Sarmila/GeoWiki-Features huggingface dataset:
In intercolumns there are statues of Saint Roch and John the Evangelist. They are decorated with statues of angels. The lance there is a circular painting of Saint Imrich. • Altar of the Transfiguration on the Mount Tabor. It is located in the southern nave. The altar is Baroque from the 18th century but is decorated with Renaissance ornaments from the older altars from the 17th century.

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Middelie developed in the 12th century as a peat excavation settlement. It used to be a fishing village, but after the Purmer was &quot;polder&quot;ed, it lost its connection to the sea and the village stagnated. During the Reformation, Mennonites settled in the village, and used to make up half the population until the 20th century.

Geographic entities mentioned:
surface_form: Purmer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.488888888889
lon: 5.0069444444444
Grinde (landform). A &quot;grinde&quot; (plural: &quot;grinden&quot;) is an almost treeless area of wet heathland found on the rounded bunter sandstone ridges of the Northern Black Forest in Germany. The &quot;grinden&quot; reached their greatest extent in the early 19th century when they ran from the Kniebis mountain near Freudenstadt in the south to the heights near Dobel in the north.

Geographic entities mentioned:
surface_form: Kniebis
instance_of: Mountain
countries: Germany
coordinates: lat: 48.476388888889
lon: 8.2938888888889
The &quot;grinden&quot; reached their greatest extent in the early 19th century when they ran from the Kniebis mountain near Freudenstadt in the south to the heights near Dobel in the north. Today they are restricted to the highest parts of the Northern Black Forest around the summits of the Hornisgrinde, Schliffkopf and Kniebis (900 to). They still cover an area of about 180 ha.

Geographic entities mentioned:
surface_form: Hornisgrinde
instance_of: Mountain
countries: Germany
coordinates: lat: 48.606944444444
lon: 8.2025
surface_form: Schliffkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 48.535277777778
lon: 8.2152777777778
surface_form: Kniebis
instance_of: Mountain
countries: Germany
coordinates: lat: 48.476388888889
lon: 8.2938888888889
Lake St. Martin. Lake St. Martin is a lake in the Interlake region of Manitoba, Canada. The lake is situated between Lake Manitoba and Lake Winnipeg. Lake St. Martin is downstream from the Fairford River with its Fairford River Control Structure. The Fairford River is the only outlet for Lake Manitoba. With the artificially increased flow and limited outflow, Lake St.

Geographic entities mentioned:
surface_form: Lake Manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Martin was turned into a reservoir. The outflow for Lake St. Martin exits through Dauphin River and into Lake Winnipeg, at a lower rate than the water comes in. Settlements on the lake, including the Lake St. Martin First Nation, were flooded and made uninhabitable after the 2011 Assiniboine River flood. Fairford River Control Structure.

Geographic entities mentioned:
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Lake St. Martin is negatively impacted by the Fairford Water Control Structure as the water levels are either artificially high or low depending on the rainy or drought conditions (Ahmed, et al., 2019). Portage Diversion. In 1970 the Portage Diversion was constructed on the Assiniboine River that brought more water to Lake St. Martin via Lake Manitoba.

Geographic entities mentioned:
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Portage Diversion. In 1970 the Portage Diversion was constructed on the Assiniboine River that brought more water to Lake St. Martin via Lake Manitoba. This Portage Diversion brought water from the Assiniboine River to an entirely different watershed through digging a 29 km long channel to Lake Manitoba. This Portage Diversion was designed to protect Winnipeg and Portage la Prairie from flooding.

Geographic entities mentioned:
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
This Portage Diversion was designed to protect Winnipeg and Portage la Prairie from flooding. By diverting water from population centers to Lake St. Martin, the population at risk was changed (Manitoba Infrastructure, nd). This increased water sent from Assiniboine River created even larger water flowing to Lake St. Martin, which caused more land loss. In Lake St.

Geographic entities mentioned:
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Martin (AAE Tech Services Inc. et al., 2016). 2011 flood. In 2011, Manitoba was hit with a &quot;superflood&quot; called the Assiniboine flood. To protect Winnipeg, Portage la Prairie, and agricultural land, the provincial government opened the Portage Diversion. The flood waters were diverted into Lake Manitoba, which put many residences and cottages on Lake Manitoba at risk for flooding.

