In today's world, Aldan (river) has become increasingly relevant. Whether due to its impact on society, its influence on popular culture or its relevance in the scientific field, Aldan (river) has become a topic of general interest for a wide spectrum of audiences. In this article we will explore topics related to Aldan (river), analyzing its importance, its implications and its evolution over time. From its origins to the present, Aldan (river) has been the object of debate, controversy and fascination, and in the following lines we will seek to shed light on this topic that is so relevant in the contemporary world.
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Aldan | |
---|---|
Location | |
Country | Russia |
Physical characteristics | |
Source | Stanovoy Mountains |
• location | Neryungri, Sakha |
• coordinates | 56°29′06″N 123°44′02″E / 56.485°N 123.734°E |
• elevation | 1,224 m (4,016 ft) |
Mouth | Lena |
• location | Sakha |
• coordinates | 63°26′46″N 129°33′13″E / 63.44611°N 129.55361°E |
• elevation | 43 m (141 ft) |
Length | 2,273 km (1,412 mi) |
Basin size | 729,000 km2 (281,000 sq mi) |
Discharge | |
• average | 5,489 m3/s (193,800 cu ft/s) (near mouth) |
Basin features | |
Progression | Lena→ Laptev Sea |
Tributaries | |
• left | Amedichi, Amga |
• right | Timpton, Uchur, Maya, Allakh-Yun |
The Aldan (Sakha and Russian: Алдан) is the second-longest right tributary of the Lena in the Sakha Republic in eastern Siberia. The river is 2,273 kilometres (1,412 mi) long, of which around 1,600 kilometres (990 mi) is navigable. It has a drainage basin of 729,000 square kilometres (281,000 sq mi).
The river was part of the River Route to Okhotsk. In 1639 Ivan Moskvitin ascended the rivers Aldan and Maya and crossed to the Ulya to reach the Sea of Okhotsk.
Its basin is known for gold and for Cambrian fossils.
The Aldan rises in the Stanovoy Mountains southwest of Neryungri. It flows roughly in a northeast / ENE direction south of the Lena Plateau across the Aldan Highlands, where it forms the northern border of the Sunnagyn Range. Then it flows past Aldan and through Tommot, Ust-Maya, Eldikan and Khandyga before turning northwest. In its last stretch it flanks the southern slopes of the Verkhoyansk Range and joins the Lena near Batamay.
The river's main tributaries are the following: