Sarmila/GeoWiki-Features huggingface dataset:
Artifacts dating to the Late Archaic period have been found at Lake Abitibi. Application of &quot;Abitibi&quot; to describe the lake and the people living in the area around it was first noted in The Jesuit Relations in 1640. One of the first Europeans in this area was Pierre de Troyes, who built a post on Lake Abitibi when he was on his way to capture English HBC posts on James Bay in 1686.

Geographic entities mentioned:
surface_form: lake abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
surface_form: abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
surface_form: abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
Being unproductive due to competition, the HBC abandoned Abitibi House in 1811. When two companies merged in 1821, the HBC took over the trading post of the North West Company on Lake Abitibi. The construction of the Grand Trunk Pacific Railway (now Canadian National Railway) through this district made it of some importance at the start of the 20th century. Lake Abitibi Islands.

Geographic entities mentioned:
surface_form: lake abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
surface_form: abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
The construction of the Grand Trunk Pacific Railway (now Canadian National Railway) through this district made it of some importance at the start of the 20th century. Lake Abitibi Islands. The Lake Abitibi Islands Provincial Park protects nearly all the islands on the Ontario side of Lake Abitibi. It includes 786 islands, from tiny shoals to large islands of up to.

Geographic entities mentioned:
surface_form: lake abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
surface_form: abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
The lake takes its name from the river. &quot;Abitibi&quot; comes from the Algonquin words &quot;abitah&quot;, meaning middle and &quot;nipi&quot; meaning water, possibly a reference to its geographic location between the Harricana (from the Algonquin word &quot;Nanikana&quot;, meaning &quot;the main way&quot;) to the east and the Kapuskasing&ndash;Mattagami river system to the west.

Geographic entities mentioned:
surface_form: abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
This moved the HBC to set up a post, called Abitibi House, on Lake Abitibi in 1794, located on the peninsula at the mouth of the Duparquet River. In subsequent decades this post, as well as competing posts of the North West Company, were rebuilt or moved to various locations around the lake and its islands. Being unproductive due to competition, the HBC abandoned Abitibi House in 1811.

Geographic entities mentioned:
surface_form: abitibi
instance_of: Lake
countries: Canada
coordinates: lat: 48.666666666666664
lon: -79.75
&quot;Palaestina Prima&quot; with its capital in Caesarea Maritima encompassed the central parts of Palestine, including the coastal plain, Judea, and Samaria. &quot;Palaestina Secunda&quot; had its capital in Scythopolis and included northern Transjordan, the lower Jezreel Valley, the Galilee, and the Golan area.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Kendu Bay. Kendu Bay is a bay and town in Kenya. The area is the part of Rachuonyo North District in Homa Bay County. Overview. It is located on the shores of Lake Victoria along Katito-Homa-Bay road. It is the headquarters of the district.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Saint Catherine's Monastery. Saint Catherine's Monastery (,), officially the Sacred Autonomous Royal Monastery of Saint Catherine of the Holy and God-Trodden Mount Sinai, is a Christian monastery located in the Sinai Peninsula of Egypt. Located at the foot of Mount Sinai, it was built between 548 and 565, and is the world's oldest continuously-inhabited Christian monastery.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
The monastery library holds unique and rare works, such as the Codex Sinaiticus and the Syriac Sinaiticus, as well as a collection of early Christian icons, including the earliest known depiction of Christ Pantocrator. Saint Catherine's has as its backdrop the three mountains it lies near: Willow Peak (possibly the biblical Mount Horeb, peak c.

Geographic entities mentioned:
surface_form: Willow Peak
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.555555555555557
lon: 33.96722222222222
Saint Catherine's has as its backdrop the three mountains it lies near: Willow Peak (possibly the biblical Mount Horeb, peak c. west); Jebel Arrenziyeb, peak c.1km south; and Mount Sinai (locally, by tradition identified with the biblical Mount Sinai; peak south). Christian traditions.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
Amenities. The Somerset Regional Council operates a public library at the corner of Michel and Main Streets (). The Lowood branch of the Queensland Country Women's Association meets at 106 Main Street (). The Fernvale Lowood Uniting Church is at 1503 Brisbane Valley Highway in Fernvale. Attractions. Nearby Lake Wivenhoe is a popular place for activities such as boating and fishing.

