Title: Mount Cleveland (Vermont)
Content:  Mount Cleveland is a mountain in the Green Mountains in the U.S. state of Vermont. Located in the Breadloaf Wilderness of the Green Mountain National Forest, its summit is in the town of Lincoln in Addison County. The mountain is named after Grover Cleveland, former president of the United States. Mount Cleveland is one of five peaks in Vermont's Presidential Range.
Title: Mount Cleveland (Montana)
Content:  Mount Cleveland is the highest mountain in Glacier National Park, located in Montana, United States. It is also the highest point in the Lewis Range, which spans part of the northern portion of the Park and extends into Canada. It is located approximately 3 mi southeast of the southern end of Waterton Lake, and approximately 5 mi south of the US/Canada border. The east side of the future national park was purchased by the federal government from the Blackfoot Confederacy in 1895 during the second term of President Cleveland. According to the United States Board on Geographic Names, the mountain is named for the former president. While not of great absolute elevation (the mountain is more than 2300 ft lower than Granite Peak, the highest 
Title: Mount Cleveland (Alaska)
Content:   Mount Cleveland is an almost symmetrical andesite stratovolcano in the Islands of Four Mountains, a volcanic group in the Aleutian Arc. Like all stratovolcanoes, Mount Cleveland grew as explosive eruptions, effusive eruptions, and lahars built it layer by layer into a convex shape. It lies southeast of Mount Carlisle and northeast of Herbert Island. Mount Cleveland forms the western half of Chuginadak Island, a broad and uneven bell-shaped landmass, and is the highest of the four volcanic islands. The island is completely uninhabited; the nearest settlement is Nikolski on Umnak Island, about 75 km eastward. Mount Cleveland is 8 - 8.5 km wide at its base and roughly 29 km3 in volume. The volcano's slope increases markedly with 
Title: Mount Cleveland (Montana)
Content:  in Montana), Mount Cleveland is notable for its large, steep rise above local terrain. For example, its west flank rises over 5500 ft in less than 2 mi; the northwest face, steepest on the mountain, rises 4000 ft in less than 0.4 mi. The other faces show almost as much vertical relief. This scale and steepness of relief is quite rare in the contiguous United States. Mount Cleveland is 50th on a list of peaks in the contiguous U.S. with the most topographic prominence. The massif upon which Mount Cleveland is situated also includes 10001 ft Kaiser Point, which is the seventh tallest peak in the park and is only .67 mi to the northeast. The first recorded ascent of Mount Cleveland was in 
Title: Mount Cleveland (Alaska)
Content:  Mount Cleveland (also known as Cleveland Volcano) is a nearly symmetrical stratovolcano on the western end of Chuginadak Island, which is part of the Islands of Four Mountains just west of Umnak Island in the Fox Islands of the Aleutian Islands of Alaska. Mt. Cleveland is 5675 ft high, and one of the most active of the 75 or more volcanoes in the larger Aleutian Arc. Aleutian natives named the island after their fire goddess, Chuginadak, who they believed inhabited the volcano. In 1894 a team from the U.S. Coast and Geodetic Survey visited the island and gave Mount Cleveland its current name, after then-president Grover Cleveland. One 
Title: Mount Cleveland (Alaska)
Content:  from 19° at its lower flanks to 35° near its summit. Like many other Aleutian volcanoes, Cleveland's flanks are especially rough up to 300 m, covered by multiple overlapping lava flows and debris fans that form an apron around the mountain. Lava flows are always built on top of debris flows as a result of the snow melt caused by the emission of heat just before an eruption. The flows are generally short, under 1 km, and thin, less than 10 m thick, and are somewhat vegetated. Although Mount Cleveland is the tallest mountain in the group, it is rarely completely snowed in because of its constant activity disrupts snowfall. A lack of extant erosion shows that Mount 
Title: Mount Cleveland (Vermont)
Content:  Mount Cleveland stands within the watershed of Lake Champlain, which drains into the Richelieu River in Québec, the Saint Lawrence River, and then eventually into the Gulf of Saint Lawrence. The north side of Mount Cleveland drains into Stetson Brook, thence into the Mad River, the Winooski River, and into Lake Champlain. The south and east sides of Mount Cleveland drain into Austin Brook and then into the Mad River. The west side of Mount Cleveland drains into the New Haven River, thence into Otter Creek, and into Lake Champlain.
Title: Mount Cleveland (Alaska)
Content:  The native Aleut name for Mount Cleveland is Chuginadak (the name currently given to the island as a whole), referring to the Aleut fire goddess, thought to reside in the volcano. The volcano's name is a reference to its constant activity, and shows that it was likely highly active even in the distant past. Aleut oral tradition states that, at one time, the western and eastern halves of Chuginadak were separate islands, and that the isthmus joining them was created by volcanic activity sometime in prehistory. The "Islands of Four Mountains" name, the geographic group name for Cleveland and its neighbors, was given to the islands by Russian cartographers in the 19th century. Its current name, Mount Cleveland, was given to it by a U.S. Coast and Geodetic Survey expedition in 1894, when it was originally observed by the USS Concord. Like the other volcanoes in the Four Islands group, which were named after prominent American politicians at the time, Mount Cleveland was named after then-president Grover Cleveland.
Title: Mount Cleveland (Alaska)
Content:  is likely a Holocene volcano, forming within the last 10,000 years. All known events have occurred at Mount Cleveland's summit vent, but there are at least five small andesite to dacite volcanic domes on the lower flanks. At times Cleveland has had a summit lava dome. The volcano has no caldera. The eastern half of Chuginadak, to which Mount Cleveland is connected by a narrow isthmus, consists of several low-lying volcanic cones and two prominent peaks that have been heavily eroded, partly by glaciers. Known as the Tana volcanic complex, the two features measure 1170 m and 1093 m in elevation. A sample of rhyolite has been recovered from Concord Point, the easternmost point on the island.
Title: Mount Cleveland (Alaska)
Content:  as its remoteness makes it a difficult area to investigate, and discrepancies in names have caused confusion between events there and those on nearby Carlisle. Even today, not all possible events are confirmed as eruptions by the Alaska Volcano Observatory, and many are listed as "possible." In observed history, Mount Cleveland may have first erupted in 1744; the first confirmed eruption occurred in 1828. The volcano erupted again in 1836 (possibly), 1893, 1897 (possibly), 1929 (possibly), 1932, and 1938 (possibly). The first notable eruption from Mount Cleveland was a Volcanic Explosivity Index (VEI) 3 Vulcanian eruption that occurred between June 10 and June 13, 1944. Lava flows extended 5 km from the summit, and an ash 

Question: In what country is Mount Cleveland?
Answer: United States of America.
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