Sarmila/GeoWiki-Features huggingface dataset:
Ecology. Described by Wuerthner (2003) as a &quot;rocks and ice wilderness,&quot; much of the Mount Washington Wilderness consists of lava flows and rubble. However, it does include some forested areas, as well as 28 lakes in the northern and southwestern parts of the space. Vegetation in the area includes mountain hemlock, lodgepole pine, ponderosa pine, and whitebark pine.

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Lakes in the wilderness sustain populations of brook trout, cutthroat trout, and rainbow trout, and frogs can be observed around some of them. Human history. The barrenness of Mount Washington's surroundings means that it has seen little historical recreational use. A wagon road at McKenzie Pass was built in 1872, which was later paved during the 1930s and became Oregon Route 242.

Geographic entities mentioned:
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It received its name from the nearby McKenzie River, which in turn derived its name from Donald McKenzie, a fur trader who explored the area in 1812. On August 26, 1923, Mount Washington was climbed for the first time by six boys from Bend: Ervin McNeal, Phil Philbrook, Armin Furrer, Wilbur Watkins, Leo Harryman, and Ronald Sellars.

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Before Mount Washington's surroundings were designated a wilderness area in 1964, the Willamette National Forest administration had planned to open them to commercial timber production to address a shortage in Lane County, asserting that the land had little aesthetic or recreational merit. The area was established anyway, as Forest Service agents argued it would improve &quot;wilderness&quot;.

Geographic entities mentioned:
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Mount Washington forms part of the High Cascades physiographic region in central Oregon, an arc of Pliocene to Quaternary lava flows, cinder cones, and fissure vents that trend from north to south, with occasional large stratovolcanoes. Near Mount Washington, the High Cascades form a lava field with high-alumina, diktytaxitic basalt erupted from cinder cones.

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Near Mount Washington, the High Cascades form a lava field with high-alumina, diktytaxitic basalt erupted from cinder cones. These volcanoes have been eroded by glaciers and reduced to buttes in the Cascade arc, and much of the vents in the area were covered by Mount Washington.

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Some basalt lava flows occur on the edges of Mount Washington at the Cache Creek and Dry Creek canyons or as outcrops that form benches (long, relatively narrow strips of relatively level or gently inclined land bounded by distinctly steeper slopes above and below) about away from Washington from Patjens Lake to the McKenzie River.

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Whether Mount Washington is a stratovolcano or shield volcano is debated within the literature. Wood and Kienle (1990) refer to it as a &quot;mafic shield volcano,&quot; and the Global Volcanism Program of the Smithsonian Institution also considers it a shield volcano with a pyroclastic cone. Sherrod et al. (2004) classify Mount Washington as a &quot;steep-sided&quot; shield volcano. E. M.

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Taylor describes Mount Washington as a stratovolcano cone that reaches an elevation of above an older shield volcano, referring to it as &quot;a glacially-gutted Pleistocene stratovolcano.&quot; Hildreth (2007) likewise calls it a &quot;a glacially sculpted mafic stratocone [...] with a broad apron of mafic lavas.&quot; In his argument for classifying Mount Washington as a stratovolcano, Hildreth adds that it is made of composite materials with steep slopes and a high relief of.

Geographic entities mentioned:
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However, Hildreth acknowledges that there is morphological continuity from steep mafic cones into transitional, cone-shaped shield volcanoes like Olallie Butte. Mount Washington has a diameter of about. It has a summit cone, a volcanic plug comprised by cinder, lava flows, and intrusive rock that covers Washington's volcanic conduit. This plug is made of micronorite with a diameter of.

Geographic entities mentioned:
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There are dikes exposed throughout the summit cone, mostly oriented from north to south, with another dike swarm trending north from the central plug. The summit formed over a platform of basaltic andesite lavas from early eruptions at Mount Washington, made of thinner flows combined with pyroclastic rock. The volcano has a mafic composition, with subalkaline basalt and basaltic andesite.

Geographic entities mentioned:
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The volcano has a mafic composition, with subalkaline basalt and basaltic andesite. Lava flows from Washington exhibit breccia with plagioclase and olivine, with palagonite tuff at the northeastern slope of the mountain that might indicate a past subglacial eruption during Washington's cone-building phase.

