Question: Diakhandara Glacier is located in the mountain range that is on which continent?

Context articles: Huallanca mountain range
Adishi Glacier
Qaflankuh Mountain Range
Neptune Glacier
DuBridge Range
Diakhandara Glacier
Elkhead Mountains
Karatag River
Rush Peak
Pamir Mountains

The Huallanca mountain range (possibly from Quechua, "wallanka" mountain range; a cactus plant ("Opuntia subulata"); name of several localities and name of a mountain in the Wallanka range, also spelled "Huallanca"), Chawpi Hanka ("central ridge (or peak)", "Chaupi Janca, Chaupijanca") or Shikra Shikra ("sikra" woven basket, "many baskets", "Shicra Shicra") lies in the Andes of Peru.
 It is located in the Ancash Region, Bolognesi Province.
 The Wallanka mountain range is a small range southeast of the Cordillera Blanca and north of the Waywash mountain range extending between 9°52' and 10°03'S and 76°58' and 77°04'W for about 19 km in a northeasterly direction.
Adishi Glacier (Georgian: ადიშის მყინვარი ) is a valley glacier located in the central part of the Greater Caucasus Mountain Range in the Svaneti Region of Georgia.
 The glacier lies on the southern slopes of the Caucasus.
 The length of the Adishi Glacier is 9 km and its surface area is 12.9 km2 .
 The tongue of the glacier descends down to 2298 m above sea level.
 The glacier feeds off of the runoff and ice flows from the adjacent glaciers that are located on the southern slopes of Tetnuldi, Gistola and Lakutsia.
 The Adishi Glacier is the source of the river Adishischala.
 The glacier takes its name from the nearby village Adishi.
Qaflankuh or Qaflankuh Mountain Range (Persian: رشته کوه‌ها‌ی قافلانکوه / Reshteh Kuh-hā-ye Qāflānkuh) is a mountain range that is located about 20 kilometres north of the city of Zanjan in Zanjan Province, Iran.
 With an average width of almost 20 kilometres and a length of about 100 kilometres, this mountain range is stretched in a northwest-southeast direction, beginning from northwest of Zanjan, passing north of Zanjan and ending southeast of Zanjan.
 The Qezel Owzan River flows in a valley that separates Qaflankuh Mountains on the south from Talish Mountains on the north.
 With an elevation of 2971 metres, Mount Sendan Dagh is the highest mountain of the range which is located in the southeast section of this mountain range.
 There are some mineral hot springs containing sulphur in different parts of this range.
 Geologically, Qaflankuh Mountain Range was formed during the Tertiary volcanism and plutonism and is made mainly of the Eocene volcanic rocks with very small sections of intrusive rocks in the northern and southern parts of the range.
Neptune Glacier ( ) is a glacier on the east coast of Alexander Island, Antarctica, 12 nautical miles (22 km) long and 4 nautical miles (7 km) wide, flowing east into George VI Sound and the George VI Ice Shelf to the south of Triton Point.
 Although Neptune Glacier is not located within the mountain range Planet Heights, the glaciers name derives from the mountain range along with many other nearby glaciers named after planets of the Solar System.
 There are also other nearby landforms named in association with these glaciers.
 The glacier was first sighted from the air by Lincoln Ellsworth on November 23, 1935, and roughly mapped from photos obtained on that flight by W.L.G. Joerg.
 The mouth of the glacier was positioned in 1936 by the British Graham Land Expedition (BGLE).
 Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for the planet Neptune following a Falkland Islands Dependencies Survey (FIDS) survey in 1949.
 The head of the glacier was mapped from air photos taken by the Ronne Antarctic Research Expedition (RARE), 1947–48, by Searle of the FIDS in 1960.
DuBridge Range ( ) is a mountain range, over 20 nautical miles (37 km) long in the Admiralty Mountains.
 The range trends southwest–northeast between Pitkevitch Glacier and Shipley Glacier and terminates at the north coast of Victoria Land just west of Flat Island, Antarctica.
 This mountain range was first mapped by the United States Geological Survey from surveys and U.S Navy air photos, 1960–63, and was named by the Advisory Committee on Antarctic Names for Lee DuBridge, a member of the National Science Board for several years, and Science Advisor to the President of the United States, 1969–70.
 The mountain range lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Diakhandara Glacier is a glacier situated on the south slope of the Gissar Range, in the Pamir Mountains of northern Tajikistan, situated at where the Diakhandara River flows into the Karatag River.
 The glacier was first observed on 18 August, 1940, and the first investigation of the glacier was made in 1958 and discovered to be completely covered in moraines.
The Elkhead Mountains are a mountain range in Colorado.
 The mountain range is considered to be low altitude within Colorado as the mountains are under 11000 ft .
 Located within Routt and Moffat counties, the mountain range is far from metropolitan areas and has few lakes and streams, so it attracts few visitors.
 The mountain range is a volcanic range and all of the peaks were formed by volcanic action.
 The mountain range extends approximately 16 mi east to west and 10 mi north to south, and its center is located at , approximately 20 mi northeast of Craig and north of Hayden, Colorado 13 mi south of the Wyoming border.
 Almost all of the peaks within the Elkhead Mountains are a part of Routt National Forest.
 Significant peaks are: Bears Ears, Sugar Loaf, Saddle Mountain, Black Mountain, Pilot Knob, and Meaden Peak.
The Karatag or Qoratagʻ is a river of northwestern Tajikistan and eastern Uzbekistan.
 It flows through Shirkent National Park and flows down the south slopes of the Gissar Range mountain range.
 Large seismic landslides occur in the river basin and it also contains several glacial lakes.
 It is an inflow to the Surkhandaria River.
 Zambar River and the Diakhandara River are tributaries, the latter of which meets the Karatag at the Diakhandara Glacier.
Rush Peak is a mountain in the Karakoram mountain range of Central Asia.
 It is located in the Nagar District of Gilgit-Baltistan, Pakistan.
 While not a high peak by local standards, it is noteworthy as a remote trekking destination.
 It can be reached via Nagar Valley and Hoper Village.
 The peak can be accessed via Hoper Glacier (Bualtar Glacier) and Barpu Glacier.
 The peak is relatively easy to climb in the summer months and ascents have been made by amateur climbers without proper mountaineering gear.
 In winter, access to the mountain is made difficult by heavy snows.
 The top of the peak provides stunning views of Miar Peak (6,824 m), Miar Glacier and Phuparash Peak (6,574 m).
 On a clear day, one can look east and see some of the world's highest mountains, including K2 and Broad Peak.
 At the mountain's base lies one of the world's highest alpine lakes, Rush Lake (4,694m).
The Pamir Mountains, or the Pamirs, are a mountain range in Central Asia at the junction of the Himalayas with the Tian Shan, Karakoram, Kunlun, Hindu Kush, Suleman and Hindu Raj ranges.
 They are among the world’s highest mountains.