lake Müritz is part of the Müritz-Elde Waterway, a Class I federal waterway.

Geographic entities mentioned:
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
The former Müritz district was named after the lake. The biggest towns bordering the lake are Waren (Müritz) and Röbel, both major centres of tourism in the Mecklenburg Lake District. Lake Müritz is part of the Müritz-Elde Waterway, a Class I federal waterway. It is managed by the Lauenburg Waterway and Shipping Authority (&quot;Wasser- und Schifffahrtsamt Lauenburg&quot;). Divisions.

Geographic entities mentioned:
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
At the southern shore is the Little Müritz (&quot;Kleine Müritz&quot;) from which the Müritzarm and the Müritzsee branch off further to the south. Lake Müritz measures about from north to south and about from east to west; and has a catchment area of about.

Geographic entities mentioned:
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
Because it also feeds the River Havel to the east via the Mirow Canal, which is part of the Müritz-Havel Waterway, and the Bolter Canal as well as via the chains of adjoining lakes, it has artificially been turned into a bifurcated waterway. Creation. Lake Müritz was formed during the Weichselian glaciation between the Pomeranian and the Frankfurt Stages.

Geographic entities mentioned:
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
Local services provided in the London area included taxis, limousines, school buses, paratransit services, minibus charters, shuttle services and airport services. It also operated Foot's Bay Marina on Lake Joseph in Muskoka, and Trillium Sport Aviation Inc., a 50 percent owned affiliate, based at London International Airport.

Geographic entities mentioned:
surface_form: Lake Joseph
instance_of: Lake
countries: Canada
coordinates: lat: 45.17444444444445
lon: -79.7238888888889
Capital punishment in the Isle of Man. There is a long history of capital punishment in the Isle of Man. Until the 17th century, many convicted prisoners were executed at Hango Hill. Capital punishment in the Isle of Man was formally abolished in 1993. The Isle of Man is a British Crown Dependency, but not part of the United Kingdom (which had effectively abolished capital punishment in 1965).

Geographic entities mentioned:
surface_form: Hango Hill
instance_of: Mountain
countries: Isle of Man
coordinates: lat: 54.0767
lon: -4.63833
List of islands of Azerbaijan. Azerbaijan has many islands along the coast of the Caspian Sea. Most are part of the Baku Archipelago.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Mattmarksee. __NOTOC__
Mattmark dam is a reservoir in the Saas Valley of the Canton of Valais, Switzerland. The Mattmark dam was built from 1960 to 1965. The lake's surface area is. The lake lies at a height of 2,197 metres above sea level, between the massifs of the Rimpfischhorn and Stellihorn. The highest peak visible from the lake is the Strahlhorn (4,190 m). Engineering and dimensions.

Geographic entities mentioned:
surface_form: Rimpfischhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.023055555556
lon: 7.8838888888889
surface_form: Stellihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.036388888889
lon: 8.0022222222222
surface_form: stellihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.1669
lon: 7.73931
Mattmarksee. __NOTOC__
Mattmark dam is a reservoir in the Saas Valley of the Canton of Valais, Switzerland. The Mattmark dam was built from 1960 to 1965. The lake's surface area is. The lake lies at a height of 2,197 metres above sea level, between the massifs of the Rimpfischhorn and Stellihorn. The highest peak visible from the lake is the Strahlhorn (4,190 m). Engineering and dimensions.

Geographic entities mentioned:
surface_form: Strahlhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.013222222222
lon: 7.90175
surface_form: strahlhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.4528
lon: 8.09519
surface_form: strahlhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.38614
lon: 7.90811
The highest peak visible from the lake is the Strahlhorn (4,190 m). Engineering and dimensions. Mattmark is the largest rock-fill/earth dam in Europe: a 120 m-high embankment 780 m long that impounds up to 100 million cubic metres of water behind a 373 m-wide crest. Construction began in 1958 and the first full impoundment was reached in 1969, two years after commissioning.

Geographic entities mentioned:
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
Mattmark disaster. On 30 August 1965, 88 construction workers, 56 of them of Italian nationality, were buried under 2,000,000 m³ of ice and debris by a glacier collapse of the Allalin glacier. The risk involved in constructing the accommodation barracks directly below the glacier tongue, which eventually broke off, was not taken into account.

Geographic entities mentioned:
surface_form: allalin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.046138888889
lon: 7.8948055555556
Seven years after the accident, the Valais judiciary acquitted all 17 defendants, including engineers and managers of Elektrowatt and officials of the Swiss Accident Insurance Fund. In 2005, journalist Kurt Marti revealed that those responsible for the construction site knew about the dangers of the Allalin glacier and that the court ignored all incriminating facts in its decision.

Geographic entities mentioned:
surface_form: allalin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.046138888889
lon: 7.8948055555556