Geographic entities mentioned:
surface_form: Lake Wivenhoe
instance_of: Lake
countries: Australia
coordinates: lat: -27.25
lon: 152.51666666667
Bay View. Bay View is located on the southeast shore of the city of Milwaukee overlooking Lake Michigan. Bay View boundaries are Becher Street/Bay Street to the north, Morgan Avenue to the south, and Sixth Street to the west. Located about 3 miles (5 km) south of downtown on the lake, Bay View originally was developed as a company town by the Milwaukee Iron Company, located near its rolling mill.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Duncan Hollow. Duncan Hollow is a valley in Oregon County in the U.S. state of Missouri. Duncan Hollow bears the name of a pioneer citizen named Duncan who is buried in the valley in an unmarked grave.

Geographic entities mentioned:
surface_form: duncan hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.8033893
lon: -91.3370797
Duncan Hollow. Duncan Hollow is a valley in Oregon County in the U.S. state of Missouri. Duncan Hollow bears the name of a pioneer citizen named Duncan who is buried in the valley in an unmarked grave.

Geographic entities mentioned:
surface_form: duncan hollow
instance_of: Valley
countries: United States
coordinates: lat: 36.8033893
lon: -91.3370797
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
Brownie Lake. Brownie Lake is a lake in Hennepin County, Minnesota, and within the city limits of Minneapolis. It is the northernmost lake in the Minneapolis Chain of Lakes (Brownie Lake, Cedar Lake, Lake of the Isles, Bde Maka Ska, and Lake Harriet). It is within Brownie Lake Park, and administered by the Minneapolis Park and Recreation Board (MPRB). Hydrology.

Geographic entities mentioned:
surface_form: Lake of the Isles
instance_of: Lake
countries: United States
coordinates: lat: 44.954722
lon: -93.3075
surface_form: Bde Maka Ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3869
lon: -121.7
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 29.1925638
lon: -95.082994
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: lake harriet
instance_of: Lake
countries: United States
coordinates: lat: 44.921388888889
lon: -93.305277777778
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 46.221
lon: -93.404
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.97777778
lon: -94.46138889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5275
lon: -68.801111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.960277777778
lon: -93.321111111111
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.78972222
lon: -94.73388889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2144
lon: -92.571
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9111048
lon: -74.4729616
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.59
lon: -93.523333333333
There are no natural inflows to Brownie Lake, but it receives storm sewer runoff from six locations around the lake. Water flows out through a canal connecting Brownie to Cedar Lake, which is hydrologically connected to Lake of the Isles and Bde Maka Ska. Brownie Lake is part of the Minnehaha Creek Watershed District.

Geographic entities mentioned:
surface_form: Lake of the Isles
instance_of: Lake
countries: United States
coordinates: lat: 44.954722
lon: -93.3075
surface_form: Bde Maka Ska
instance_of: Lake
countries: United States
coordinates: lat: 44.941944444444
lon: -93.312222222222
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3869
lon: -121.7
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 29.1925638
lon: -95.082994
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 46.221
lon: -93.404
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.97777778
lon: -94.46138889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5275
lon: -68.801111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.960277777778
lon: -93.321111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.78972222
lon: -94.73388889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2144
lon: -92.571
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9111048
lon: -74.4729616
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.59
lon: -93.523333333333
Target Corporation relocated employees from this site in 2015, and put the property on the market. Recreational facilities. Brownie Lake is encircled by a packed dirt walking path. An additional paved multi-use path, the Cedar Lake Trail, runs north-south along Cedar Lake Parkway, just to the east and elevated above Brownie Lake. This path is part of the Grand Rounds National Scenic Byway.

