Aksoran
Mountain in Kazakhstan
From Wikipedia, the free encyclopedia
Aksoran (Kazakh: Ақсораң; Russian: Аксоран) is a mountain in Aktogay District, Karaganda Region, Kazakhstan.[4]
| Aksoran | |
|---|---|
| Ақсораң | |
Mt. Aksoran | |
| Highest point | |
| Elevation | 1,565 m (5,135 ft)[1] |
| Prominence | 843 m (2,766 ft)[2] |
| Coordinates | 48°25′37″N 75°28′47″E[1][3] |
| Geography | |
  Aksoran Location in Kazakhstan | |
| Country | Kazakhstan |
| Region | Karaganda Region |
| District | Aktogay |
| Parent range | Kyzylarai; Kazakh Uplands |
| Geology | |
| Rock age | Late Paleozoic |
| Mountain type | Granite massif |
| Climbing | |
| Easiest route | from Shabanbay Bi |
The mountain is located about 10 kilometres (6 mi) to the ENE of Shabanbay Bi village, formerly known as Shilym.[5] Geologically the peak is made up of Permian granite.[6]
Geography
Aksoran rises in the Kyzylarai, a massif of the Kazakh Uplands (Saryarka).[7] The mountain has a barren appearance and its slopes are steep, rocky and strongly dissected.[4]
With an elevation of 1,565 metres (5,135 ft), it is the highest mountain in the Kazakh Uplands, as well as the highest point of Central Kazakhstan.[6][1][3]
The Kyzylarai massif extends approximately 70 km west–east and 50–60 km north–south across parts of the Karaganda Region.[7] Aksoran has a topographic prominence of 843 metres, making it the dominant summit of the massif.[2]
In clear weather, distant massifs such as Bektauata may be visible from the summit.[4]
Climate
Aksoran lies within the continental steppe climatic zone of Central Kazakhstan. Winters are cold, with average January temperatures around −15 °C, while summers are warm to hot, with July averages near 25 °C.[8]
Annual precipitation averages between 300 and 400 mm, falling mainly in spring and early summer.[8] Snow accumulation during winter contributes to seasonal runoff that feeds small intermittent streams in the surrounding uplands.[4]
Geology
Aksoran consists primarily of Late Paleozoic granites formed during the Hercynian orogeny.[9] These granitic intrusions are associated with tectonic processes that shaped the Kazakh Uplands during the Carboniferous–Permian period.[9]
Surrounding formations include Devonian–Carboniferous sedimentary deposits such as limestones and terrigenous sequences that were later uplifted and intruded by granite bodies.[10]
Flora and fauna
Vegetation in the Aksoran area is characteristic of the Kazakh steppe, with feather grass (Stipa) and wormwood (Artemisia) dominating lower elevations.[11] Pine forests occur in parts of the Kyzylarai massif.[12]
Wildlife includes argali (Ovis ammon), lynx (Lynx lynx), Pallas’s cat (Otocolobus manul), and red fox (Vulpes vulpes). Birds of prey such as the golden eagle (Aquila chrysaetos) and Eurasian eagle-owl (Bubo bubo) inhabit the region.[13]
Several species present in the Kyzylarai region are listed in Kazakhstan’s Red Data Book of endangered species.[13]
Tourism
Aksoran is a destination for hiking and eco-tourism. The ascent from Shabanbay Bi involves approximately 560–600 metres of elevation gain, with a round trip typically taking between 4 and 8 hours.[5]
Infrastructure is limited, and visitors generally rely on local guesthouses in Shabanbay Bi village.[14]