Geology

The geological structure of the Zomin National Nature Park gives it a unique character and coloration, significantly influencing the formation of geomorphological and forest landscapes.

According to studies conducted by researchers of the Tashkent State University, the following geomorphological landscape types have been identified and examined:

• Moist, high-mountain nivation forms of relief, located at 3700–4000 m above sea level;

• Erosional-denudational high mountains, dissected by steep cliffs and deep gorges, located at 3000–3700 m;

• Paleozoic-era pre-Paleogene denudational coal formations, found at around 3500 m;

• Erosional-accumulative highlands with semi-steep slopes, 2100–2750 m;

• Mid-mountain pre-Paleogene denudational layers, formed during the Paleozoic era, 2200–3000 m;

• Accumulative-erosional terraced mid-mountains, 1650–2500 m;

• Canyon-shaped valleys and erosional-gravitational landforms, 1650–2160 m;

• Low-mountain accumulative-erosional foothills, 1200–2500 m above sea level.

These geomorphological features demonstrate that, despite their diversity, the high-mountain regions play a decisive role in the differentiation of natural conditions.

In the northern part of the park (particularly along the Yettikechuv, Urikli, and Usmonli streams), the geological structure consists mainly of rocky slopes.

Paleozoic coal deposits played a crucial role in the formation of the famous Supa and Chortangi depressions.

These distinctive geological features make the area highly attractive for tourists and alpinists alike.