Skuta (2532 m) is a prominent peak in the central Kamnik–Savinja Alps. It stands at the junction between the high‑mountain karst plateaus of Veliki podi to the west and Mali podi to the east. Its position between Grintovec and the Rinka peaks forms an important section of the main ridge above the Kamniška Bistrica valley and Logarska dolina.

Geographical setting

Skuta is situated:

  • above the Kamniška Bistrica valley to the south,

  • above Logarska dolina to the north,

  • between Grintovec (2558 m) to the west and Mala Rinka and Turska gora to the east,

  • in an area where routes from Kamniška Bistrica, Jezersko, and Logarska dolina converge.

On its western slope, just below the summit, lies the distinctive rock formation Štruca (2457 m), a long, rounded monolith that is one of the characteristic features of the Veliki podi karst.

Geomorphology

Skuta is composed of compact Triassic limestone, which has shaped:

  • steep, broken northern slopes descending toward Logarska dolina,

  • smooth, glacially polished surfaces on the Veliki podi plateau,

  • karst features such as karren, fissures, and small dolines on the southern and eastern slopes,

  • scree‑filled gullies and ledges formed by freeze‑thaw weathering.

The area is distinctly alpine, with strong winds, long‑lasting snow cover, and significant temperature fluctuations that continually reshape the terrain.

Access routes

1. Via Kokrško sedlo

  • Starting point: Kamniška Bistrica → Kokrško sedlo → Skuta.

  • A technically demanding route across the southern slopes.

  • Walking time: 5–6 hours.

2. Via Kamniško sedlo and Turski žleb

  • A long and exposed high‑mountain route.

  • Suitable for experienced mountaineers.

3. From Logarska dolina via Okrešelj

  • Starting point: Logarska dolina → Okrešelj → Turski žleb → ridge toward Skuta.

  • Demanding and partly exposed.

4. Via Mlinarsko sedlo

  • Starting point: Ravenska Kočna → Češka koča → Mlinarsko sedlo → Skuta.

  • A ridge route with exposed sections.

Character and significance

Skuta combines:

  • a pronounced high‑mountain karst landscape,

  • a varied ridge environment between Grintovec and the Rinka peaks,

  • demanding approaches from three major alpine valleys,

  • proximity to the distinctive rock formation Štruca on its western slope.

A visit to Skuta offers insight into the central Kamnik–Savinja Alps, where karst plateaus, steep walls, and open ridges meet in a compact high‑mountain setting.