Sarmila/GeoWiki-Features huggingface dataset:
The clashes represented an attempt by the Ottomans to break the Albanian rebels in the region. Background. After the losses in the Battles of Kaçanik and Carraleva, during the Albanian revolt of 1910, Albanian rebels such as Idriz Seferi, Abaz Bekteshi, Islam Pra, Sinan Maxhera etc. withdrew to the mountains of Karadak and organized small military formations (Chetas).

Geographic entities mentioned:
surface_form: Karadak
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
withdrew to the mountains of Karadak and organized small military formations (Chetas). These formations inflicted significant damage on the Ottoman forces in Karadak, using captured weapons and limited ammunition to conduct surprise attacks on difficult and unfamiliar terrain, the Ottomans lost over 2,000 men in Karadak alone.

Geographic entities mentioned:
surface_form: Karadak
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
surface_form: Karadak
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
Battle. On March 2, 1910, Osman Pasha assembled the Ottoman army consisting of around 15,000 men, detailing their tasks. Around 3,000 troops under Feyza Bey were to march from Preševo towards Karadak, while another group from Skopje approached Drenogllava under Sahid Bey. Osman Pasha himself led 6,000 troops from the Morava Valley.

Geographic entities mentioned:
surface_form: Karadak
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
Turkish historian Süleyman Külçe, claimed that the Ottomans lost 8 officers and 113 soldiers, and that Albanians had around 500 killed. However, the Serbian consulate in Skopje concluded that over 2,000 Ottoman soldiers had been killed in Karadak and the Kaza of Gjilan after the Battle of Kaçanik.

Geographic entities mentioned:
surface_form: Karadak
instance_of: Mountain
countries: Serbia
Kosovo
North Macedonia
coordinates: lat: 42.166666666667
lon: 21.416666666667
The university's academic facilities are located on six properties: Main Campus; Health Sciences Campus; West Research Campus; the Field Station for Coastal Studies in New Holland, North Carolina; the Millennial Research Innovation Campus in Greenville's warehouse district; and an overseas campus in Certaldo Alto, Italy. ECU also operates the Coastal Studies Institute.

Geographic entities mentioned:
surface_form: New Holland
instance_of: Lake
countries: United States
coordinates: lat: 35.4987
lon: -76.189
Campus. East Carolina is separated into three distinct campuses: Main Campus, Health Sciences Campus, and West Research Campus. It owns two sports complexes: Blount Recreational Sports Complex and North Recreational Complex. It owns a field station in New Holland, North Carolina. Main. The main campus, also known as the east campus, is about in an urban residential area of downtown Greenville.

Geographic entities mentioned:
surface_form: New Holland
instance_of: Lake
countries: United States
coordinates: lat: 35.4987
lon: -76.189
All 8 community centers are currently active. They are located in Ahoskie, Elizabeth City, Lillington, Spruce Pine, Bolivia, Thomasville, Lumberton, and Sylva. Field Station for Coastal Studies. The field station is located in New Holland, North Carolina. The area serves as a field station for the coastal studies, coastal resource management, and biology programs.

Geographic entities mentioned:
surface_form: New Holland
instance_of: Lake
countries: United States
coordinates: lat: 35.4987
lon: -76.189
It also serves as a facility for small retreats and as a base for research on coastal issues. It was listed on the National Register of Historic Places in 1980. It is adjacent to the Mattamuskeet Wildlife Refuge. North Recreational Complex. North Recreational Complex (NRC) is an athletic complex located on a parcel of land north of East Carolina University's main campus.

Geographic entities mentioned:
surface_form: Mattamuskeet Wildlife Refuge
instance_of: Lake
countries: United States
coordinates: lat: 35.4987
lon: -76.189
ECU houses and manages the UNC Coastal Studies Institute (UNC-CSI) which is an inter-university, marine research institute located on Roanoke Island in Manteo along the Croatan Sound on the Outer Banks, established in 2003 focusing on Estuarine Ecology and Human Health, Coastal Processes and Engineering, Public Policy and Coastal Sustainability, and Maritime Heritage. Administration.

