1. Ascent class
  2. Climbing area
  3. Peak, its height, ascent route
  4. Estimated difficulty category
  5. Route characteristics
  6. Number of pitons driven
  7. Number of travel hours
  8. Number of overnight stays
  9. Names of team leader and participants, their sports qualification
  10. Team coach
  11. Date of ascent
  12. Organization

combined 2.9.6 Dagestan mountains Mt. Addala-shukhgel, 4151 m, via N ridge 2B height difference — 850 m, average steepness — 45°, length of sections: 1st cat. diff. – 590 m, 2nd – 200 m, 3rd – 75 m rocky – 5/0, icy – 2/0 7 no overnight stays Shanavazov Sh. — 1st sports category Il'ina E. — 2nd sports category Aliskandiev A. A. — 3rd sports category Dzhavatkhanova P. — 2nd sports category Kozorezov E. F. July 9, 1986 Mountain Club of Dagestan State University "Eos" img-0.jpeg

  1. Addala via W-NW ridge. 4B
  2. Addala via N ridge. 2B, optional. M-t group's route img-1.jpeg

Section R1–R2 img-2.jpeg

Sections R3–R6 img-3.jpeg Sections R2–R4 img-4.jpeg Section R0–R1 img-5.jpeg The first known attempt to ascend Mt. Addala-shukhgel via N ridge was made in May 1974 by a group led by K. E. Akhmedkhanov, but it was unsuccessful due to heavy snow cover on the route and approaches. The group turned back from the R3–R4 section.

In June 1974, a group led by A. Aligaziev ascended Addala via N ridge, having started the ascent from the Northwest cirque. No route description was made.

Judging by the contents of a note found in the summit cairn, on October 5, 1985, a duo of climbers from Baku, T. Tagiev and A. Zharkov, completed the described route. The group did not register with the KSP and did not provide a route description. The difficulty assessment of the route is not given in the note.

Description of the approach to the route: From the "Sulak-high-mountain" weather station, follow the left-bank (orographically) moraine of the NE Addala glacier and descend to the glacier about 40 meters from its end.

Proceed along the glacier, initially in the direction of the N-E wall, and then, after passing the 2nd stage of the glacier's icefall, turn right and approach the rocks and scree of the N ridge. From the weather station, it takes 1–1.5 hours. Movement on the glacier is only in teams.

Explanation for the diagram: — The ridge is composed of heavily destroyed shales. — Gendarmes — outcrops of sandstone, slabs. — Belaying is required along the entire ridge.

During the ascent, the route was in ideal condition. Snow cover may complicate its passage within 1/2 – 1st cat. diff.

Descent is recommended via the Charasen-anda ridge to the Tsobegodari kutaan.

img-6.jpeg

C-3 sphere of r. Aggan-Mayrent

Route diagram

img-7.jpeg

Peak Addala 6. 60 m, 5°, 1 200 m 50°, 2 5. 5°, 1 15 m, 65°, 3 80 m, 15°, 1 300 m, 20°, 1 60 m, 45°, 3 Sections: R0–R1 – MS. SULAK — ice plateau R1–R2 – ice plateau – N ridge R2–R3 – along the ridge to the wall R3–R4 – wall R4–R5 – along the ridge to the saddle R5–R6 – saddle – ridge shoulder R6–R7 – shoulder – summit 300 m, 25°, 1

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