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Tupopdan

Coordinates: 36°33′26″N 74°56′01″E / 36.557184°N 74.933606°E / 36.557184; 74.933606
From Wikipedia, the free encyclopedia

Tupopdan
Passu Cathedral
North aspect
Highest point
Elevation6,106 m (20,033 ft)[1][2]
Prominence1,255 m (4,117 ft)[2]
Parent peakKarun Kuh[2]
Isolation12.7 km (7.9 mi)[2]
Coordinates36°33′26″N 74°56′01″E / 36.557184°N 74.933606°E / 36.557184; 74.933606[2]
Geography
Tupopdan is located in Karakoram
Tupopdan
Tupopdan
Location of Tupopdan
Tupopdan is located in Gilgit Baltistan
Tupopdan
Tupopdan
Tupopdan (Gilgit Baltistan)
Tupopdan is located in Pakistan
Tupopdan
Tupopdan
Tupopdan (Pakistan)
Map
Interactive map of Tupopdan
LocationKashmir
CountryPakistan
Administrative territoryGilgit-Baltistan
DistrictHunza
Parent rangeKarakoram
South Ghujerab Mountains
Geology
Rock typeLimestone[1]
Climbing
First ascentJuly 6, 1987

Tupopdan, also known as Passu Cathedral or Passu Cones, is a mountain in northern Pakistan.

Description

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Tupopdan is a 6,106-metre (20,033-foot) summit in the South Ghujerab Mountains subrange of the Karakoram. The mountain is situated 10 kilometres (6.2 mi) north of the village of Passu and the mountain is one of the most scenic sights along the Karakoram Highway.[1] Precipitation runoff from this mountain's slopes drains into tributaries of the Hunza River. Topographic relief is significant as the north face rises 1,700 metres (5,577 ft) in 1.5 kilometres (0.93 mi), and the summit rises 3,600 metres (11,811 ft) above the Hunza River in seven kilometres (4.3 mi). The first ascent of the summit was achieved on July 6, 1987, by Andy Cave and John Stevenson via the Northeast Ridge.[3][4] One source claims that Tupopdan means "sun-drenched mountain",[5] whereas another source states it is a Wakhi word meaning "hot rock" which alludes to snow shedding quickly from the south slopes in winter.[6]

Climate

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Based on the Köppen climate classification, Tupopdan is located in a tundra climate zone with cold, snowy winters, and cool summers.[7] Weather systems are forced upwards by the mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. This climate supports two unnamed glaciers descending from the north slope. The summer months offer the most favorable weather for viewing or climbing this peak.[8]

See also

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References

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  1. ^ a b c Insight Guides Pakistan: Travel Guide eBook, Apa Publications (UK) Limited, 2025, ISBN 9781839054204
  2. ^ a b c d e "Tupopdan". Peakvisor.com. Retrieved 1 June 2025.
  3. ^ Asia, Pakistan, Tupopdan, Richard Haszko, 1988, publications.americanalpineclub.org, Retrieved June 1, 2025.
  4. ^ 1988 American Alpine Journal, The Mountaineers Books, 1988, ISBN 9781933056357, p. 260.
  5. ^ John Mock, Trekking in the Karakoram & Hindukush, Lonely Planet Publications, 2002, ISBN 9781740590860, p. 281.
  6. ^ John King, Central Asia: A Lonely Planet Travel Survival Kit, Lonely Planet Publications, 1996, ISBN 9780864423580, p. 503.
  7. ^ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN 1027-5606.
  8. ^ Passu Cones, TravelerTrails, travelertrails.com, Retrieved June 1, 2025.
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