Geographic entities mentioned:
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3869
lon: -121.7
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 29.1925638
lon: -95.082994
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 46.221
lon: -93.404
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.97777778
lon: -94.46138889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5275
lon: -68.801111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.960277777778
lon: -93.321111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.78972222
lon: -94.73388889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2144
lon: -92.571
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9111048
lon: -74.4729616
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.59
lon: -93.523333333333
A canoe/kayak rack is stationed near the dirt boat ramp at the northwest end of the lake, and rack spaces can be rented from the Minneapolis Park and Recreation Board. In the winter, the Chain of Lakes Ski Trail extends for 1 km from the tunnel to Cedar Lake, across the lake and up the western side of the basin, connecting up with the Theodore Wirth Park trails.

Geographic entities mentioned:
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3869
lon: -121.7
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 29.1925638
lon: -95.082994
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3743
lon: -74.3212
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 46.221
lon: -93.404
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.97777778
lon: -94.46138889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.5275
lon: -68.801111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.960277777778
lon: -93.321111111111
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 43.78972222
lon: -94.73388889
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2144
lon: -92.571
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 40.9111048
lon: -74.4729616
surface_form: cedar lake
instance_of: Lake
countries: United States
coordinates: lat: 44.59
lon: -93.523333333333
Hydrology. Brownie Lake is a meromictic lake, which means there are two layers of water in the lake with differing physical and chemical conditions, and which do not intermix in spring and fall as occurs in most lakes in the northern temperate zone. It is one of two meromictic bodies of water in Minneapolis, the other being Spring Lake.

Geographic entities mentioned:
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 28.0381
lon: -81.7351
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 44.76083333
lon: -92.96277778
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 44.700833333333
lon: -93.473888888889
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 42.719669
lon: -83.392527
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 42.325555555556
lon: -74.964444444444
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0111458
lon: -89.1607253
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 47.43638888888889
lon: -122.08888888888889
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 45.3667276
lon: -88.9628259
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6536
lon: -73.4215
Brownie Lake. Brownie Lake is a lake in Hennepin County, Minnesota, and within the city limits of Minneapolis. It is the northernmost lake in the Minneapolis Chain of Lakes (Brownie Lake, Cedar Lake, Lake of the Isles, Bde Maka Ska, and Lake Harriet). It is within Brownie Lake Park, and administered by the Minneapolis Park and Recreation Board (MPRB). Hydrology.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
Hydrology. Brownie Lake is a meromictic lake, which means there are two layers of water in the lake with differing physical and chemical conditions, and which do not intermix in spring and fall as occurs in most lakes in the northern temperate zone. It is one of two meromictic bodies of water in Minneapolis, the other being Spring Lake.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
A chemocline separates the top layer of the lake, which contains dissolved oxygen, from the bottom layer, which is anoxic. There are no natural inflows to Brownie Lake, but it receives storm sewer runoff from six locations around the lake. Water flows out through a canal connecting Brownie to Cedar Lake, which is hydrologically connected to Lake of the Isles and Bde Maka Ska.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
There are no natural inflows to Brownie Lake, but it receives storm sewer runoff from six locations around the lake. Water flows out through a canal connecting Brownie to Cedar Lake, which is hydrologically connected to Lake of the Isles and Bde Maka Ska. Brownie Lake is part of the Minnehaha Creek Watershed District.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
Brownie Lake is part of the Minnehaha Creek Watershed District. A distinguishing feature of Brownie Lake is the high concentrations of dissolved iron (Fe), which have historically been between 1 and 2 mmol/L in the bottom part of the lake, and still exceed 1 mmol/L today.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
From 1950 until the 1990s, an industrial cooling outlet from what was the Prudential Office Building with average total iron concentrations of 7 μmol/L was discharged into Brownie Lake at a rate of 50,000 gallons per day. Therefore, surface concentrations of dissolved iron were higher in the 1970s (~ 2 μmol/L) than they are today (< 1 μmol/L).

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
Therefore, surface concentrations of dissolved iron were higher in the 1970s (~ 2 μmol/L) than they are today (< 1 μmol/L). Total phosphate concentrations in Brownie Lake can reach 46 μmol/L. In 2014, Brownie had total phosphorus levels considered eutrophic by the Minnesota Pollution Control Agency (MPCA).