Geographic entities mentioned:
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Martin and Lake Manitoba by draining them into Lake Winnipeg. The outlet was closed in 2012 (Manitoba infrastructure, nd). 2014 flood. In 2014, another flood event occurred on the Assiniboine River in Manitoba. The Fairford River Water Control Structure was at full capacity draining water into Lake St. Martin. The artificially increased flow caused major flooding for the surrounding communities.

Geographic entities mentioned:
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Due to the Fairford River structure the impacts on the ecosystem greatly reduced the fish population and the land could no longer be used for cattle raising (Westdal, 2013). Evacuation and compensation. The peoples who lived on the Lake St. Martin reserve, as well as people from other reserves, were forced to evacuate for the 2011 Assiniboine river flood.

Geographic entities mentioned:
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
The Fairford River is the only outlet for Lake Manitoba. With the artificially increased flow and limited outflow, Lake St. Martin was turned into a reservoir. The outflow for Lake St. Martin exits through Dauphin River and into Lake Winnipeg, at a lower rate than the water comes in. Settlements on the lake, including the Lake St.

Geographic entities mentioned:
surface_form: lake winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Without an environmental assessment, the major project of the Lake St. Martin Emergency Outlet Channel was constructed and began to operate on November 1, 2011 (Manitoba Minister of Conservation, 2011). The outlet channel lowered lake levels in Lake St. Martin and Lake Manitoba by draining them into Lake Winnipeg. The outlet was closed in 2012 (Manitoba infrastructure, nd). 2014 flood.

Geographic entities mentioned:
surface_form: lake winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
The Fairford River Water Control Structure was at full capacity draining water into Lake St. Martin. The artificially increased flow caused major flooding for the surrounding communities. The Lake St. Martin emergency channel was only partially opened as the residents around Lake Winnipeg had concerns for their cottages flooding. The channel closed in 2015 (Manitoba Infrastructure, nd).

Geographic entities mentioned:
surface_form: lake winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
821). The area around Lake St. Martin is almost entirely populated by Indigenous people. Those impacted by the flood include Indigenous people living at Pinaymootang, Little Saskatchewan, Lake St. Martin and then on the Lake Winnipeg side — Daphne River First Nation communities (Indigenous services Canada, 2022). The communities had a thriving fishery and agriculture before the flooding.

Geographic entities mentioned:
surface_form: lake winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Martin via Lake Manitoba. This Portage Diversion brought water from the Assiniboine River to an entirely different watershed through digging a 29 km long channel to Lake Manitoba. This Portage Diversion was designed to protect Winnipeg and Portage la Prairie from flooding. By diverting water from population centers to Lake St.

Geographic entities mentioned:
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Martin (AAE Tech Services Inc. et al., 2016). 2011 flood. In 2011, Manitoba was hit with a &quot;superflood&quot; called the Assiniboine flood. To protect Winnipeg, Portage la Prairie, and agricultural land, the provincial government opened the Portage Diversion. The flood waters were diverted into Lake Manitoba, which put many residences and cottages on Lake Manitoba at risk for flooding.

Geographic entities mentioned:
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
The water diversions at Portage and Fairford forced relocations of two communities after eight years of displacement from 2011 to 2019. The Manitoban government decided to divert the water flow to Lake St. Martin First Nation to lessen the impact of flooding on Winnipeg and other non-Indigenous homes and farm lands (Thompson, 2015). The flood damaged all housing and infrastructure at Lake St.

Geographic entities mentioned:
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Financial benefits. The government of Manitoba made a calculated decision in flooding Lake St. Martin (Ballard, 2012). The water was flowing towards Winnipeg until the province diverted the flood water. The government chose to divert water to Lake St. Martin to flood a lake surrounded by Indigenous reserves. Ballard (2012) explains how the government of Manitoba's decision to flood Lake St.

Geographic entities mentioned:
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Lake St. Martin. Lake St. Martin is a lake in the Interlake region of Manitoba, Canada. The lake is situated between Lake Manitoba and Lake Winnipeg. Lake St. Martin is downstream from the Fairford River with its Fairford River Control Structure. The Fairford River is the only outlet for Lake Manitoba. With the artificially increased flow and limited outflow, Lake St.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
The lake is situated between Lake Manitoba and Lake Winnipeg. Lake St. Martin is downstream from the Fairford River with its Fairford River Control Structure. The Fairford River is the only outlet for Lake Manitoba. With the artificially increased flow and limited outflow, Lake St. Martin was turned into a reservoir. The outflow for Lake St.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Fairford River Control Structure. Natural flows of water are modified and fluctuated to serve development interests. In 1961, the construction of the Fairford Water Control Structure was finished. The Fairford River connects Lake Manitoba to Lake St. Martin with the water control structure allowing the Province to regulate water levels in Lake Manitoba and flood Lake St. Martin.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
This Portage Diversion brought water from the Assiniboine River to an entirely different watershed through digging a 29 km long channel to Lake Manitoba. This Portage Diversion was designed to protect Winnipeg and Portage la Prairie from flooding. By diverting water from population centers to Lake St. Martin, the population at risk was changed (Manitoba Infrastructure, nd).

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
To protect Winnipeg, Portage la Prairie, and agricultural land, the provincial government opened the Portage Diversion. The flood waters were diverted into Lake Manitoba, which put many residences and cottages on Lake Manitoba at risk for flooding. To protect cottagers, residences, farmland areas that were Provincial lands with high property values to Lake St.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
The 2011 flood resulted in &quot;the lake area increased by 13%&quot; (2019). To lower the high water levels an emergency channel was pushed through under the Emergency Measures Act. Without an environmental assessment, the major project of the Lake St. Martin Emergency Outlet Channel was constructed and began to operate on November 1, 2011 (Manitoba Minister of Conservation, 2011).

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Martin Emergency Outlet Channel was constructed and began to operate on November 1, 2011 (Manitoba Minister of Conservation, 2011). The outlet channel lowered lake levels in Lake St. Martin and Lake Manitoba by draining them into Lake Winnipeg. The outlet was closed in 2012 (Manitoba infrastructure, nd). 2014 flood. In 2014, another flood event occurred on the Assiniboine River in Manitoba.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
The Lake St. Martin emergency channel was only partially opened as the residents around Lake Winnipeg had concerns for their cottages flooding. The channel closed in 2015 (Manitoba Infrastructure, nd). Impacts of flooding. Indigenous people are most at risk from flooding in Canada and the world (Thistlethwaite et al., 2020). Chakraborty et al.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
Martin (Ballard, 2012). The water was flowing towards Winnipeg until the province diverted the flood water. The government chose to divert water to Lake St. Martin to flood a lake surrounded by Indigenous reserves. Ballard (2012) explains how the government of Manitoba's decision to flood Lake St. Martin is due to First Nations' reserve land being federal Crown land. In flooding Lake St.

Geographic entities mentioned:
surface_form: manitoba
instance_of: Lake
countries: Canada
coordinates: lat: 50.996
lon: -98.762
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Lake St. Martin. Lake St. Martin is a lake in the Interlake region of Manitoba, Canada. The lake is situated between Lake Manitoba and Lake Winnipeg. Lake St. Martin is downstream from the Fairford River with its Fairford River Control Structure. The Fairford River is the only outlet for Lake Manitoba. With the artificially increased flow and limited outflow, Lake St.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Martin. Lake St. Martin is a lake in the Interlake region of Manitoba, Canada. The lake is situated between Lake Manitoba and Lake Winnipeg. Lake St. Martin is downstream from the Fairford River with its Fairford River Control Structure. The Fairford River is the only outlet for Lake Manitoba. With the artificially increased flow and limited outflow, Lake St. Martin was turned into a reservoir.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Lake St. Martin is downstream from the Fairford River with its Fairford River Control Structure. The Fairford River is the only outlet for Lake Manitoba. With the artificially increased flow and limited outflow, Lake St. Martin was turned into a reservoir. The outflow for Lake St. Martin exits through Dauphin River and into Lake Winnipeg, at a lower rate than the water comes in.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
The Fairford River connects Lake Manitoba to Lake St. Martin with the water control structure allowing the Province to regulate water levels in Lake Manitoba and flood Lake St. Martin. This resulted in a loss of Indian reserve land in Lake St. Martin. The water dam on Fairford River changed the shape of the Lake and changed the Lake into a reservoir. Lake St.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Martin. This resulted in a loss of Indian reserve land in Lake St. Martin. The water dam on Fairford River changed the shape of the Lake and changed the Lake into a reservoir. Lake St. Martin is negatively impacted by the Fairford Water Control Structure as the water levels are either artificially high or low depending on the rainy or drought conditions (Ahmed, et al., 2019). Portage Diversion.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Martin, the population at risk was changed (Manitoba Infrastructure, nd). This increased water sent from Assiniboine River created even larger water flowing to Lake St. Martin, which caused more land loss. In Lake St. Martin, agricultural land was transformed into marshland (Schertow et al., 2012). Further, the ecosystem was changed and natural cycles for water disrupted.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Martin, which caused more land loss. In Lake St. Martin, agricultural land was transformed into marshland (Schertow et al., 2012). Further, the ecosystem was changed and natural cycles for water disrupted. These disruptions decrease fish population and influence the surrounding settlements of Lake St. Martin (AAE Tech Services Inc. et al., 2016). 2011 flood.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
The flood waters were diverted into Lake Manitoba, which put many residences and cottages on Lake Manitoba at risk for flooding. To protect cottagers, residences, farmland areas that were Provincial lands with high property values to Lake St. Martin Indigenous reserves that were federal Crown land, without value.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
To protect cottagers, residences, farmland areas that were Provincial lands with high property values to Lake St. Martin Indigenous reserves that were federal Crown land, without value. The Fairford Water Control Structure was opened to flood thousands of Indigenous people from several reserves. Worst hit was the Lake St. Martin community. Everyone from the Lake St.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
The Fairford Water Control Structure was opened to flood thousands of Indigenous people from several reserves. Worst hit was the Lake St. Martin community. Everyone from the Lake St. Martin community was evacuated in an emergency situation and all the homes and buildings were flooded. The outflow from Lake St. Martin was greatly reduced due to ice blockages in the Dauphin River.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Worst hit was the Lake St. Martin community. Everyone from the Lake St. Martin community was evacuated in an emergency situation and all the homes and buildings were flooded. The outflow from Lake St. Martin was greatly reduced due to ice blockages in the Dauphin River. According to Ahmed et al. The 2011 flood resulted in &quot;the lake area increased by 13%&quot; (2019).

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
The outlet was closed in 2012 (Manitoba infrastructure, nd). 2014 flood. In 2014, another flood event occurred on the Assiniboine River in Manitoba. The Fairford River Water Control Structure was at full capacity draining water into Lake St. Martin. The artificially increased flow caused major flooding for the surrounding communities. The Lake St.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Indigenous people are most at risk from flooding in Canada and the world (Thistlethwaite et al., 2020). Chakraborty et al. states that &quot;Canadian Indigenous communities bear significant financial, psychological, and social burdens associated with flooding, and they have been disproportionately affected by flood-related displacement&quot; (2021, p. 821). The area around Lake St.

Geographic entities mentioned:
surface_form: bear
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.2833
lon: -126.967
The Manitoban government decided to divert the water flow to Lake St. Martin First Nation to lessen the impact of flooding on Winnipeg and other non-Indigenous homes and farm lands (Thompson, 2015). The flood damaged all housing and infrastructure at Lake St. Martin and most of Little Saskatchewan caused the need for intensive rebuilding.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
In 2020, families were still displaced. Though families are returning home, they are deeply traumatized by the displacement and environmental injustice (Hoye, 2019). Financial benefits. The government of Manitoba made a calculated decision in flooding Lake St. Martin (Ballard, 2012). The water was flowing towards Winnipeg until the province diverted the flood water.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
Financial benefits. The government of Manitoba made a calculated decision in flooding Lake St. Martin (Ballard, 2012). The water was flowing towards Winnipeg until the province diverted the flood water. The government chose to divert water to Lake St. Martin to flood a lake surrounded by Indigenous reserves. Ballard (2012) explains how the government of Manitoba's decision to flood Lake St.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
In flooding Lake St. Martin the responsibility for financial compensation shifts from the province to the federal government for lands under their jurisdiction. The province saved money from massive flood damage impacting cities under their jurisdiction, despite the environmental damage in reserves on nearby Lake St. Martin. Government and the history of Indigenous flooding.

Geographic entities mentioned:
surface_form: lake st. martin
instance_of: Lake
countries: Canada
coordinates: lat: 51.6169
lon: -98.4828
It covers of lake and countryside. The valley contains the Elan Valley Reservoirs and Elan Village, designed by architect Herbert Tudor Buckland as part of the same scheme. Elan Village is the only purpose-built Arts and Crafts &quot;Model Village&quot; in Wales. It is also famous for its picturesque scenery.

Geographic entities mentioned:
surface_form: Elan Valley Reservoirs
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 52.27222222222222
lon: -3.688888888888889
surface_form: elan valley reservoirs
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 52.27222222222222
lon: -3.688888888888889
surface_form: elan valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.262222222222
lon: -3.5886111111111
Elan Valley. The Elan Valley () is a river valley situated to the west of Rhayader, in Powys, Wales, sometimes known as the &quot;Welsh Lake District&quot;. It covers of lake and countryside. The valley contains the Elan Valley Reservoirs and Elan Village, designed by architect Herbert Tudor Buckland as part of the same scheme.

Geographic entities mentioned:
surface_form: elan valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.262222222222
lon: -3.5886111111111
It is also famous for its picturesque scenery. Over 80% of the valley is designated as Sites of Special Scientific Interest, and a popular cycle trail, the Elan Valley Trail'&quot;, makes a loop from Rhayader around the reservoirs. Part of the trail overlaps with a spur of National Cycle Route 81 (&quot;Lon Cambria&quot;). As of 2015 it is an International Dark Sky Park.

Geographic entities mentioned:
surface_form: elan valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.262222222222
lon: -3.5886111111111
These include &quot;Local Hero&quot; (1983), &quot;Harry Potter and the Prisoner of Azkaban&quot; (2004) and &quot;Harry Potter and the Deathly Hallows – Part 1&quot; (2010). The famous island used for &quot;Harry Potter&quot; in Loch Eilt is called Eilean na Moine. It was used as Dumbledore's grave, which was later digitally placed on Loch Arkaig.

Geographic entities mentioned:
surface_form: Loch Arkaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.971989
lon: -5.158376
surface_form: loch arkaig
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.971989
lon: -5.158376
Loch Eilt. Loch Eilt is a freshwater loch in Lochaber, in the West Highlands of Scotland. It is between the villages of Glenfinnan and Lochailort, 30 km west of Fort William. The A830 road runs along the north shore, while the West Highland Line railway follows the south shore. Loch Eilt separates the traditional districts of Morar to the north and Moidart to the south.

Geographic entities mentioned:
surface_form: loch eilt
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.879
lon: -5.586
The A830 road runs along the north shore, while the West Highland Line railway follows the south shore. Loch Eilt separates the traditional districts of Morar to the north and Moidart to the south. The loch has a number of small islands, including Eilean Mòr, Eilean an Tighe, Eilean Gaineamhach, Eilean nan Corra-ghriodhach and Eilean na Mòine.

Geographic entities mentioned:
surface_form: loch eilt
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.879
lon: -5.586
The loch has a number of small islands, including Eilean Mòr, Eilean an Tighe, Eilean Gaineamhach, Eilean nan Corra-ghriodhach and Eilean na Mòine. Loch Eilt has been used as a location in several films. These include &quot;Local Hero&quot; (1983), &quot;Harry Potter and the Prisoner of Azkaban&quot; (2004) and &quot;Harry Potter and the Deathly Hallows – Part 1&quot; (2010).

Geographic entities mentioned:
surface_form: loch eilt
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.879
lon: -5.586
These include &quot;Local Hero&quot; (1983), &quot;Harry Potter and the Prisoner of Azkaban&quot; (2004) and &quot;Harry Potter and the Deathly Hallows – Part 1&quot; (2010). The famous island used for &quot;Harry Potter&quot; in Loch Eilt is called Eilean na Moine. It was used as Dumbledore's grave, which was later digitally placed on Loch Arkaig.

Geographic entities mentioned:
surface_form: loch eilt
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.879
lon: -5.586
It and Tsinstikeptum Indian Reserve No. 10 are jointly normally referred to as the Westbank Indian Reserve. Tsinstikeptum Indian Reserve No. 9 is located six miles southwest of Kelowna proper, adjacent to McDougall Creek. The reserve is 641.80 ha in area. The southernmost portion of the reserve lies on the shores of Okanagan Lake. Demographics.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Crane, Oregon. Crane is an unincorporated town and census designated place in Harney County, Oregon, United States, northeast of Malheur Lake on Oregon Route 78. Its population was 116 at the 2020 census. History. Crane was named for the prominent local features Crane Creek and Crane Creek Gap.

Geographic entities mentioned:
surface_form: Malheur Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.332777777778
lon: -118.79305555556
Route 95 at Burns Junction. According to the U.S. Census Bureau, the Crane CDP has an area of, all of it land. It is northeast of Malheur Lake and by road northeast of the main entrance to Malheur National Wildlife Refuge. By 2001, the town had some residences, the school facility, a post office, and a combined gas station and store. Demographics.

Geographic entities mentioned:
surface_form: Malheur Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.332777777778
lon: -118.79305555556
Mananantanana. The Mananantanana is a river in Haute Matsiatra region, is located in eastern Madagascar. It flows into the Mangoky River. It has its springs in the Andringitra Massif. Together with the Matsiatra it forms the Mangoky River.

Geographic entities mentioned:
surface_form: Mangoky River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -21.316666666667
lon: 43.533333333333
Pizzo Cavregasco. Pizzo Cavregasco is a mountain of Lombardy, Italy. It has an elevation of 2,535 metres.

Geographic entities mentioned:
surface_form: pizzo cavregasco
instance_of: Mountain
countries: Italy
coordinates: lat: 46.24027778
lon: 9.27555556
Kristiansand is connected by four main roads: European Route E18 from Oslo, Aust-Agder, covering the easternmost parts of Kristiansand; European route E39 from Stavanger, Flekkefjord and the coastal towns and villages in Vest-Agder; Norwegian National Road 9 from Evje, Setesdal and Grim; and Norwegian National Road 41 from Telemark, northern Aust-Agder, Birkeland, Tveit and the airport Kristiansand Airport, Kjevik.

Geographic entities mentioned:
surface_form: Setesdal
instance_of: Valley
countries: Norway
coordinates: lat: 58.92025
lon: 7.7206388888889
Tachie, British Columbia. Tachie is a Carrier village in British Columbia, located where the Tachie River enters Stuart Lake. It is one of the reserves belonging to Tl'azt'en Nation. &quot;Tachie&quot; is the English spelling of the Carrier language name &quot;Tache&quot;.

Geographic entities mentioned:
surface_form: Stuart Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.55
lon: -124.58333333333
In 1937, Shteyn published a volume of about sixty woodcuts by Geller called &quot;From Land to Land&quot;, produced as part of the Federal Art Project (FAP), the visual arts arm of the Great Depression-era New Deal Works Progress Administration (WPA) Federal One program in the United States. The cover featured a goat on the shore of Lake Michigan with Chicago's skyline in the background.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Erica urna-viridis. &quot;Erica urna-viridis&quot;, the sticky heath or bottle-green heath, is a species of &quot;Erica&quot; that was naturally restricted to the city of Cape Town, South Africa, in particular the Peninsula Sandstone Fynbos of Table Mountain. It bears sticky green flowers - the origin of its common names - and grows to a height of about 1 meter.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The origin of the species name (&quot;sangay&quot;) derives from Sangay National Park, which is the largest Andean national park in Ecuador. The park itself is named after a volcano called Sangay, one of Ecuador's most active volcanoes that lies within the park. Sangay National Park was the site of the discovery of the eastern caenolestid in 2010. Taxonomy.

Geographic entities mentioned:
surface_form: Sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
25, issued by Walther von Brauchitsch that same day. This final plan committed one Hungarian corps of three brigades west of the Danube from Lake Balaton to Barcs, and twelve brigades (nine on the front and three in reserve) for an offensive in Bačka (&quot;Bácska&quot;). The Danube Flotilla was to cover the flanks, and the air force was to stand by for orders.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Deployment. The Yugoslav Army was organized into three army groups and the coastal defense troops. The 3rd Army Group was the strongest with the 3rd, 3rd Territorial, 5th and 6th Armies defending the borders with Romania, Bulgaria and Albania. The 2nd Army Group with the 1st and 2nd Armies, defended the region between the Iron Gates and the Drava River.

Geographic entities mentioned:
surface_form: Iron Gates
instance_of: Valley
countries: Serbia
Romania
coordinates: lat: 44.671111111111
lon: 22.529722222222
Its English translation is attributed to Filipino Indologist Juan R. Francisco, assisted by Maranao scholar Nagasura Madale, based on Francisco's ethnographic research in the Lake Lanao area in the late 1960s. It narrates the adventures of the monkey-king, Maharadia Lawana, to whom the Gods have granted immortality.

Geographic entities mentioned:
surface_form: Lake Lanao
instance_of: Lake
countries: Philippines
coordinates: lat: 7.88
lon: 124.2525
An area of high topographical relief continues to the east of the mountain towards Mica Peak and the Coeur d'Alene Mountains of the Bitterroot Range, in turn part of the Rocky Mountains. To the north the mountain descends slowly along a ridge, and then into the lower Dishman Hills and eventually into Spokane Valley.

Geographic entities mentioned:
surface_form: Spokane Valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
To the north the mountain descends slowly along a ridge, and then into the lower Dishman Hills and eventually into Spokane Valley. To the south and west the mountain towers over relatively flat terrain, with the vast farmland of the Palouse and the Columbia Plateau extending as far as the eye can see.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
Krell Hill. Krell Hill, also known as Tower Mountain, is a peak at the southern end of the Selkirk Mountains in Spokane County, Washington. It rises abruptly to the southeast of the relatively flat South Hill area of the city of Spokane.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.8572
lon: -107.623
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.265
lon: -74.104166666667
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.4984
lon: -73.3317
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.10944444444445
lon: -75.22611111111111
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.588333333333
lon: -120.70333333333
surface_form: krell hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.3446
lon: -117.175
To the south and west the mountain towers over relatively flat terrain, with the vast farmland of the Palouse and the Columbia Plateau extending as far as the eye can see. Tower Mountain, while not the official name, is commonly used because of the tall television and radio towers along the ridge atop the mountain.

Geographic entities mentioned:
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.8572
lon: -107.623
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.265
lon: -74.104166666667
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.4984
lon: -73.3317
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.10944444444445
lon: -75.22611111111111
surface_form: tower mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.588333333333
lon: -120.70333333333
Krell Hill. Krell Hill, also known as Tower Mountain, is a peak at the southern end of the Selkirk Mountains in Spokane County, Washington. It rises abruptly to the southeast of the relatively flat South Hill area of the city of Spokane.

Geographic entities mentioned:
surface_form: south hill
instance_of: Mountain
countries: United States
coordinates: lat: 43.281388888889
lon: -75.295
These granite monoliths are a popular location with rock climbers. The Conservation Futures program, after a few years of negotiations, completed a trailhead on Stevens Creek Road in August 2012 allowing climbers and hikers a shorter route to the rocks from the south. Before the Stevens Creek access was approved visitors had to start from the north at Holman and Rockcrest.

Geographic entities mentioned:
surface_form: stevens creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.4458
lon: -122.064
The Conservation Futures program, after a few years of negotiations, completed a trailhead on Stevens Creek Road in August 2012 allowing climbers and hikers a shorter route to the rocks from the south. Before the Stevens Creek access was approved visitors had to start from the north at Holman and Rockcrest. From there visitors would hike up the valley of Iller Creek for over 2 miles.

Geographic entities mentioned:
surface_form: stevens creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.4458
lon: -122.064
The Conservation Futures program, after a few years of negotiations, completed a trailhead on Stevens Creek Road in August 2012 allowing climbers and hikers a shorter route to the rocks from the south. Before the Stevens Creek access was approved visitors had to start from the north at Holman and Rockcrest. From there visitors would hike up the valley of Iller Creek for over 2 miles.

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
To the north and adjacent to Krell Hill is a slightly smaller mountain peak connected by a ridge; this peak is also sometimes referred to by the same name, due to both peaks containing tall towers. The mountain rises roughly 1,700 feet above the floor of the Spokane Valley and 1,200 feet above the adjacent portions of the city of Spokane. Browne's Mountain.

Geographic entities mentioned:
surface_form: spokane valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Krell Hill. Krell Hill, also known as Tower Mountain, is a peak at the southern end of the Selkirk Mountains in Spokane County, Washington. It rises abruptly to the southeast of the relatively flat South Hill area of the city of Spokane.

Geographic entities mentioned:
surface_form: krell hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.3446
lon: -117.175
They are prominent at all times of day, but especially at night with their flashing red lights. The towers can be seen from many locations around the Spokane area and northern Palouse. To the north and adjacent to Krell Hill is a slightly smaller mountain peak connected by a ridge; this peak is also sometimes referred to by the same name, due to both peaks containing tall towers.

Geographic entities mentioned:
surface_form: krell hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.3446
lon: -117.175
It is named for pioneer lawyer J.J. Browne, who built one of the first homes in the area in 1908. It sits on the northwesternmost foothill of the Krell Hill, where it abruptly begins its rise from the Glenrose and Moran Prairies. The neighborhood is entirely residential and suburban in nature. Its location on the hillside gives the area panoramic views of Spokane and beyond.

Geographic entities mentioned:
surface_form: krell hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.3446
lon: -117.175
Some of the roads in the neighborhood are private. Iller Creek Conservation Area. The Iller Creek Conservation Area consists of 966.62 acres on the eastern side of Krell Hill and is part of Spokane County's Conservation Futures program. Iller Creek drains the eastern slopes of the mountain along with a ridge to the east.

Geographic entities mentioned:
surface_form: krell hill
instance_of: Mountain
countries: United States
coordinates: lat: 47.3446
lon: -117.175
Environmental issues in the San Joaquin Valley. The San Joaquin Valley of California has seen environmental issues arise from agricultural production, industrial processing, and the region's use as a transportation corridor, experiencing some of the nation’s worst air quality, high rates of childhood asthma, and contaminated drinking water.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Geographically, the San Joaquin Valley stretches from the Tehachapi Mountains in the south, between the California coastal ranges and the Sierra Nevada range, and opening into Sacramento–San Joaquin River Delta in the north.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
A reception Home (New Orpington Lodge, later St. George's Home) was established in Hintonburg, Ottawa, in 1895. In addition, land was obtained in Manitoba in 1895, and in 1897 the New Southwark Training Farm was opened in the village of Makinak in the Lake Dauphin district of Manitoba. The Society selected the children from industrial and Poor Law schools, and from other sources.

Geographic entities mentioned:
surface_form: Lake Dauphin district
instance_of: Lake
countries: Canada
coordinates: lat: 51.2696
lon: -99.7792
Rätikon. The Rätikon is a mountain range of the Central Eastern Alps, located at the border between Vorarlberg, Liechtenstein and Graubünden. It is the geological border between the Eastern and Western Alps and stretches from the Montafon as far as the Rhine. In the south, the Prättigau is its limit, and in the north, it is the Walgau. In the east, it borders the Silvretta groups.

Geographic entities mentioned:
surface_form: Montafon
instance_of: Valley
countries: Austria
coordinates: lat: 47.08
lon: 9.9
Rätikon. The Rätikon is a mountain range of the Central Eastern Alps, located at the border between Vorarlberg, Liechtenstein and Graubünden. It is the geological border between the Eastern and Western Alps and stretches from the Montafon as far as the Rhine. In the south, the Prättigau is its limit, and in the north, it is the Walgau. In the east, it borders the Silvretta groups.

Geographic entities mentioned:
surface_form: Prättigau
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9165
lon: 9.8537194444444
Their plan was to collect one billion won (about $1,250,000 in 1993) through kidnapping and extortion targeting the wealthy. Part of their training included hiking and camping on Jirisan, the second tallest mountain in South Korea. The more experienced members provided detailed lessons on handling dynamite and executing kidnappings. Victims.

Geographic entities mentioned:
surface_form: Jirisan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.336944444444
lon: 127.73055555556