Geographic entities mentioned:
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In the late Pleistocene, large glaciers extending more than to the east and west carved cirques into the slopes of the volcano. The George Lake and Dry Creek cirques, which face north and northeast, respectively, show evidence of holding glaciers similar to those documented at Canyon Creek cirque on Three Fingered Jack with moraines.

Geographic entities mentioned:
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Major cinder cones in the wilderness include Belknap Crater, Twin Craters, Scott Mountain, and the Sand Mountain craters. Eruptions from a chain of spatter cones mark the most recent activity at Mount Washington. About one mile in length, they trend northeast, with their mid-section parallel to depressions in the Cache Creek valley between Mount Washington and Blue Lake Crater.

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Eruptions from a chain of spatter cones mark the most recent activity at Mount Washington. About one mile in length, they trend northeast, with their mid-section parallel to depressions in the Cache Creek valley between Mount Washington and Blue Lake Crater. The northernmost vent of Mount Washington has a depth of and likely only ever erupted volcanic gas.

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Mount Washington basaltic andesite. There are four major types of basalt and basaltic andesite in the central Cascades: early high-alumina olivine tholeiitic (HAOT) basalt, normal High Cascade HAOT basalt, North Sister basaltic andesites, and Mount Washington type basaltic andesites.

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It also extends to the east and west of the major Cascade arc. Otherwise, the Mount Washington and North Sister basaltic andesites display lithologic similarities including a dearth of pyroxene phenocrysts and augite microphenocrysts, and both groups were probably near-primary melts.

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Its volcanic edifice was produced through the eruption of basaltic andesite and mafic volcanic ash, the latter being preserved as palagonite tuff along the northeastern and southwestern flanks of the summit cone. Compared to larger stratovolcanoes in the Cascade volcanic arc, Mount Washington, like the rest of Oregon's Matterhorns, had a relatively short eruptive life.

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Compared to larger stratovolcanoes in the Cascade volcanic arc, Mount Washington, like the rest of Oregon's Matterhorns, had a relatively short eruptive life. Several spatter cones produced basaltic andesite on the lower northeastern side of the volcano, following a fissure that reached from Washington's summit.

Geographic entities mentioned:
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Several spatter cones produced basaltic andesite on the lower northeastern side of the volcano, following a fissure that reached from Washington's summit. There were no lava flows from this eruption, nor at an eruption at the nearby Blue Lake Crater, which produced volcanic material that displayed petrographic similarities to the Mount Washington splatter cone deposits.

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instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
lon: -123.2459807
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 27.4354
lon: -81.5117
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 41.1635044
lon: -74.2603249
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1666
lon: -86.6321
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 42.1019
lon: -73.4325
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 38.9149
lon: -114.309
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 40.4271
lon: -80.0112
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.270827777778
lon: -71.303483333333
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.3321
lon: -121.839
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.4259
lon: -121.7
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.415277777778
lon: -121.51861111111
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 40.501944444444
lon: -114.03222222222
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 37.68
lon: -119.282
surface_form: blue lake
instance_of: Lake
countries: United States
coordinates: lat: 47.017222222222
lon: -95.005
Sherrod et al. (2004) argue that the spatter cones and activity from Blue Lake Crater represent the most recent eruptions near the McKenzie Pass and Santiam Pass region. It is still possible that new volcanic cones could be produced at the base of Mount Washington. However, according to Taylor, Causey, and MacLeod (1983), the volcano itself is unlikely to still be active. Recreation.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.5311964
lon: -123.2459807
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 42.1019
lon: -73.4325
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 38.9149
lon: -114.309
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 40.4271
lon: -80.0112
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.270827777778
lon: -71.303483333333
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 44.3321
lon: -121.839
surface_form: mount washington
instance_of: Mountain
countries: United States
coordinates: lat: 47.4259
lon: -121.7
Recreation. While the area is not used as frequently as many other wilderness areas in the Oregon branch of the Cascade Range, it offers scenic lakes and trails. The Pacific Crest Trail passes over the western side of Mount Washington. Other trails include a loop around the Patjens Lakes, the Hand Lake trail, and the Benson Lake route. The U.S.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Recreation. While the area is not used as frequently as many other wilderness areas in the Oregon branch of the Cascade Range, it offers scenic lakes and trails. The Pacific Crest Trail passes over the western side of Mount Washington. Other trails include a loop around the Patjens Lakes, the Hand Lake trail, and the Benson Lake route. The U.S.

