The Ural Mountains are a narrow mountain range that runs about 2,500 kilometers through western Russia, starting from the Arctic Ocean’s coast to northwestern Kazakhstan. The mountains are important for two main reasons. First, they form the popular boundary separating Eurasian landmass into two continents; Europe and Asia. Secondly, they are some of the world’s oldest mountains, dating back 300-250 million years ago. Although erosion has lowered the mountains’ elevations considerably, they are still unusually high for their ages. The range’s highest point is Mount Narodnaya, rising 1,895 meters. The mountains are rich in numerous natural resources, including coal, metal ore, and precious stones, contributing significantly to Russia’s mineral sector.
Origin Of The Name
Russians referred to the Ural Mountains by several names, most of which were derived from the Russian word for stone or rock. The name “Urals” emerged around 16th and 17th centuries and was mainly used to refer to the range’s southern portion. However, it became the name for the entire range around the 18th century. The name may have been derived from a Bashkir word for “stone belt.” According to a Bashkir legend, Ural was a hero who was famous for his legendary and heroic deeds. When he died, his people piled up stones on his grave, which later turned into the huge Ural Mountains. In Russian, the mountain range is known as Uralskie Gory
The Ural Range is a narrow mountain range extending approximately 2,500 kilometers south to north from the Ural River to the Pay-Khoy Ridge. On the north, the mountain chain continues to Novaya Zemlya and Vaygach Islands. The Ural Mountains form Uralian orogenic belt’s major portion. This orogenic belt stretches 3,500 kilometers from the Aral Sea to the Novaya Zemlya. The Urals are relatively narrow, with the width varying from 32 to 145 kilometers.
The Ural Range is divided into five major sections; Southern, Central, Northern, Sub-Arctic (Nether-Polar), and Arctic (Polar). The Polar Urals, the northernmost section, extends about 400 kilometers from north to south between Mount Konstantinov Kamen and Khulga River. They cover about 25,000 square kilometers, with most mountains rising to 1,000-1,100 meters. However, Mount Payer, Polar Urals’ highest peak, rises 1,499 meters above sea level.
The Polar Urals transition into Nether-Polar Ural, which runs 225 kilometers to Shchugor on the south. This section contains much wider and higher peaks, including the entire range’s highest peak, Mount Narodnaya, which rises 1,895 meters above sea level. Other high peaks in the region are Manaraga (1,662 meters) and Karpinsky (1,878 meters). Both the Polar and Nether-Polar Urals are marked by permafrost.
The Northern Ural extends 560 kilometers further south from River Usa. This section contains several ridges topping 1,000 meters, with Mount Telposiz as the highest peak, rising 1,617 meters above sea level. However, most summits are flat and are peneplain remnants. Extensive weathering in this section has resulted in a “sea of stone” formation on mountain slopes. The Central Urals are the range’s lowest section, extending 320 kilometers south to the Ufa River. Mount Sredny Baseg is the highest peak in Central Ural, rising 994 meters.
Southern Urals form the mountain range’s last portion. This section extends 550 kilometers to the Ural River and comprises complex relief with several ridges and valleys, with the ridges rising to 1,200 meters. Mount Yamantau is the highest peak at 1,640 meters. The Southern Urals terminate at the Mughalzhar Hills.
Drainage And Climate
Numerous rivers originate from the Ural Mountains, with the majority draining into the Caspian Sea and the Arctic Ocean. The Pechora River drains parts of Polar, Nether-Polar, and Northern Urals before emptying into the Barents Sea. Its major tributaries include Usa, Shchugor, and Ilych. The Ob River system drains the eastern slope and empties into the Kara Sea. Ob basin’s main rivers include Tavda, Tura, Iset, and Tobol, with most of these rivers frozen for most parts of the year. The Kama and Ural River basins belong to the Caspian Sea drainage basin. The Kama receives its water from Belaya, Chusovaya, and Vishera. The Urals also contains several deep lakes, with the Central and Southern Urals’ eastern slopes having the highest number of lakes. Some of the largest lakes are Tavatuy, Itkul, Turgoyak, and Uvildy.
The lakes' and rivers’ locations are closely related to climate and topography. The Urals’ climate is mainly continental, with the elongated mountain ridges absorbing most sunlight. The regions west of the Urals are much warmer in winter than the eastern region because of the warm Atlantic wind on the west and cold Siberian air on the east. July is the warmest month, with temperatures rising to 50 degrees Fahrenheit. The western areas also receive the most rainfall, at 1,000 mm in the Northern Urals.
Flora And Fauna
The Urals have varied landscapes dominated by steppes and forests. Steppes dominate the southern and southeastern Urals, with meadow steppes developing on lower slopes. These lower parts of the slopes are covered by mountain and zigzag cloves, dropwort, and meadow grass. The forests are generally diverse and dominated by coniferous taiga forests in the western and eastern areas, while the southern region is dominated by deciduous forests. The Northern Urals contain conifers such as Siberian pine, Siberian fir, Siberian spruce, and Scot pine. The Southern Urals are dominated by forests with diverse compositions, while Polar Urals have sparse and low-lying forests. The forests and steppes are home to animals such as brown bears, elk, wolf, fox, lynx, and squirrels.