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Ngga Pulu

Summit on Mount Carstensz, Indonesia


Summary

Summit on Mount Carstensz, Indonesia

FieldValue
nameNgga Pulu
photoNgga_Pulu,_15,951_ft.jpg
photo_captionThe North Wall Firn glacier with Ngga Pulu (flat peak, right) and Sumantri (sharp peak, center).
elevation_m4862
prominence_m100
prominence_ref
mapIndonesia Central Papua#Indonesia
coordinates
label_positionbottom
locationCentral Papua, Indonesia
rangeSudirman Range
first_ascent5 December 1936 by Anton Colijn, Jean Jacques Dozy and Frits Wissel
easiest_routerock/snow/ice climb

Ngga Pulu is summit on the north rim of Mount Carstensz in the western part of the island of New Guinea rising 4862 m. Trigonometric measurements showed that Ngga Pulu was (and had been for many centuries before) the highest mountain of New Guinea and also the highest summit of the Australia-New Guinea continent. The elevation of Ngga Pulu in 1936 was about 4907 m, and it was the highest and most prominent peak between the Himalaya and the Andes. However, due to glacial melting, Ngga Pulu lost a high margin of elevation in the 20th century, being surpassed by Puncak Jaya. It is surrounded by one of Indonesia's only three glaciers, including the one on Puncak Trikora.

Name

Ngga Pulu is the only summit of Mount Carstensz with a regular indigenous name. Sumantri and the current summit used to be called the NW and SE peaks of Ngga Pulu. Heinrich Harrer labeled the NW peak Ngapalu on his map drawn in 1962, while calling the SE Peak (the current Ngga Pulu) Sunday Peak. When Indonesia took control of Western New Guinea in 1963, the peaks were known as Puntjak Soekarno and Puncak Jaya until the Carstensz Pyramid was established as the highest summit. Sometime after 1973 the NW summit was renamed to Sumantri, in honor of the recently deceased Minister of Energy and Mineral Resources.

Climbing history

Anton Colijn, Jean Jacques Dozy and Frits Wissel reached the summit on 5 December 1936 during the Carstensz Expedition over the Northwall Firn. Subsequent ascendants were Heinrich Harrer and company in 1962 and a Japanese-Indonesian expedition in 1964.https://web.archive.org/web/20181126152211/http://papuaweb.org/dlib/bk/hope1976/01.pdf. Dick Isherwood first ascended the 600 m high north face in a solo effort in September 1972.

Loss of elevation and ice

The 1936 Carstensz Expedition measured a height of 5030 m for this summit. An Australian topographic survey in 1973 established that the 1936 barometric estimates were all between 117 and too high, suggesting a true height of 4907 ± for Ngga Pulu in 1936. All prominence key cols in the inner Carstensz area were entirely ice-covered, so the Carstensz Pyramid at the time was a just a sub-peak of Ngga Pulu, with around 200 m of prominence. The Australian scientific expeditions of 1971–73 measured Ngga Pulu at 4862 m, and the ice melting in the key col resulted in a prominence of around 300 m. By the year 2000, all New Guinea glaciers outside the Carstensz area had disappeared. Inside the Carstensz area, a former sub-peak, the now rocky summit of Sumantri, is now some meters higher than the still ice-covered Ngga Pulu. Thus, now Ngga Pulu has less than 100 m of prominence as a sub-peak of the 4870 m Sumantri, which itself has a prominence around 350 m. The glacial melting has produced significant elevation changes for prominence key cols in the inner Carstensz area and it is also probable that other former big ice-capped peaks in New Guinea lost various meters in elevation such as Puncak Mandala, East Carstensz Top and Ngga Pilimsit. Scientists are monitoring the glacial retreat and estimate that by about 2020–2030, all New Guinea glaciers may disappear.

References

Sources

References

  1. [http://www.peakbagger.com/peak.aspx?pid=24496 "Ngga Pulu, Indonesia"] Peakbagger.com. Peakbagger currently gives a prominence of less than 100 m for this peak. Retrieved 2012-07-09.
  2. R.J. Isherwood, [http://www.alpinejournal.org.uk/Contents/Contents_1973_files/AJ%201973%20188-194%20Isherwood%20Dugundugoo.pdf The Dugundugoo], [[The Alpine Journal]] 1973, pp 188–194.
  3. Edward G. Anderson, [http://www.papuaweb.org/dlib/bk/hope1976/02.pdf Topographic Survey and Cartography] in ''The Equatorial Glaciers of New Guinea'', A.A. Balkema, Rotterdam, 1976
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