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
Some of the phosphate inputs are likely anthropogenic. A pumping station was created in 1957 to pump water from Bassett Creek into Brownie Lake in order to maintain the desired water levels in the Chain of Lakes. In 1966, water from the Mississippi River was pumped into Bassett Creek, which then entered Brownie.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Minnesota began using salt to de-ice roads in 1950. Past stormwater inputs from nearby Interstate 394 were likely a direct source of salt. Road salt has been linked to enhanced chemical stratification in Twin Cities lakes, including Brownie Lake. While lake lowering initiated the onset of meromixis (see History), road salt pollution stabilizes the lake against intermixing. Geology.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
While lake lowering initiated the onset of meromixis (see History), road salt pollution stabilizes the lake against intermixing. Geology. The geology of Minneapolis in the vicinity of Brownie Lake generally consists of lower Paleozoic carbonates and clastic rocks overlain by unconsolidated Pleistocene glacial sediments. Holocene alluvium and wetland sediments are also found adjacent to the lake.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
Holocene alluvium and wetland sediments are also found adjacent to the lake. The uplands immediately surrounding Brownie Lake are composed of a mixture of sands, gravels, and glacial tills deposited during the Last Glacial Maximum by the Laurentide Ice Sheet between 16,500 and 13,900 cal yr BP.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
These deposits include a mixture of sediments derived from both northwest- and northeast-sourced glacial ice, with northeast-sourced sediments containing a greater abundance of iron-rich rocks from the Lake Superior region. Brownie Lake lies on the edge of a buried bedrock valley filled with as much as 300 feet of glacial debris.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
These buried valleys have little surface expression, but are associated with clusters of lakes, and locally influenced the course of modern rivers and streams. A bicycle guide to the Geology of the Chain of Lakes includes a stop at Brownie Lake. Natural history. Open water plants in Brownie Lake include yellow and white water lilies, coontail, pondweeds, and lesser duckweed.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
A bicycle guide to the Geology of the Chain of Lakes includes a stop at Brownie Lake. Natural history. Open water plants in Brownie Lake include yellow and white water lilies, coontail, pondweeds, and lesser duckweed. The aquatic invasive species Eurasian watermilfoil and curly-leaf pondweed are also present.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
The Minnesota Department of Natural Resources reports a number of fish taxa in Brownie Lake including black bullhead, black crappie, bluegill, hybrid sunfish, largemouth bass, northern pike, pumpkinseed, tiger muskellunge, walleye, yellow bullhead, yellow perch, bowfin (dogfish), common carp, white sucker, fathead minnow, and golden shiner.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
Phytoplankton predominate over zooplankton in Brownie Lake. In recent monitoring (2012), Cryptomonads (Cryptophyta) were most abundant in winter. Chrysophyte populations peaked in April, while Dinoflagellates (Pyrrhophyta) and green algae (Chlorophyta) both peaked in June.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
Chrysophyte populations peaked in April, while Dinoflagellates (Pyrrhophyta) and green algae (Chlorophyta) both peaked in June. The summer was then dominated by cyanobacteria (Cyanophyta), with an increase in Cryptomonad (Cryptophyta) abundance by October. Brownie Lake is inhabited by methanogenic archaea in the anoxic bottom waters, which produce methane (CH4; natural gas).

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
A population of methanotrophic bacteria at the chemocline<nowiki/>consume methane diffusing out of the anoxic portion of the lake by reaction with oxygen. A new species of bacteria was discovered from Brownie Lake in 2021 and named &quot;Candidatus&quot; Chlorobium masyuteum&quot;. This organism is photosynthetic, and uses sunlight energy to convert dissolved iron into rust.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
McNair named the lake &quot;Brownie&quot;, after a nickname of his daughter, Agnes McNair. It was formerly called &quot;Hillside Harbor&quot;. Brownie Lake was then acquired by the expansion of the Glenwood Park, now Theodore Wirth Park, in 1907. In 1867 the St. Paul & Pacific Railroad Company built a railroad track across the southern end of Brownie Lake. In 1883 James J. Hill took over the St.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
In 1883 James J. Hill took over the St. Paul & Pacific Railroad and expanded the track into a double track mainline that connected the wheat fields west of the Mississippi to the flour mills of Minneapolis. The expansion of the railroad embankment in 1883 filled in the southwestern arm of Brownie Lake, and reduced the surface area of Brownie Lake by 34%.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
The hydraulic connections reduced the lake level of Brownie Lake by 2 to 3 meters, which drew Brownie Lake down into its steep-sided local catchment, significantly reducing its surface area, and increasing shelter from wind.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
This path is part of the Grand Rounds National Scenic Byway. Within Brownie Lake Park, a 1.4-mile single track mountain biking trail loops along the western slope of the Brownie Lake basin. This trail connects to the Glenwood Loop and the Southwest Wirth loop, and all trails are maintained by Minnesota Off-Road Cyclists.