Geographic entities mentioned:
surface_form: benson lake
instance_of: Lake
countries: United States
coordinates: lat: 38.01525
lon: -119.52958
Washington is part of the informal group of volcanoes known as Oregon's Matterhorns, which includes Mount Thielsen, Three Fingered Jack, Mount Bailey, and Diamond Peak. The name originates from the spire-like appearance of the volcanoes' summits, which resembles the pinnacle of the Matterhorn in Switzerland.

Geographic entities mentioned:
surface_form: mount thielsen
instance_of: Mountain
countries: United States
coordinates: lat: 43.152837292
lon: -122.066514283
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: mount bailey
instance_of: Mountain
countries: United States
coordinates: lat: 43.155144764
lon: -122.219995761
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: three fingered jack
instance_of: Mountain
countries: United States
coordinates: lat: 44.478965122
lon: -121.843058797
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
surface_form: mount bailey
instance_of: Mountain
countries: United States
coordinates: lat: 39.4153
lon: -105.46
Mount Washington formed during the late Pleistocene epoch; the volcano itself is not older than a few hundred thousand years. Harris (2005) estimates that it has not erupted for more than 250,000 years, similar to Mount Thielsen; this date is supported by James, Manga, and Rose (1999). Paleomagnetic evidence suggests that the volcano and associated lava flows exhibit normal magnetic polarity.

Geographic entities mentioned:
surface_form: mount thielsen
instance_of: Mountain
countries: United States
coordinates: lat: 43.152837292
lon: -122.066514283
However, it does include some forested areas, as well as 28 lakes in the northern and southwestern parts of the space. Vegetation in the area includes mountain hemlock, lodgepole pine, ponderosa pine, and whitebark pine. Ponderosa pine occurs at the eastern base of the volcano, with Douglas fir on the western side. Vegetation is sparse on lava-covered surfaces.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
It is 36 km in width and wide open to the northwest. It is limited in the north by Cape Svyatoy Nos, a prominent headland. This bay is in a vast region of wetlands. Lake Bustakh, the largest lake in the neighboring area, lies 37 km inland from the shores of the bay. Owing to its northerly location the Ebelyakh Bay is covered with ice most of the year.

Geographic entities mentioned:
surface_form: Lake Bustakh
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 72.53333
lon: 142
Guadalimar. The Guadalimar () is a river of the Iberian Peninsula, a right-bank tributary of the Guadalquivir. Its 180-km long course spans across the Spanish provinces of Albacete and Jaén. The river's main tributaries are the Guadalmena, the Giribaile and the. The hydronym comes from the Arabic &quot;al-Wādī-l-aḥmar&quot; (الوادي الأحمر 'the red river bed').

Geographic entities mentioned:
surface_form: Guadalmena
instance_of: Watercourse
countries: Spain
coordinates: lat: 38.312675
lon: -2.9384194444444
Guadalimar. The Guadalimar () is a river of the Iberian Peninsula, a right-bank tributary of the Guadalquivir. Its 180-km long course spans across the Spanish provinces of Albacete and Jaén. The river's main tributaries are the Guadalmena, the Giribaile and the. The hydronym comes from the Arabic &quot;al-Wādī-l-aḥmar&quot; (الوادي الأحمر 'the red river bed').

Geographic entities mentioned:
surface_form: guadalimar
instance_of: Watercourse
countries: Spain
coordinates: lat: 37.98333333
lon: -3.73333333
Guadalimar. The Guadalimar () is a river of the Iberian Peninsula, a right-bank tributary of the Guadalquivir. Its 180-km long course spans across the Spanish provinces of Albacete and Jaén. The river's main tributaries are the Guadalmena, the Giribaile and the. The hydronym comes from the Arabic &quot;al-Wādī-l-aḥmar&quot; (الوادي الأحمر 'the red river bed').