Geographic entities mentioned:
surface_form: Croatan Sound
instance_of: Landform
countries: United States
coordinates: lat: 35.8375
lon: -75.69722222
Blaine, West Virginia. Blaine is an unincorporated community in Mineral County, West Virginia, United States. It is part of the Cumberland, MD-WV Metropolitan Statistical Area. It lies near the intersection of the North Branch Potomac River and West Virginia Route 42. The community has the name of James G. Blaine, a businessperson.

Geographic entities mentioned:
surface_form: North Branch Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
Cruickshank was educated at the University of Minnesota and ordained in 1963. He served in the Robson Valley area until 1965 when he became director of the Anglican Lay Training Centre at Sorrento. In 1983 he became dean of New Westminster, a post he held until his election as Bishop of Cariboo.

Geographic entities mentioned:
surface_form: Robson Valley
instance_of: Valley
countries: Canada
coordinates: lat: 53.25
lon: -120
The Koettlitz Glacier runs along the northwestern foot of Mount Morning and separates it from the Royal Society Range away. Mount Discovery lies next to Mount Morning and is separated from it by the Discovery Glacier. The volcano was originally described in the early to middle 20th century, before more detailed analyses took place in the 1970s, 1980s and 2000s.

Geographic entities mentioned:
surface_form: Mount Discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Spinel peridotite and less commonly clinopyroxenite, dunite, harzburgite, lherzolite, norite, pyroxenite and websterite have been reported as xenoliths. The early volcanic rocks of Mount Morning are comparable to mildly alkaline rocks from Mount Melbourne, while the more alkaline late volcanic rocks resemble these from Mount Erebus.

Geographic entities mentioned:
surface_form: Mount Melbourne
instance_of: Mountain
coordinates: lat: -74.333333333333
lon: 164.7
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: mount erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount melbourne
instance_of: Mountain
coordinates: lat: -74.333333333333
lon: 164.7
Morning Glacier. A glacier on the northeast slope of Mount Morning. The glacier flows from the peak for about, terminating partway down the mountain, approximately south of Lake Morning, and west of the upper Vereyken Glacier. Named by US-ACAN (1994) in association with Mount Morning. Mason Spur. An elevated spur, partially ice-covered and over high, which projects eastward from Mount Morning.