Geographic entities mentioned:
surface_form: brownie lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.9675
lon: -93.32444444444444
When the wind no longer mixed oxygenated surface water with the bottom waters of Brown Lake, sedimentary iron became soluble and was mobilized into the anoxic bottom water at a concentration several hundred times greater than the surface water, increasing the relative density of the bottom water and beginning a positive feedback system in which other ions such as sodium and chloride could also accumulate, further minimizing the probability that wind energy would be sufficient to mix surface water into the increasingly dense bottom water.

Geographic entities mentioned:
surface_form: brown lake
instance_of: Lake
countries: United States
coordinates: lat: 43.241993
lon: -74.4908049
In 2024, &quot;Frankfurt am Main&quot; was selected to undertake an around the world deployment, accompanying the frigate. The tanker along with &quot;Baden-Württemberg&quot; participated in the Maritime Partnership Exercise (MPX) with the Indian Navy's from 21 to 23 October 2024 in the Bay of Bengal and the Indian Ocean.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Prior to the pearl trade in Hyderabad, pearls were sourced from Basra, Iraq. The pearls from this city were prized for its hardness unlike those found in the Bay of Bengal, which are softer and, thus, less durable. However, the discovery of oil and the later establishment of the oil industry polluted the Persian Gulf, led to the decline of pearl trade in Basra.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The area is bounded on the north by Cranberry Lake, a portion of the Oswegatchie River, the road leading to Inlet and private lands; on the east by the Colton town line and private lands in the vicinity of Gull Lake, a road leading to Gull Lake and the Remsen to Lake Placid railroad; on the south by Stillwater Reservoir; on the southwest by the Pepperbox Wilderness Area and on the west by the Aldrich Pond Wild Forest and the Watson East Triangle Wild Forest.

Geographic entities mentioned:
surface_form: Cranberry Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.172222222222
lon: -74.823888888889
The East Branch Oswegatchie on the parts across from High Rock still has very tall white pines, across it on an adjacent tract of state land, that was acquired by New York State in a tax sale in 1884. Several fires burned large areas south of Cranberry Lake. The blowdowns of 1950 and 1995 did considerably more damage. South of the St.

Geographic entities mentioned:
surface_form: Cranberry Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.172222222222
lon: -74.823888888889
In addition to these spots, other points of interest to the hiker, camper and fisherman are: High Falls on the Oswegatchie River; Alder Bed Flow on the Middle Branch of the Oswegatchie River; Cat Mountain; Sand Lake; Wolf Pond; Big Deer Pond; Nicks Pond; &quot;The Plains,&quot; which are very similar in soil and cover type to that of the Moose River Plains; and the numerous, clear, spring-fed ponds, most of which support brook trout.

Geographic entities mentioned:
surface_form: Cat Mountain
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 26.79809
lon: 117.02816
surface_form: Big Deer Pond
instance_of: Lake
countries: United States
coordinates: lat: 44.068577777778
lon: -74.838708333333
The river has received increasing use in recent years and care must be taken that such use does not result in resource degradation. There is a 3.5 mile canoe carry at approximately 18 miles upstream that leads the traveler to Lows Lake via Big Deer Pond. The existing lean-tos on the river will be phased out and ultimately replaced by primitive tent sites.