Geographic entities mentioned:
surface_form: الوادي الأحمر
instance_of: Watercourse
countries: Spain
coordinates: lat: 37.98333333
lon: -3.73333333
Sokolska planina. Sokolska planina (Serbian Cyrillic: Соколска планина) is a mountain in western Serbia, near the town of Krupanj. Its highest peak &quot;Rožanj&quot; has an elevation of 973 meters above sea level.

Geographic entities mentioned:
surface_form: sokolska planina
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.28277778
lon: 19.45972222
The Italian territory extends over about 10° of latitude, therefore, while remaining in the context of temperate climates without extremes of heat, cold or aridity, the climatic difference between the north and the south of the country is not at all negligible, going from the nival climates of the Alpine peaks to the cool semi-continental temperate climate of the Po Valley, to the Mediterranean climate of the central-southern coasts and the islands.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
In most of the inland northern and central regions, the climate ranges from humid subtropical to humid continental and oceanic. In particular, the climate of the Po Valley geographical region is mostly continental, with harsh winters and hot summers. The coastal areas of Liguria, Tuscany and most of the South generally fit the Mediterranean climate stereotype (Köppen climate classification).

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Ampatuyoc (Churcampa). Ampatuyoc (possibly from in the Quechua spelling &quot;Hamp'atuyuq&quot;; &quot;hamp'atu&quot; frog, &quot;-yuq&quot; a suffix, &quot;the one with a frog (or frogs)&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It is located in the Huancavelica Region, Churcampa Province, Churcampa District. A lake named Chinchiqucha lies at its feet.

Geographic entities mentioned:
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -12.56138889
lon: -74.46277778
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6528
lon: -74.3989
surface_form: ampatuyoc (churcampa)
instance_of: Mountain
countries: Peru
coordinates: lat: -12.67583333
lon: -74.39527778
Ampatuyoc (Churcampa). Ampatuyoc (possibly from in the Quechua spelling &quot;Hamp'atuyuq&quot;; &quot;hamp'atu&quot; frog, &quot;-yuq&quot; a suffix, &quot;the one with a frog (or frogs)&quot;) is a mountain in the Andes of Peru which reaches a height of approximately. It is located in the Huancavelica Region, Churcampa Province, Churcampa District. A lake named Chinchiqucha lies at its feet.

Geographic entities mentioned:
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -12.56138889
lon: -74.46277778
surface_form: hamp'atuyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6528
lon: -74.3989
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6528
lon: -74.3989
surface_form: hamp'atuyuq
instance_of: Mountain
countries: Peru
coordinates: lat: -12.67583333
lon: -74.39527778
surface_form: ampatuyoc
instance_of: Mountain
countries: Peru
coordinates: lat: -12.67583333
lon: -74.39527778
It is part of the Ishim River basin. The bottom is flat and the lakeshore is clayey and gently sloping, Ulken Koskol is located in an area where there are numerous lakes. Kishi Koskol lies to the SSE, Shalkar to the south and lake Saumalkol to the southwest. River Kamysakty has its sources a little to the NW of the northern end of Ulken Koskol. The lake is fed mainly by snow and precipitation.

Geographic entities mentioned:
surface_form: Saumalkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.27901
lon: 68.16772
surface_form: saumalkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.81289
lon: 74.9927
surface_form: shalkar
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.55
lon: 51.68333333
Ulken Koskol. Ulken Koskol (;) is a salt lake in Aiyrtau District, North Kazakhstan Region, Kazakhstan. Saumalkol town, the district capital (formerly Volodarskoye), is located to the southwest. Kenashchi village lies to the southwest of the southwestern shore. Geography. Ulken Koskol is an endorheic lake in the Kazakh Uplands. It is part of the Ishim River basin.

