paragraph_text: In 1984, India launched Operation Meghdoot to capture the Siachen Glacier in the contested Kashmir region. In Op Meghdoot, IAF's Mi-8, Chetak and Cheetah helicopters airlifted hundreds of Indian troops to Siachen. Launched on 13 April 1984, this military operation was unique because of Siachen's inhospitable terrain and climate. The military action was successful, given the fact that under a previous agreement, neither Pakistan nor India had stationed any personnel in the area. With India's successful Operation Meghdoot, it gained control of the Siachen Glacier. India has established control over all of the 70 kilometres (43 mi) long Siachen Glacier and all of its tributary glaciers, as well as the three main passes of the Saltoro Ridge immediately west of the glacier—Sia La, Bilafond La, and Gyong La. Pakistan controls the glacial valleys immediately west of the Saltoro Ridge. According to TIME magazine, India gained more than 1,000 square miles (3,000 km2) of territory because of its military operations in Siachen.

paragraph_text: The Fossil Falls is a unique geological feature, located in the Coso Range of California in the United States. Volcanic activity in the mountain range, along with meltwater from glaciers in the nearby Sierra Nevada, played a role in the creation of the falls. They are located near the community of Little Lake, off US 395 (at a red cinder cone called "Red Hill") on Cinder Road to Red Hill, with signs to Fossil Falls.

paragraph_text: Ramorino Glacier () is the long glacier situated northwest of upper Crosswell Glacier and southeast of Cervellati Glacier on the east slope of Sentinel Range in the Ellsworth Mountains, Antarctica. It flows northeastwards between Epperly Ridge and Shinn Ridge, and enters Crosswell Glacier northwest of Mount Segers. The feature was named by US-ACAN in 2006 after Maria Chiara Ramorino, manager of the Italian team that compiled and promulgated the SCAR Composite Gazetteer of Antarctica, 1998-2006.

paragraph_text: Honnør Glacier () is a glacier flowing to the east side of Lützow-Holm Bay, Antarctica, to the north of the Byvågåsane Peaks. A glacier tongue extending seaward from this feature was mapped by the Lars Christensen Expedition 1936–37 and named Honnørbrygga (the honor wharf). The Japanese Antarctic Research Expedition, 1957–62, found the glacier tongue had broken off but amended the original naming to apply to the glacier.

paragraph_text: Mount Phillips () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Lupfer Glacier is located on the east slope of Mount Phillips.

paragraph_text: Spit-Ball Sadie is a 1915 American short comedy film featuring Harold Lloyd. It was Lloyd's first appearance as his "Lonesome Luke" character.

paragraph_text: The Hohtälli is a mountain of the Swiss Pennine Alps, located southeast of Zermatt in the canton of Valais. It lies on the range that separates the Findel Glacier from the Gorner Glacier, between the Gornergrat and the Stockhorn. Its summit has an elevation of 3,275 metres and includes a cable car station. The Hohtälli is part of a ski area and features several ski runs leading down the mountain.

paragraph_text: Wilkins Runway is a single runway aerodrome operated by Australia, located on upper glacier of the ice sheet Preston Heath, Budd Coast, Wilkes Land, on the continent of Antarctica, but southeast of the actual coast. It is named after Sir Hubert Wilkins, a pioneer of Antarctic aviation and exploration.

paragraph_text: On Earth, 99% of glacial ice is contained within vast ice sheets in the polar regions, but glaciers may be found in mountain ranges on every continent except Australia, and on a few high-latitude oceanic islands. Between 35°N and 35°S, glaciers occur only in the Himalayas, Andes, Rocky Mountains, a few high mountains in East Africa, Mexico, New Guinea and on Zard Kuh in Iran. Glaciers cover about 10 percent of Earth's land surface. Continental glaciers cover nearly 13,000,000 km2 (5×10^6 sq mi) or about 98 percent of Antarctica's 13,200,000 km2 (5.1×10^6 sq mi), with an average thickness of 2,100 m (7,000 ft). Greenland and Patagonia also have huge expanses of continental glaciers.

paragraph_text: Maine Ridge () is a ridge that extends northwest–southeast between Matataua Glacier and Tedrow Glacier in the Royal Society Range, Antarctica. It was named after the University of Maine, Orono, in association with other features in the immediate area named for educational institutions, such as Emmanuel Glacier, Johns Hopkins Ridge, and Rutgers Glacier.

paragraph_text: The Royal Society Range () is a majestic mountain range in Victoria Land, Antarctica. With its summit at , the massive Mount Lister forms the highest point in this range. Mount Lister is located along the western shore of McMurdo Sound between the Koettlitz, Skelton and Ferrar glaciers. Other notable local terrain features include Allison Glacier, which descends from the west slopes of the Royal Society Range into Skelton Glacier.

