Map including Koramlik (Ku-la-mu-le-k'o) (DMA, 1980)
2004, “Late Quaternary slip-rate on the Altun Fault west to the Qarqan River”, in F. Wang, Xiwei Xu, Rongzhang Zheng, W.-B. Chen, editors, Seismol Geol / Dizhen Dizhi[1], volume 26, Research Gate, →ISSN, →OCLC, archived from the original on May 12, 2021:
The method of calculating the slip-rate of a fault is to divide the displacement of a ridge lies between two neighboring terraces of one river by the age of the lower terrace. The displacements of rivers are not considered in this study because of its uncertainty. At Koramlik, the slip-rate of the Altun Fault since 6.02 ± 0.47ka BP is 11.6 ± 2.6mm/yr, and since 15.76 ± 1.19ka BP is 9.6 ± 2.6mm/yr.
2004, Earthquake Research in China[2], volume 18, →ISSN, →OCLC, page 399:
[...]south to Koramlik village, a seasonal river runs from mountains northward and passes the village (site A in Fig. 3).
[2007 September, Communication Construction Administration Bureau of Xinjiang Uigur Autonomous Region for the Asian Development Bank, “PRC: Xinjiang Regional Road Improvement Project (Korla-Kuqa Section)”, in Asian Development Bank[4], archived from the original on June 06, 2023, page 11:
Now, telephone is not available for each village in project affected area, the signal of China Mobile not covering this region, having weak signal of China Mobile in Kulamuleke township headquarter, no telephone set in households visited and no mobile telephone neither]
2008, World Atlas Trade & Logistics Edition[5], World Trade Press, →ISBN, page 86:
Koramlik
[2011 October 8, “Man realizes villagers’ dream of watching film”, in China Daily[6], archived from the original on 17 September 2023[7]:
Tong Gemin screens a film in the yard of a villager in Kulamuleke village on Oct 5, 2011.]