Geographic entities mentioned:
surface_form: saumalkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.27901
lon: 68.16772
surface_form: saumalkol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.81289
lon: 74.9927
Ulken Koskol. Ulken Koskol (;) is a salt lake in Aiyrtau District, North Kazakhstan Region, Kazakhstan. Saumalkol town, the district capital (formerly Volodarskoye), is located to the southwest. Kenashchi village lies to the southwest of the southwestern shore. Geography. Ulken Koskol is an endorheic lake in the Kazakh Uplands. It is part of the Ishim River basin.

Geographic entities mentioned:
surface_form: ulken koskol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.37833
lon: 68.36806
Saumalkol town, the district capital (formerly Volodarskoye), is located to the southwest. Kenashchi village lies to the southwest of the southwestern shore. Geography. Ulken Koskol is an endorheic lake in the Kazakh Uplands. It is part of the Ishim River basin. The bottom is flat and the lakeshore is clayey and gently sloping, Ulken Koskol is located in an area where there are numerous lakes.

Geographic entities mentioned:
surface_form: ulken koskol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.37833
lon: 68.36806
Kenashchi village lies to the southwest of the southwestern shore. Geography. Ulken Koskol is an endorheic lake in the Kazakh Uplands. It is part of the Ishim River basin. The bottom is flat and the lakeshore is clayey and gently sloping, Ulken Koskol is located in an area where there are numerous lakes. Kishi Koskol lies to the SSE, Shalkar to the south and lake Saumalkol to the southwest.

Geographic entities mentioned:
surface_form: ulken koskol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.37833
lon: 68.36806
It is part of the Ishim River basin. The bottom is flat and the lakeshore is clayey and gently sloping, Ulken Koskol is located in an area where there are numerous lakes. Kishi Koskol lies to the SSE, Shalkar to the south and lake Saumalkol to the southwest. River Kamysakty has its sources a little to the NW of the northern end of Ulken Koskol. The lake is fed mainly by snow and precipitation.

Geographic entities mentioned:
surface_form: ulken koskol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.37833
lon: 68.36806
River Kamysakty has its sources a little to the NW of the northern end of Ulken Koskol. The lake is fed mainly by snow and precipitation. Since the water is salty and has high mineral content it is not suitable for drinking. Ulken Koskol is largely surrounded by agricultural fields. Flora. Sedges and fescue grow in the fields nearby that are not plowed.

Geographic entities mentioned:
surface_form: ulken koskol
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.37833
lon: 68.36806
It was depopulated before the outbreak of the 1948 Arab-Israeli war. Location. The village was on the north edge of a hill at the edge of a wadi bed, overlooking the Jezreel Valley and the Nazareth hills to the north and northeast. It was the smallest of a group of three villages (known collectively as al-Ghubayyat) located together; the others were Al-Ghubayya al-Fawqa and Al-Ghubayya al-Tahta.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
The lake is a popular area for hiking, swimming, and fishing cutthroat trout. Lower Florence Lake is located further down the slope from Upper Florence Lake, approximately 15 miles west of the city of Leavenworth. Self-issued Alpine Lake Wilderness permit is required for transit within the Lake Alice area.

Geographic entities mentioned:
surface_form: Upper Florence Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6570413
lon: -120.9352396
surface_form: lower florence lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6537191
lon: -120.9393131
The lake is a popular area for hiking, swimming, and fishing cutthroat trout. Lower Florence Lake is located further down the slope from Upper Florence Lake, approximately 15 miles west of the city of Leavenworth. Self-issued Alpine Lake Wilderness permit is required for transit within the Lake Alice area.

Geographic entities mentioned:
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 29.6417
lon: -82.3567
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 44.8779156
lon: -96.6338965
surface_form: alpine lake
instance_of: Lake
countries: United States
coordinates: lat: 37.9622
lon: -119.304
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 47.22277778
lon: -95.08277778
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 47.6474147
lon: -120.917581
surface_form: lake wilderness
instance_of: Lake
countries: United States
coordinates: lat: 47.3746
lon: -122.036
Chatter Creek Trail #1580 is approximately 5.5 miles long and travels fairly closely to the course of Chatter Creek. The trail leads past Lake Sylvester and Lake Alice reaching and joining Icicle Ridge Trail #1580 on the north skirt of Grindstone mountain. Upper Florence Lake is located just under the main trail along the summit of Icicle Ridge, west out of the junction with Chatter Creek Trail.

Geographic entities mentioned:
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 29.6417
lon: -82.3567
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 44.8779156
lon: -96.6338965
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6978
lon: -115.905
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 47.22277778
lon: -95.08277778
surface_form: lake alice
instance_of: Lake
countries: United States
coordinates: lat: 47.6474147
lon: -120.917581
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6373
lon: -120.9134
surface_form: lake sylvester
instance_of: Lake
countries: United States
coordinates: lat: 47.6340416
lon: -120.9247133
Lower Florence Lake. Lower Florence Lake is a freshwater lake located on the west skirt of Ladies Peak and Cape Horn, and North of Grindstone Mountain, in Chelan County, Washington. The lake is a popular area for hiking, swimming, and fishing cutthroat trout. Lower Florence Lake is located further down the slope from Upper Florence Lake, approximately 15 miles west of the city of Leavenworth.

Geographic entities mentioned:
surface_form: cape horn
instance_of: Mountain
countries: United States
coordinates: lat: 47.657222222222
lon: -120.91694444444
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6978
lon: -115.905
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: lower florence lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6537191
lon: -120.9393131
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6373
lon: -120.9134
Campsites are located along the first few miles of Chatter Creek Trail until the trail becomes more forested around the bowls formed for Lakes Sylvester and Alice. Self-issued Alpine Lake Wilderness permit required for transit within the Grindstone Mountain area and can be obtained at the Chatter Creek Trailhead and the Campground past the Guard station.

Geographic entities mentioned:
surface_form: alpine lake
instance_of: Lake
countries: United States
coordinates: lat: 37.9622
lon: -119.304
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6978
lon: -115.905
surface_form: grindstone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.6373
lon: -120.9134
surface_form: lake wilderness
instance_of: Lake
countries: United States
coordinates: lat: 47.3746
lon: -122.036
Lower Florence Lake. Lower Florence Lake is a freshwater lake located on the west skirt of Ladies Peak and Cape Horn, and North of Grindstone Mountain, in Chelan County, Washington. The lake is a popular area for hiking, swimming, and fishing cutthroat trout. Lower Florence Lake is located further down the slope from Upper Florence Lake, approximately 15 miles west of the city of Leavenworth.

Geographic entities mentioned:
surface_form: lower florence lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6537191
lon: -120.9393131
Icicle Ridge Trail shortly afterward will bend left straight towards Upper Florence Lake over Mary ridge approximately 3/4 mile down the slope. Lower Florence Lake is further down the skirt of the ridge. Campsites are located along the first few miles of Chatter Creek Trail until the trail becomes more forested around the bowls formed for Lakes Sylvester and Alice.

Geographic entities mentioned:
surface_form: lower florence lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6537191
lon: -120.9393131
Self-issued Alpine Lake Wilderness permit is required for transit within the Lake Alice area. Along with neighboring lakes, Lake Florence was given its name by Albert Hale Sylvester, a topographer for the United States Geological Survey working throughout the North Cascades National Park Complex sometime between 1949 and 1957. Access.

Geographic entities mentioned:
surface_form: lake florence
instance_of: Lake
countries: United States
coordinates: lat: 28.0025
lon: -81.687
surface_form: lake florence
instance_of: Lake
countries: United States
coordinates: lat: 28.3260214
lon: -80.7840257
Chatter Creek Trail #1580 is approximately 5.5 miles long and travels fairly closely to the course of Chatter Creek. The trail leads past Lake Sylvester and Lake Alice reaching and joining Icicle Ridge Trail #1580 on the north skirt of Grindstone mountain. Upper Florence Lake is located just under the main trail along the summit of Icicle Ridge, west out of the junction with Chatter Creek Trail.

Geographic entities mentioned:
surface_form: upper florence lake
instance_of: Lake
countries: United States
coordinates: lat: 47.6570413
lon: -120.9352396