Geographic entities mentioned:
surface_form: Big Deer Pond
instance_of: Lake
countries: United States
coordinates: lat: 44.068577777778
lon: -74.838708333333
There is also a canoe carry from Chair Rock Creeks' inlet on Cranberry Lake to Grass Pond on Lows Lake. Public access. The Five Ponds area is accessible to the public from the north and also from the south if one has a boat or canoe, from the east from the vicinity of Lake Lila in the William C. Whitney Wilderness Area and along the Remsen to Lake Placid railroad.

Geographic entities mentioned:
surface_form: Lake Lila
instance_of: Lake
countries: United States
coordinates: lat: 44.002222222222
lon: -74.755555555556
Hasan Baba Tekke. The Hasan Baba Tekke () is a former &quot;tekke&quot; (a house for the gathering of dervishes) in the Vale of Tempe, Greece. The &quot;tekke&quot; is a large complex, now largely ruined, near the village of, on the banks of the Pineios River.

Geographic entities mentioned:
surface_form: Vale of Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
It may provide evidence for the formation of gas giant planets by disk instability. Discovery and follow-up studies. AB Aur b was discovered by a team led by Thayne Currie, Kellen Lawson, and Glenn Schneider using the Subaru Telescope on Mauna Kea, Hawaii and the Hubble Space Telescope (HST).

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
It has numerous springs, which makes it attractive for tourism, the largest source of revenue, together with dryland farming and animal husbandry. It has a water bottling facility. The center (370 m) is located in a valley between the two highest points of the municipal territory, the &quot;Puig de Les Pedrisses&quot;(1330,6 m) and the &quot;Roc de Frausa&quot; (1421 m). History.

Geographic entities mentioned:
surface_form: Roc de Frausa
instance_of: Mountain
countries: Spain
France
coordinates: lat: 42.422734
lon: 2.724178
Mount Talbot. Mount Talbot is located on the northern side of Shale Pass on the Alberta-British Columbia border. It was officially named on 4 November 1925 after Senator Peter Talbot (1854-1919), an early pioneer of the Lacombe region of central Alberta. A teacher and farmer, he turned to politics and became an elected representative of the Northwest Territories and later the province of Alberta.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount talbot
instance_of: Mountain
countries: Canada
coordinates: lat: 53.6164
lon: -119.717
Mount Talbot. Mount Talbot is located on the northern side of Shale Pass on the Alberta-British Columbia border. It was officially named on 4 November 1925 after Senator Peter Talbot (1854-1919), an early pioneer of the Lacombe region of central Alberta. A teacher and farmer, he turned to politics and became an elected representative of the Northwest Territories and later the province of Alberta.

Geographic entities mentioned:
surface_form: mount talbot
instance_of: Mountain
countries: Canada
coordinates: lat: 53.6164
lon: -119.717
Nobleton, Ontario. Nobleton (2021 population 6,507) is an unincorporated community in southwestern King, Ontario, Canada. It is the third-largest community in the township, after King City and Schomberg. Located south of the Oak Ridges Moraine, Nobleton is surrounded by hills and forests. Many horse farms are found on Nobleton's eastern periphery.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
To the northwest is Hammertown. Geography. Nobleton is at an elevation of approximately 300 m, just south of the regional peak of the Oak Ridges Moraine. The Humber River flows in the southwestern part with a conservation area covering the southwest. The Oak Ridges Moraine is to the north and is covered with pine forests with a few other types of trees and lakes to the north and the northeast.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
The Humber River flows in the southwestern part with a conservation area covering the southwest. The Oak Ridges Moraine is to the north and is covered with pine forests with a few other types of trees and lakes to the north and the northeast. Nobleton Lakes is located nearly 2 to 3 km north and includes two lakes and a golf and Country Club.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Mount Collinson. Mount Collinson () is a mountain located in the far east of Hong Kong Island, Hong Kong. The mountain has a sea level elevation of. It is situated within the Shek O Country Park, which has an area of 7.01 square kilometres (2.71 square miles). It is located in the southeastern corner of Hong Kong Island.