paragraph_text: The Cannonball Cliffs () are cliffs at the south side of the terminus of Neptune Glacier on the east side of Alexander Island, Antarctica. The feature consists of two east-west ridges about high, joined by a narrow north-south ridge. The feature was mapped from trimetrogon air photography taken by the Ronne Antarctic Research Expedition, 1947–48, and from survey by the Falkland Islands Dependencies Survey, 1948–50. The name was applied by the UK Antarctic Place-Names Committee for the sandstone in the area, which contains numerous spherical, brown concretions known as "cannon-ball" concretions.

paragraph_text: Lambert Glacier is a major glacier in East Antarctica. At about 60 miles (100 km) wide, over 250 miles (400 km) long, and about 2,500 m deep, it holds the Guinness world record for the world's largest glacier. It drains 8% of the Antarctic ice sheet to the east and south of the Prince Charles Mountains and flows northward to the Amery Ice Shelf. It flows in part of Lambert Graben and exits the continent at Prydz Bay.

paragraph_text: Hydraotes Chaos is a broken-up region in the Oxia Palus quadrangle of Mars, located at 0.8° North and 35.4° West. It is 417.5 km across and was named after a classical albedo feature name. More information and more examples of chaos regions can be found at Martian chaos terrain. The area contains small conical edifices, called Hydraotes Colles, which were interpreted as the Martian equivalent of terrestrial cinder cones formed by volcanic activity.

paragraph_text: Håhellerskarvet, meaning "shark cave mountain" in Norwegian, is a high partially ice-covered mountain between Austreskorve Glacier and Lunde Glacier in the Mühlig-Hofmann Mountains of Queen Maud Land, East Antarctica. Other nearby geographic features include Håhelleren Cove, indenting the north side of Håhellerskarvet, Håhelleregga Ridge, an irregular rock ridge just north of Håhellerskarvet, Håhellerbotnen Cirque, a large cirque on the east side of Håhelleregga Ridge, and Jøkulkyrkja, a broad, ice-topped mountain located east of Lunde Glacier. All of these geographic features were plotted from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60).

paragraph_text: Due to its location at the South Pole, Antarctica receives relatively little solar radiation. This means that it is a very cold continent where water is mostly in the form of ice. Precipitation is low (most of Antarctica is a desert) and almost always in the form of snow, which accumulates and forms a giant ice sheet which covers the land. Parts of this ice sheet form moving glaciers known as ice streams, which flow towards the edges of the continent. Next to the continental shore are many ice shelves. These are floating extensions of outflowing glaciers from the continental ice mass. Offshore, temperatures are also low enough that ice is formed from seawater through most of the year. It is important to understand the various types of Antarctic ice to understand possible effects on sea levels and the implications of global cooling.

paragraph_text: Ball Glacier is a glacier long with the head located between Mount Lister and Mount Hooker on the east side of the Royal Society Range. The glacier flows northeast between Craw Ridge and Tasman Ridge into Blue Glacier. It was named by the New Zealand Geographic Board after Gary Ball, a New Zealand mountaineer who climbed Mount Lister with an Italian field party, 1976–77, and camped on this glacier; he was field assistant with R.H. Findlay’s New Zealand Antarctic Research Program party to this area, 1980–81.

paragraph_text: Atlantis Chaos is a region of chaos terrain in the Phaethontis quadrangle of Mars. It is located around 34.7° south latitude, and 177.6° west longitude. It is encompassed by the Atlantis basin. The region is across, and was named after an albedo feature at 30° S, 173° W.

paragraph_text: Griffiths Glacier is a prominent cirque-type glacier located northeast of Crisp Glacier in the Gonville and Caius Range, Victoria Land, Antarctica. The feature drains east-southeast to Debenham Glacier to the east of Second Facet. It was named after Harold Griffiths (died 1974) who was associated with Antarctic exploration for over 50 years. He was instrumental in the New Zealand Antarctic Society's campaign to get the New Zealand Government to establish a presence in Antarctica.

paragraph_text: Bastion Hill () is a prominent ice-free feature in the Brown Hills of Antarctica, rising to and projecting southward into Darwin Glacier just east of Touchdown Glacier. The descriptive name, the hill supposedly suggesting a bastion, was given by the Darwin Glacier Party of the Commonwealth Trans-Antarctic Expedition (1956–58).

Question: Which continent has the mountain range that includes Ball Glacier?
Answer: Antarctica