Geographic entities mentioned:
surface_form: Lake Morning
instance_of: Lake
coordinates: lat: -78.35
lon: 163.88333333
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
This volcanic group has erupted alkaline lavas during the course of the Cenozoic. It is subdivided into three provinces, the Hallett, the Melbourne and the Erebus province; Mount Morning is the southernmost volcano of the Erebus province. Mount Morning rises from a Paleozoic basement, the Koettlitz Group which crops out close to Gandalf Ridge in the form of granite and metasedimentary rocks.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
The name was suggested by geologist Anne C. Wright, Department of Geoscience, New Mexico Institute of Mining and Technology, a member of the NMUMT field party that camped on the ridge in the 1985–86 season. The party's tent was blown to shreds by 100-knot winds, requiring evacuation of the party by helicopter. This ridge is renowned for consistently strong winds.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
A glacier which, together with Morning Glacier, drains the northeast slopes of Mount Morning. Vereyken Glacier flows north between Riviera Ridge and Hurricane Ridge into Koettlitz Glacier. Named by US-ACAN (1994) after Jill Vereyken, ASA manager of Field Support Services, McMurdo Station, who was active in coordination and planning of science support in Antarctica from 1984. Riviera Ridge.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Testa Ridge. A volcanic ridge, extending north–south between Weidner Ridge and Riviera Ridge on the north slope of Mount Morning. Named by Advisory Committee on Antarctic Names (US-ACAN) (1994) after J. Ward Testa, biologist, University of Minnesota (later of University of Alaska); conducted seal studies during ten field seasons in McMurdo Sound and other coastal regions, 1980–94. Campbell Crag.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Parallel to and about from Weidner Ridge. Named by US-ACAN (1994) after Michael L. Savage, Department of Meteorology, University of Wisconsin. Along with Charles Stearns, he developed the use of automatic weather stations in Antarctica during four field seasons, 1980–86. Morning Glacier. A glacier on the northeast slope of Mount Morning.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
A number of parasitic vents mainly in the form of cinder cones dot the mountain. The volcano was initially active during the Miocene and erupted in two separate stages with a hiatus in between. The older stage has a different chemical composition than the recent one and is heavily eroded by glaciers.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
The volcano was initially active during the Miocene and erupted in two separate stages with a hiatus in between. The older stage has a different chemical composition than the recent one and is heavily eroded by glaciers. The most recent parasitic vents were active about 20,000 years ago and the volcano could erupt again. Geography and geomorphology.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Geology. The West Antarctic Rift is a major geological feature in Antarctica and one of Earth's largest continental rifts. It is a region of active crustal extension and spreading, which may be ongoing today. Volcanic activity occurs at the rift and includes the McMurdo Volcanic Group, a long chain of volcanoes in Victoria Land.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Volcanic activity was focused along geologic lineaments on Mount Morning, which were reused during more recent eruptions. Eruptions took place at Mount Morning about 20,000 years ago, forming well-preserved cinder cones. In the 1960s thermal anomalies were observed at Gandalf Ridge, implying that the volcano may still be active, although ground surveys did not detect fumarolic activity.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Campbell Crag. A rock peak rising to high at the south end of Testa Ridge on the north slope of Mount Morning. Named by US-ACAN (1994) after Richard J. (Rick) Campbell, ASA, fixed-wing Flight Operations Coordinator at McMurdo Station, active in science support in Antarctica from 1981. Weidner Ridge.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Mount Morning is almost entirely covered with snow and ice except where it is ablated by southerly winds. Outcrops of volcanic rocks form the north-northeastern Riviera Ridge and northeastern Hurricane Ridge on the northern flank, Mason Spur on the southern flank and on Helms Bluff on the eastern flank. Gandalf Ridge is a promontory formed by northward-tilted debris and penetrated by Dikes.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: helms
instance_of: Mountain
coordinates: lat: -82.0667
lon: -87.9667
Moraines occur on these two ridges and moraines dating to the Wisconsin glaciation have been reported. Glaciers descending from Mount Morning feed the Koettlitz Glacier. Several lakes are found on the volcano and at its foot, including Lake Morning at the end of the Riviera Ridge and Lake Discovery at the foot of the Hurricane and Gandalf ridges. Geology.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Loading by glaciers may have influenced volcanic activity at Mount Morning, and conversely, the growth of Mount Morning and Discovery may have formed substrates for the formation of new glaciers - initially the mountains may not have had much glaciation.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Thus, Mount Morning was considered dormant by Martin, Cooper and Dunlap 2010 and might be the source of tephra layers found in the area. History and name. The volcano was discovered by the Discovery Expedition in 1901-1904 and named after a relief ship that took part in the expedition. Gandalf Ridge.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
Tolkien's Lord of the Rings. Hurricane Ridge. The eastern of two broad, mainly ice-free ridges that descend north from Mount Morning. Riviera Ridge is the other, to the west, and Gandalf Ridge and Lake Discovery are located at the north end of this ridge. The name was suggested by geologist Anne C.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
The party's tent was blown to shreds by 100-knot winds, requiring evacuation of the party by helicopter. This ridge is renowned for consistently strong winds. Juxtaposed with Riviera Ridge, which is similar in appearance to this ridge to the west. Vereyken Glacier. A glacier which, together with Morning Glacier, drains the northeast slopes of Mount Morning.

Geographic entities mentioned:
surface_form: strong
instance_of: Mountain
coordinates: lat: -70.583333333333
lon: -62.75
Mason Spur was considered by Martin &quot;et al.&quot; 2021 to be a separate volcano from Mount Morning. Owing to the lack of running water, the main edifice (unlike Mason Spur, where traces of marine and water erosion are present) is uneroded and parasitic vents have a young appearance.

Geographic entities mentioned:
surface_form: young
instance_of: Mountain
coordinates: lat: -84.45
lon: 179.8
Mount Morning. Mount Morning is a shield volcano at the foot of the Transantarctic Mountains in Victoria Land, Antarctica. It lies from Ross Island. Mount Morning rises to an elevation of and is almost entirely mantled with snow and ice. A wide summit caldera lies at the top of the volcano and several ice-free ridges such as Hurricane Ridge and Riviera Ridge emanate from the summit.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
The most recent parasitic vents were active about 20,000 years ago and the volcano could erupt again. Geography and geomorphology. Mount Morning lies in Victoria Land, about from Ross Island and at the foot of the Transantarctic Mountains. The Koettlitz Glacier runs along the northwestern foot of Mount Morning and separates it from the Royal Society Range away.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Geography and geomorphology. Mount Morning lies in Victoria Land, about from Ross Island and at the foot of the Transantarctic Mountains. The Koettlitz Glacier runs along the northwestern foot of Mount Morning and separates it from the Royal Society Range away. Mount Discovery lies next to Mount Morning and is separated from it by the Discovery Glacier.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
The volcano rises to above sea level and is capped by a wide caldera that may be the source of a glacier at its northeastern end. Mount Morning has been defined as a large shield volcano that consists of a central volcano overlying an older volcanic complex. With a volume of it is one of the largest volcanoes in the region.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
With a volume of it is one of the largest volcanoes in the region. Fissure vents have produced at least 185 parasitic vents on the slopes of Mount Morning. They are cinder cones, fissure ridges, lava domes and volcanic necks, and their diameters range from a few metres to a few hundred metres. Many of the vents form alignments, some cone craters overlap or the vents themselves have linear shapes.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Lava flows emanate from cones and make up the present-day surface of the volcano. Mount Morning is almost entirely covered with snow and ice except where it is ablated by southerly winds. Outcrops of volcanic rocks form the north-northeastern Riviera Ridge and northeastern Hurricane Ridge on the northern flank, Mason Spur on the southern flank and on Helms Bluff on the eastern flank.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Dikes, lava domes, lava flows and pyroclastic deposits are found in outcrops. Mason Spur also contains breccias from pillow lavas, while Gandalf Ridge features a diamictite and a cross-cutting fault. Mason Spur was considered by Martin &quot;et al.&quot; 2021 to be a separate volcano from Mount Morning.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: martin
instance_of: Mountain
coordinates: lat: -69.6667
lon: -62.9833
Glacial erosion has eroded some parts of the volcano, leaving volcanic necks in Pinnacle Valley, has etched glacial striations into exposed volcanic rocks and deposited glacial till. The Vereyken Glacier descends the northeastern slopes of Mount Morning between Hurricane Ridge and Riviera Ridge. Moraines occur on these two ridges and moraines dating to the Wisconsin glaciation have been reported.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Moraines occur on these two ridges and moraines dating to the Wisconsin glaciation have been reported. Glaciers descending from Mount Morning feed the Koettlitz Glacier. Several lakes are found on the volcano and at its foot, including Lake Morning at the end of the Riviera Ridge and Lake Discovery at the foot of the Hurricane and Gandalf ridges. Geology.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Mount Morning rises from a Paleozoic basement, the Koettlitz Group which crops out close to Gandalf Ridge in the form of granite and metasedimentary rocks. Based on rocks erupted by Mount Morning, the crust appears to be thin and has a calc-alkaline composition. Tectonic sutures in this basement may have allowed magma to ascend to the surface in the Mount Morning region. Composition.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Aegirine, aenigmatite, amphibole, augite, clinopyroxene, alkali feldspar, glass, iron oxide-titanium oxide, nepheline, plagioclase and quartz make up the groundmass. The volcanic rocks contain xenoliths consisting of syenite and of rocks from older stages of Mount Morning activity.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
The older rocks define the &quot;Mason Spurr lineage&quot; while the younger ones are referred to as the &quot;Riviera Ridge lineage&quot;. Basaltic rocks are concentrated on the lower slopes, while phonolite is mainly found in the upper sector of Mount Morning.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Basaltic rocks are concentrated on the lower slopes, while phonolite is mainly found in the upper sector of Mount Morning. The composition changes between the early and late volcanic activity of Mount Morning may be due to alteration in crustal magma processes. Eruption history. Mount Morning has been active during the Miocene, Pliocene and Pleistocene.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
The composition changes between the early and late volcanic activity of Mount Morning may be due to alteration in crustal magma processes. Eruption history. Mount Morning has been active during the Miocene, Pliocene and Pleistocene. Argon-argon dating and potassium-argon dating have been used to infer the duration of volcanic activity at Mount Morning.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Even older activity at Mount Morning may be recorded in volcanic deposits from Cape Roberts which go back to 24.1 million years ago. This is a long lifespan for a volcano by Antarctic standards, and may be due to tectonic factors that kept magma generation focused on Mount Morning for a long time.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Volcanic activity mostly occurred under the atmosphere, with the exception of some lavas that may have been erupted in a subaqueous environment and hyaloclastites which have been used to infer that glaciers existed there 15.4 million years ago. Volcanic activity was focused along geologic lineaments on Mount Morning, which were reused during more recent eruptions.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Volcanic activity was focused along geologic lineaments on Mount Morning, which were reused during more recent eruptions. Eruptions took place at Mount Morning about 20,000 years ago, forming well-preserved cinder cones. In the 1960s thermal anomalies were observed at Gandalf Ridge, implying that the volcano may still be active, although ground surveys did not detect fumarolic activity.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
History and name. The volcano was discovered by the Discovery Expedition in 1901-1904 and named after a relief ship that took part in the expedition. Gandalf Ridge. A volcanic ridge at the northwest end of Hurricane Ridge, to the north of Mount Morning on Scott Coast. Gandalf is a whimsical name put forward by geologist Philip R.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Tolkien's Lord of the Rings. Hurricane Ridge. The eastern of two broad, mainly ice-free ridges that descend north from Mount Morning. Riviera Ridge is the other, to the west, and Gandalf Ridge and Lake Discovery are located at the north end of this ridge. The name was suggested by geologist Anne C.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
This ridge is renowned for consistently strong winds. Juxtaposed with Riviera Ridge, which is similar in appearance to this ridge to the west. Vereyken Glacier. A glacier which, together with Morning Glacier, drains the northeast slopes of Mount Morning. Vereyken Glacier flows north between Riviera Ridge and Hurricane Ridge into Koettlitz Glacier.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Kyle. The name alludes to the warm sunny conditions experienced on the ridge in contrast to the storm conditions previously experienced on nearby &quot;Hurricane Ridge&quot;. Testa Ridge. A volcanic ridge, extending north–south between Weidner Ridge and Riviera Ridge on the north slope of Mount Morning. Named by Advisory Committee on Antarctic Names (US-ACAN) (1994) after J.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Ward Testa, biologist, University of Minnesota (later of University of Alaska); conducted seal studies during ten field seasons in McMurdo Sound and other coastal regions, 1980–94. Campbell Crag. A rock peak rising to high at the south end of Testa Ridge on the north slope of Mount Morning. Named by US-ACAN (1994) after Richard J.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Named by US-ACAN (1994) after Richard J. (Rick) Campbell, ASA, fixed-wing Flight Operations Coordinator at McMurdo Station, active in science support in Antarctica from 1981. Weidner Ridge. A linear volcanic outcrop, approximately long, between and parallel to Savage Ridge and Testa Ridge on the north slope of Mount Morning. Named by US-ACAN after George A.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Along with Charles Stearns he developed the use of automatic weather stations in Antarctica in the period 1982–2005. Savage Ridge. A linear volcanic outcrop approximately long descending from the northwest slope of Mount Morning. Parallel to and about from Weidner Ridge. Named by US-ACAN (1994) after Michael L. Savage, Department of Meteorology, University of Wisconsin.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Along with Charles Stearns, he developed the use of automatic weather stations in Antarctica during four field seasons, 1980–86. Morning Glacier. A glacier on the northeast slope of Mount Morning. The glacier flows from the peak for about, terminating partway down the mountain, approximately south of Lake Morning, and west of the upper Vereyken Glacier.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Morning Glacier. A glacier on the northeast slope of Mount Morning. The glacier flows from the peak for about, terminating partway down the mountain, approximately south of Lake Morning, and west of the upper Vereyken Glacier. Named by US-ACAN (1994) in association with Mount Morning. Mason Spur. An elevated spur, partially ice-covered and over high, which projects eastward from Mount Morning.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Named by US-ACAN (1994) in association with Mount Morning. Mason Spur. An elevated spur, partially ice-covered and over high, which projects eastward from Mount Morning. Named by US-ACAN in 1963 for Robert Mason, USARP Representative at McMurdo Station, 1962–63.

Geographic entities mentioned:
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: mount morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
In the 1960s thermal anomalies were observed at Gandalf Ridge, implying that the volcano may still be active, although ground surveys did not detect fumarolic activity. Thus, Mount Morning was considered dormant by Martin, Cooper and Dunlap 2010 and might be the source of tephra layers found in the area. History and name.

Geographic entities mentioned:
surface_form: martin
instance_of: Mountain
coordinates: lat: -69.6667
lon: -62.9833
The rest of the municipality borders the Norwegian Sea. The municipality is quite rugged with the exception of the area east of Myre which is very flat and marshy. The large lake Alsvågvatnet lies near this flat area, just east of the village of Alsvåg. This flat area lies just to the north of the tall mountain Snøkolla, which is the highest point in the municipality.

Geographic entities mentioned:
surface_form: Alsvågvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 68.895555555556
lon: 15.208055555556
The municipality is quite rugged with the exception of the area east of Myre which is very flat and marshy. The large lake Alsvågvatnet lies near this flat area, just east of the village of Alsvåg. This flat area lies just to the north of the tall mountain Snøkolla, which is the highest point in the municipality. The Anda Lighthouse is located on the tiny island of Anden. Important Bird Area.

Geographic entities mentioned:
surface_form: Snøkolla
instance_of: Mountain
countries: Norway
coordinates: lat: 68.84
lon: 15.1925
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. The Lewis Overthrust extends over from Mount Kidd in Alberta, south to Steamboat Mountain which is located 55 miles south of Old Man of the Hills, which places Old Man of the Hills within the southern part of the Lewis Overthrust. Climate.

Geographic entities mentioned:
surface_form: Mount Kidd
instance_of: Mountain
countries: Canada
coordinates: lat: 50.89361111111111
lon: -115.18972222222222
surface_form: old man of the hills
instance_of: Mountain
countries: United States
coordinates: lat: 48.053055555556
lon: -112.7725
surface_form: old man of the hills
instance_of: Mountain
countries: United States
coordinates: lat: 48.053055555556
lon: -112.7725
surface_form: steamboat mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.3661
lon: -112.3999
Old Man of the Hills. Old Man of the Hills is an mountain summit located in Teton County of the U.S. state of Montana. Description. Old Man of the Hills is located along the Rocky Mountain Front, which is a subset of the Rocky Mountains. It is situated seven miles east of the Continental Divide, along the Bob Marshall Wilderness boundary, on land managed by Lewis and Clark National Forest.

Geographic entities mentioned:
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9727
lon: -74.3732
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.7955
lon: -79.1808
surface_form: old man of the hills
instance_of: Mountain
countries: United States
coordinates: lat: 48.053055555556
lon: -112.7725
surface_form: rocky mountain
instance_of: Landform
countries: United States
coordinates: lat: 41.7958
lon: -71.055
surface_form: rocky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.0918
lon: -74.2151
Old Man of the Hills. Old Man of the Hills is an mountain summit located in Teton County of the U.S. state of Montana. Description. Old Man of the Hills is located along the Rocky Mountain Front, which is a subset of the Rocky Mountains. It is situated seven miles east of the Continental Divide, along the Bob Marshall Wilderness boundary, on land managed by Lewis and Clark National Forest.

Geographic entities mentioned:
surface_form: old man of the hills
instance_of: Mountain
countries: United States
coordinates: lat: 48.053055555556
lon: -112.7725
Topographic relief is significant as the summit rises above the creek in. Geology. Old Man of the Hills is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.

Geographic entities mentioned:
surface_form: old man of the hills
instance_of: Mountain
countries: United States
coordinates: lat: 48.053055555556
lon: -112.7725
Climate. Based on the Köppen climate classification, Old Man of the Hills has an alpine subarctic climate characterized by long, usually very cold winters, and mild to warm summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geographic entities mentioned:
surface_form: old man of the hills
instance_of: Mountain
countries: United States
coordinates: lat: 48.053055555556
lon: -112.7725
Old Man of the Hills is located along the Rocky Mountain Front, which is a subset of the Rocky Mountains. It is situated seven miles east of the Continental Divide, along the Bob Marshall Wilderness boundary, on land managed by Lewis and Clark National Forest. The nearest town is Choteau, 32 miles to the southeast, and the nearest higher neighbor is Mount Frazier, 2.6 miles to the south-southeast.

Geographic entities mentioned:
surface_form: mount frazier
instance_of: Mountain
countries: United States
coordinates: lat: 48.018055555556
lon: -112.75166666667
Panjshir Province. Panjshir (Pashto: پنجشېر, Dari: پنجشیر, lit. 'five lions'), commonly known as Panjsher, is one of the 34 provinces of Afghanistan, located in the northeastern part of the country containing the Panjshir Valley. The province is divided into seven districts and contains 512 villages. The main inhabitants of the province are Shamali Tajiks, who speak Dari.

Geographic entities mentioned:
surface_form: Panjshir Valley
instance_of: Valley
countries: Afghanistan
coordinates: lat: 35.266666666667
lon: 69.466666666667
Two days later the September 2001 attacks occurred in the United States and this led to the start of a major U.S.-led war in Afghanistan. Containing the Panjshir Valley, in April 2004 Panjshir District of Parwan Province was turned into a province under the Karzai administration. The Afghan National Security Forces (ANSF) established several bases in the province.

Geographic entities mentioned:
surface_form: Panjshir Valley
instance_of: Valley
countries: Afghanistan
coordinates: lat: 35.266666666667
lon: 69.466666666667
Hitikau. Hitikau is a volcanic mountain of Ua Huka, in the Marquesas Islands of Polynesia. It has an elevation of, the highest point of the island, and lies to the northeast of the village of Hane. Auberge Hitikau. There is a small hostel and restaurant at the foot of the mountain in the village of Auberge Hitikau, named after the mountain.

Geographic entities mentioned:
surface_form: hitikau
instance_of: Mountain
countries: France
coordinates: lat: -8.90559959
lon: -139.52149963
It has an elevation of, the highest point of the island, and lies to the northeast of the village of Hane. Auberge Hitikau. There is a small hostel and restaurant at the foot of the mountain in the village of Auberge Hitikau, named after the mountain. It contains four double rooms, with an eatery noted for its goat and pork dishes and &quot;kaveka&quot; omelettes.

Geographic entities mentioned:
surface_form: hitikau
instance_of: Mountain
countries: France
coordinates: lat: -8.90559959
lon: -139.52149963
Amezketa. Amezketa (Spanish &quot;Amézqueta&quot;) is a town located in the province of Gipuzkoa, in the Basque Autonomous Community, in the North of Spain. It is located at the foot of Txindoki.

Geographic entities mentioned:
surface_form: Txindoki
instance_of: Mountain
countries: Spain
coordinates: lat: 43.023888888889
lon: -2.0869444444444
Other villages in Hedrum include Gjone, Kvelde, Skinmo, and Verningen. Hedrum municipality was located in the Lågendalen valley, the lower part of the valley that follows the river Numedalslågen. The valley is relatively flat and dominated by agricultural areas. The valley is surrounded by wooded hills which rise up towards tall mountain peaks.

Geographic entities mentioned:
surface_form: Lågendalen
instance_of: Valley
countries: Norway
One of his most ambitious railroad projects was the Southern's Stevenson extension, which aimed to connect Chattanooga with Stevenson, Alabama. The extension required the construction of a tunnel through Lookout Mountain. Completed in 1908, the tunnel was described by one newspaper as &quot;one of the biggest feats in railroading in the south.&quot;
Panama Canal bid.

Geographic entities mentioned:
surface_form: Lookout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
Sisophon River. rj56bwwo8zq5r7eko4qryo158lez" xml:space="preserve">Serei Sophorn River () is a river that flows through Banteay Meanchey province in Cambodia. It is a major tributary of the Tonlé Sap.

Geographic entities mentioned:
surface_form: Tonlé Sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
Knockboy. Knockboy () is a 706-metre-high mountain on the border between counties Cork and Kerry in Ireland. Geography. Knockboy is the highest peak in the Shehy Mountains and the highest mountain in County Cork with its summit shared with County Kerry. It is the 104th highest peak in Ireland. Geology.

Geographic entities mentioned:
surface_form: knockboy
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.802
lon: -9.442
Two Cruiser IIs and one Cruiser III were impressed into RAF service in 1940. Surviving aircraft. The fuselage of a Cruiser III (G-ACYK) is on display at the National Museum of Flight, East Fortune, Scotland. This aircraft crashed on 14 January 1938; in 1973, the cabin section was moved by helicopter from the crash site on the Hill of Stake near Largs to the museum.

Geographic entities mentioned:
surface_form: Hill of Stake
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.8167
lon: -4.76667
Camp Ibis was designated a California Historic Landmark (No. 985.6). The site of the Camp Ibis East of Needles, California off Highway 95, north of Interstate 40 in San Bernardino County, California. The camp was originally named after the Ibis railroad siding in Piute Valley. The camp was located at the west side of the Dead Mountains Wilderness.

Geographic entities mentioned:
surface_form: Piute Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.3033
lon: -114.881
Mehraneh river. Mehraneh roud is a river in Tabriz, crossing through the middle of Tabriz. It starts in the Sahand mountains.

Geographic entities mentioned:
surface_form: Sahand
instance_of: Mountain
countries: Iran
coordinates: lat: 37.73
lon: 46.5
Kafni Glacier. The Kafni Glacier is located in the upper reaches of the Kumaon Himalayas, to the southeast of Nanda Devi. The glacier gives rise to the Kafni River, which is a tributary of the Pindar River. The Pindar River is a tributary to Alaknanda River, which eventually is one of the two headstreams of the Ganges.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
In 2014, Dennis finished second overall behind Bradley Wiggins at the Tour of California, after placing second to Wiggins in the individual time trial on stage two, before winning the third stage to Mount Diablo. He also placed second in the Circuit de la Sarthe, and the Commonwealth Games time trial behind England's Alex Dowsett. 2014–2015.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
2018. Having won a third consecutive title in the Australian National Time Trial Championships in January, Dennis took a stage victory in the individual time trial at the Abu Dhabi Tour, which moved him into the race lead prior to the final day; he ultimately finished ninth overall, after losing time on the uphill finish to Jebel Hafeet.

Geographic entities mentioned:
surface_form: Jebel Hafeet
instance_of: Mountain
countries: United Arab Emirates
Oman
coordinates: lat: 24.05796
lon: 55.78086
Chukarska reka. The Chukarska reka () is a 37 km long river in eastern Bulgaria that flows into Lake Burgas, which drains into the Black Sea. The river takes its source from the northern slope of the peak of Shumnoto Kale (376 m) in the Hisar Heights at an altitude of 325 m, about one kilometer west of the village of Chukarka.

Geographic entities mentioned:
surface_form: Lake Burgas
instance_of: Lake
countries: Bulgaria
coordinates: lat: 42.5
lon: 27.4
It flows in direction southeast through the Burgas Plain in a wide valley covered with farmlands. The river flows into the westernmost edge of Lake Burgas some 3 km southwest of the Dolno Ezerovo neighbourhood of the city of Burgas. The lake itself drains into the Gulf of Burgas in the Black Sea. Its drainage basin covers a territory of 129 km2.

Geographic entities mentioned:
surface_form: Lake Burgas
instance_of: Lake
countries: Bulgaria
coordinates: lat: 42.5
lon: 27.4
Clew Bay Heritage Centre. Clew Bay Heritage Centre is a local history museum in Westport, County Mayo, Ireland. Located in the west of the town, on the pier, it illustrates the social history and heritage of the Clew Bay area and Westport. Topics covered include Croagh Patrick, Grace O'Malley, John MacBride, Maud Gonne, the Irish War of Independence, the 1798 Rebellion and schooling in the area.

Geographic entities mentioned:
surface_form: Croagh Patrick
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.7595
lon: -9.6584
It could also be enclosed by a low wall constructed from horizontal logs resting on a fieldstone base, with square towers at the corners. The most widely known example of the &quot;pogost&quot;, and Russian wooden architecture in general, is Kizhi Pogost on Kizhi Island in Lake Onega. Usage in Finland and Latvia.

Geographic entities mentioned:
surface_form: Lake Onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556