Geographic entities mentioned:
surface_form: mount collinson
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.25109
lon: 114.23607
Mount Collinson () is a mountain located in the far east of Hong Kong Island, Hong Kong. The mountain has a sea level elevation of. It is situated within the Shek O Country Park, which has an area of 7.01 square kilometres (2.71 square miles). It is located in the southeastern corner of Hong Kong Island. There are 7 named peaks in the park, and Mount Collinson is the highest among them. Location.

Geographic entities mentioned:
surface_form: mount collinson
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.25109
lon: 114.23607
Little Moose Mountain. Little Moose Mountain is a summit located in Central New York Region of New York located in the Town of Webb in Herkimer County, southeast of Old Forge.

Geographic entities mentioned:
surface_form: moose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.65
lon: -90.7333
surface_form: moose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.603333333333
lon: -74.220555555556
surface_form: moose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.088055555556
lon: -73.663888888889
surface_form: moose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9375
lon: -110.856
surface_form: little moose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6925
lon: -74.951944444444
surface_form: moose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 64.9406
lon: -147.991
surface_form: moose mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.669722222222
lon: -74.315833333333
It is located in the Ancash Region, Bolognesi Province, Pacllon District, and in the Lima Region, Cajatambo Province, Copa District. Huacrish lies on the sub-range west of Yerupaja, northeast of the mountain Auxilio and southeast of the Auxilio Lake.

Geographic entities mentioned:
surface_form: Auxilio
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
surface_form: yerupaja
instance_of: Mountain
countries: Peru
coordinates: lat: -10.268889
lon: -76.905278
surface_form: auxilio
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
surface_form: auxilio
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3056
lon: -76.9653
Huacrish. Huacrish (possibly from Quechua &quot;Wakrish&quot; (from &quot;wakri&quot;) for &quot;flash of lightning&quot;) is a mountain in the west of the Huayhuash mountain range in the Andes of Peru, about high. It is located in the Ancash Region, Bolognesi Province, Pacllon District, and in the Lima Region, Cajatambo Province, Copa District.

Geographic entities mentioned:
surface_form: copa
instance_of: Mountain
countries: Peru
coordinates: lat: -9.2666666666667
lon: -77.516666666667
Huacrish. Huacrish (possibly from Quechua &quot;Wakrish&quot; (from &quot;wakri&quot;) for &quot;flash of lightning&quot;) is a mountain in the west of the Huayhuash mountain range in the Andes of Peru, about high. It is located in the Ancash Region, Bolognesi Province, Pacllon District, and in the Lima Region, Cajatambo Province, Copa District.

Geographic entities mentioned:
surface_form: huacrish
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2986
lon: -76.9639
Huacrish. Huacrish (possibly from Quechua &quot;Wakrish&quot; (from &quot;wakri&quot;) for &quot;flash of lightning&quot;) is a mountain in the west of the Huayhuash mountain range in the Andes of Peru, about high. It is located in the Ancash Region, Bolognesi Province, Pacllon District, and in the Lima Region, Cajatambo Province, Copa District.

Geographic entities mentioned:
surface_form: huacrish
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2986
lon: -76.9639
surface_form: wakrish
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2986
lon: -76.9639
According to &quot;The New York Times&quot;, &quot;The town of Madisonville, La., on the other side of Lake Pontchartrain, has been captured without resistance and is now garrisoned by our forces.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
The first deliberate battle in 1609 was fought at Champlain's initiative. Champlain deliberately went along with a war party down Lake Champlain. Furthermore, this battle created 150 years of mistrust that poisoned any chances that French-Iroquois alliances would be durable and long lived. De Champlain wrote, &quot;I had come with no other intention than to make war&quot;.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
De Champlain wrote, &quot;I had come with no other intention than to make war&quot;. In the company of his Huron and Algonkin allies, Champlain and his forces fought a pitched battle with the Mohawk on the shores of Lake Champlain. Champlain singlehandedly killed three Iroquois chiefs with an arquebus despite the war chiefs having worn &quot;arrowproof body armor made of plaited sticks&quot;.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Mount Phoukas. Mount Phoukas or Foukas () is a mountain in the Peloponnesus in Greece. Anciently, it was called Apesas (;); it towered above Nemea in the territory of Cleonae, Argolis, and was where Perseus is said to have been the first person who sacrificed to Zeus Apesantius.

