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DBpedia 2015-10

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Matches in DBpedia 2015-10 for { ?s ?p "Margerie Glacier is a 21-mile-long (34 km) tide water glacier in Glacier Bay in Alaska and is part of the Glacier Bay National Park and Preserve. It begins on the south slope of Mount Root, at the Alaska-Canada border in the Fairweather Range, and flows southeast and northeast to Tarr Inlet. It was named for the famed French geographer and geologist Emmanuel de Margerie (1862–1953), who visited the Glacier Bay in 1913. It is an integral part of the Glacier Bay, which was declared a National Monument on February 26, 1925, a National Park and Wild Life Preserve on December 2, 1980, a UNESCO declared World Biosphere Reserve in 1986 and a World Heritage Site in 1992. While most of the tidewater and terrestrial glaciers in the Park are stated to be thinning and receding over the last several decades, Margerie Glacier is said to be stable and Johns Hopkins Glacier is stated to be advancing, on the eastern face of the Fairweather Range.Located at the end of the Glacier Bay, Margerie Glacier extends over a width of about 1 mile (1.6 km) and extends upstream for a length of 21 miles (34 km) to its source on the southern slopes of the hill of Mount Root, at the Alaska-Canada border. Mount Root (elevation 12,860 feet (3,920 m)), named Boundary Peak 165, is a mountain in Alaska and British Columbia, is part of the Fairweather Range (Mt. Fairweather is the tallest peak with elevation of15,325 feet (4,671 m)) of the Saint Elias Mountains. It is named after Elihu Root, who was among the diplomats involved in settling the Alaska boundary dispute between the United States and Canada. The Margerie Glacier starts from this range of mountains from Mount Root.Margerie Glacier at Mile 63 is perpendicular to the Grand Pacific Glacier at Mile 64 (widest glacier in the Glacier bay with width of about 2 miles (3.2 km)). It flows in southeast and northeast direction to Tarr Inlet, one mile (1.6 km) north of the terminus of Grand Pacific Glacier and 87 miles (140 km) northwest of Hoonah. Glacier Bay provides excellent glacier experiences of both receding and advancing glaciers existing side by side. Tarr Inlet forms the northwestern part of the Glacier Bay named in 1912 for professor of geology Dr Ralph Tarr. The Glacier Bay region, which in 1750 was a mass of ice of a single glacier, has undergone a dynamic change and is now a 65-mile long fjord.Glacier Bay and the Margerie Glacier are approachable only by air and water. The steep dropoff of the Margerie Glacier cliff facilitates large cruise ships to park close to the glacier from where one gets incredible views of the glacier.In a study of the bed rock geology and mineral resources of the Glacial Bay, out of 17 areas classified as containing mineral deposits, Margerie Glacier has been identified as containing copper deposits."@en }

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