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Ascent Passport.

  1. Ascent category — high-altitude.
  2. Ascent area, range — Central Pamir, Akademii Nauk range.
  3. Peak, its height, route — p. Kommunizma 7495 m, via the counterfort of the SW slope of the Belyaev Glacier.
  4. Estimated category of difficulty — 6B.
  5. Route characteristics: height difference — 2825 m, length of sections with 5–6 category of difficulty — 1425 m, average steepness up to 6950 m — 55°.
  6. Pitons hammered: on bivouacs — 4 rock; for belay: rock — 33, ice — 14.
  7. Number of climbing hours — 32.
  8. Number of nights and their characteristics: three nights at heights 6100, 6700, 6950 m.
  9. Full name of the leader and participants:
    1. Ilyinsky E.T. — MS, leader.
    2. Valiev K.Sh. — CMS, participant.
    3. Khrishtchaty V.N. — CMS, participant.
    4. Chumakov V.N. — CMS, participant.
  10. Coach — Ilyinsky E.T., Master of Sports, Honored Coach of KazSSR.
  11. Dates of departure and return: August 23, 1977 — August 28, 1977.

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Brief explanation for the table

On August 22 at 17:00, the group approached the counterfort of p. Kommunizma and set up a bivouac at an altitude of 4670 m.

On August 23 at 7:30, they began ascending a steep ice slope towards the saddle on the counterfort.

In the lower part of the slope, they overcame a two-meter bergschrund and, wearing crampons with alternating belay using pitons and remnants of old ice screws, reached the saddle under the first rock tower. The rocks were steep, heavily destroyed, and were overcome with belay using protrusions.

After a short traverse across rock slabs, they reached the second tower. Here, the belay was via pitons and protrusions. A piton was hammered every 30–35 m. The rocks were местами up to 70° steep.

Having overcome the rocks of the second tower, they reached a ridge 60–70 m long. They traversed the ridge with alternating belay using protrusions.

Further:

— a 15-meter rappel down a rope to an ice saddle at the base of a snow-ice slope; — ascent in crampons up the snow-ice slope.

The first rock island, composed of slabs with flow ice, was encountered at an altitude of 5500 m. Here, the belay was via pitons. Having overcome the slabs, they bypassed the hanging glacier to the left across the ice. Here, too, the belay was via ice pitons. At an altitude of 5750–5850 m, they reached the upper part of the icefall. Here, there were many crevasses, which they overcame using snow bridges with alternating belay. Some crevasses had the character of bergschrunds with overhanging upper edges. Such walls were overcome with the first person being lifted or using ice axes.

At 17:00, they stopped for the night in the area of a large bergschrund.

On August 24, they departed at 10:00. They overcame the upper part of the icefall, the steepness of which had increased. местами, there was deep snow up to 1.0 m. In the upper part, under shallow snow, there was ice.

At 12:30, they reached a rock rib. The rocks were heavily destroyed, often covered with flow ice. Steep rock walls up to 70° and 5–6 m high were encountered. img-1.jpeg

Table of main characteristics of the ascent route to p. Kommunizma via the counterfort of the Southwest slope, 6th category of difficulty.

img-2.jpegAround 13:00, a heavy snowfall began. Visibility was no more than 50 m. At 15:00, they set up a bivouac, having chopped out part of a sharp snow ridge at an altitude of 6700 m. For belay on the bivouac, they hammered 4 rock pitons.

On August 25, they departed at 9:00. On the rocks, there was snow up to 15–20 cm deep, flow ice, and almost no protrusions. The belay was via pitons.

At 13:00, they approached a steep rock tower of the shoulder of p. Kommunizma. In the lower part of the tower, there was a steep inner corner. The rocks were covered with snow and flow ice. The length of the section was 15 m. Having overcome it with thorough piton belay, they reached a rock rib with snow drifts. By chopping out the drifts and using piton belay, they traversed the rib, which led to the shoulder of the peak. Further, there was a straightforward snow ridge with cornices, which led to a large depression. Altitude 6950 m.

On August 26 at 10:00, they began the final ascent. On the slopes of the peak, there was a lot of fresh snow, and there was a constant avalanche danger.

Following the usual path: — they reached the summit at 18:00.

DateSectionsAverage steepnessLength in mCharacter of terrainDifficultyConditionWeather conditionsBelayMovement, length in mDeparture and bivouac stop time, climbing hours, weather conditions
23.08.77160°250 mice slope with bergschrund4rare remnants of old ice screwsclear7 rockalternating movement in cramponsDeparture from Belyaeva glacier at 7:30
245–70°400 mridge with snow towers4–5heavily destroyed rocksclear5 rock using protrusionsfree climbing
345°150 mice slope3snow-coveredwarmsimultaneousmovement in crampons
450°300 mice slope with islands of rock slabs5snow-covered, ice, iced slabs, icefall hazardwarm2 rock, 5 icealternating movement in crampons
545°600 micefall4snow, ice, firnwarmsimultaneous and alternating movement in crampons, belay via ice axeStop for bivouac at 17:00, altitude 6100 m, snow-ice cushion, 9.5 climbing hours.
24.08.77650°350 micefall4snow, ice, firnwarm2 rockalternating movement in cramponsDeparture at 10:00, stop for bivouac at 15:00 on a sharp snow ridge, altitude 6700 m, 5 climbing hours.
750°350 mrock rib5snow-covered, destroyed rockssnowfall10 rockfree climbing, 4 rock pitons on bivouac
25.08.77850°200 mrock rib5flow ice, destroyed rocks, snow-coveredsnowfall7 rockfree climbingDeparture at 9:00
990°15 minner corner6snow-covered rocks, flow icesnowfall3 rock using protrusions
1070°160 mrock rib5—, snow driftscold6 rocksimultaneous movement in cramponsStop for bivouac at 18:00 in a snow depression at altitude 6950 m, 9 climbing hours
26.08.7711traverse200 mfirn ridge3cornices, местами icecoldbelay via ice axe
12traverse150 mfirn ridge3avalanche hazardcoldDeparture at 10:00. On the summit by 18:00, 8 climbing hours.
1345°450 mfirn slope3frost
1445°240 mfirn ridge4frost
Total33 rock, 14 iceon bivouac — 4 rock pitons

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