Ice. Bogdanovich is the largest glacier at the junction of Mal. Alma-Ata and Komsomolsky spurs, it belongs to the type of valley glaciers and has a length of the open part of about 3 km. Bogdanovich is located on the northern exposure of the ridge that connects the peaks of Amangeldy in the west and Karlytau in the east. The glacier consists of two parts where the main one originates on the northern peaks of the Karlytau ice peak and on the igneous peaks of Karlytau and from the western slopes of the Komsomol peak. In this chamber of the glacier there are the Komsomol (2A), Heroev-Panfilovtsev (2A), Uchitel (1B) passes. The left branch of the glacier flows from the northwestern slopes of the Amangeldy peak and closes with the lane. Pioneer (1B). In the middle part of the flow, both branches of the glacier connect and give rise to the river's sources. Sauruksai.
The glacier is named in honor of Karl Ivanovich Bogdanovich, this is the researcher who studied the Vernenskoye earthquake, his work was greatly influenced by seismological schemes and tectonic schemes. The Bogdanovich Glacier is one of the most popular places for climbers. Many routes pass through it, and the view from it is very beautiful.
How to get there?
You can get to the glacier by arriving at Chimbulak ski resort, take the cable car to the Talgarsky pass. From this pass there is a well-trodden path, then you will follow the fossilized scree to the Bogdanovich tongue. Further the route will pass through the Abaya pass (represents a narrow gap in a ridge of rocks). The further path goes along the Abai glacier itself to the path leading to Tuyuk-Su, we reached the devil’s gorge and then cross from the pass to the road.
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