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View to the east across the Kali Gandaki from the trail leading toward Hidden Valley and Dhaulagiri basecamp to the Nilgiri Peaks (7061m, 6940m, 6839m respectively from north to south). Overturned anticlinal closure of Cambro-Ordovician (Annapurna Formation) and Ordovician (Nilgiri Formation) sedimentary rocks (Godin, 2003).

Godin, L. (2003) Structural evolution of the Tethyan sedimentary sequence in the Annapurna area, central Nepal Himalaya. Journal of Asian Earth Sciences, v. 22 pp. 307-328

PhotoID234

View to the east across the Kali Gandaki from the trail leading toward Hidden Valley and Dhaulagiri basecamp to the Nilgiri Peaks (7061m, 6940m, 6839m respectively from north to south). Overturned anticlinal closure of Cambro-Ordovician (Annapurna Formation) and Ordovician (Nilgiri Formation) sedimentary rocks (Godin, 2003).

Godin, L. (2003) Structural evolution of the Tethyan sedimentary sequence in the Annapurna area, central Nepal Himalaya. Journal of Asian Earth Sciences, v. 22 pp. 307-328

PhotoID234

Photograph: K. Larson