Geographic entities mentioned:
surface_form: apesas
instance_of: Mountain
countries: Greece
coordinates: lat: 37.8625
lon: 22.7392
Mount Phoukas. Mount Phoukas or Foukas () is a mountain in the Peloponnesus in Greece. Anciently, it was called Apesas (;); it towered above Nemea in the territory of Cleonae, Argolis, and was where Perseus is said to have been the first person who sacrificed to Zeus Apesantius.

Geographic entities mentioned:
surface_form: mount phoukas
instance_of: Mountain
countries: Greece
coordinates: lat: 37.8625
lon: 22.7392
surface_form: phoukas
instance_of: Mountain
countries: Greece
coordinates: lat: 37.8625
lon: 22.7392
Mount Phoukas. Mount Phoukas or Foukas () is a mountain in the Peloponnesus in Greece. Anciently, it was called Apesas (;); it towered above Nemea in the territory of Cleonae, Argolis, and was where Perseus is said to have been the first person who sacrificed to Zeus Apesantius.

Geographic entities mentioned:
surface_form: mount phoukas
instance_of: Mountain
countries: Greece
coordinates: lat: 37.8625
lon: 22.7392
surface_form: foukas
instance_of: Mountain
countries: Greece
coordinates: lat: 37.8625
lon: 22.7392
surface_form: phoukas
instance_of: Mountain
countries: Greece
coordinates: lat: 37.8625
lon: 22.7392
Another group that are &quot;distinguished from the mass of &quot; are the, or apostate ex-Muslims, who are considered renegades and traitors. Their traditional punishment is death, even, according to some scholars, if they recant their abandonment of Islam.
 / .
are non-Muslims living under the protection of an Islamic state. are exempt from certain duties assigned specifically to Muslims if they

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Powell Valley is a picturesque location, with an overlook accessible from the Northbound lanes of U.S. Route 23. A number of homes, farms, and a church are located in the valley below the overlook. The valley begins between Powell Mountain and Little Stone Mountain where the waters of the Powell River flow down from the rugged mountains of western Wise County.

Geographic entities mentioned:
surface_form: Powell Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.511197
lon: -83.396292
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.548611111111
lon: -77.842777777778
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.3936
lon: -81.0433
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
surface_form: powell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.3277022
lon: -118.699859
The valley follows the Powell River west towards the Tennessee border. Majestic Powell Valley is part of the High Knob Landform, lying literally amid its heart and eroded core, and is a true geologic wonder. The Virginia longhunter, explorer and later Revolutionary War general Joseph Martin was instrumental in opening up Powell Valley to settlement from the east.

Geographic entities mentioned:
surface_form: High Knob Landform
instance_of: Mountain
countries: United States
coordinates: lat: 36.8926
lon: -82.6296
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.8833
lon: -78.1167
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 42.428333333333
lon: -74.312777777778
surface_form: powell valley
instance_of: Valley
countries: United States
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 39.19916667
lon: -78.89916667
The valley begins between Powell Mountain and Little Stone Mountain where the waters of the Powell River flow down from the rugged mountains of western Wise County. The immense exposed rock face where Stone Mountain and Powell Mountain come together near Grindstone Ridge to the southeast from the overlook, yields a striking visual change in altitude.

Geographic entities mentioned:
surface_form: powell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.511197
lon: -83.396292
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.548611111111
lon: -77.842777777778
surface_form: stone mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.3936
lon: -81.0433
surface_form: powell mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.3277022
lon: -118.699859
Within only 0.8 mile the vertical elevation changes by) across the northern face of the Grindstone Ridge Dome of the High Knob Massif, to mark one of the greatest short-distance vertical elevation changes in the southern Appalachians (the greatest found west of the Blue Ridge in Virginia). The valley follows the Powell River west towards the Tennessee border.

Geographic entities mentioned:
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 38.8833
lon: -78.1167
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 42.428333333333
lon: -74.312777777778
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 36.8926
lon: -82.6296
surface_form: high knob
instance_of: Mountain
countries: United States
coordinates: lat: 39.19916667
lon: -78.89916667