which two continents are separated by the Ural mountain range
it is divided by the Himalayas mountain range (Asia/Europe)
The Ural Mountains separate Europe and Asia.
The north-south trending mountain range that is part of the traditional boundary between Europe and Asia is the Ural Mountains. These mountains stretch over 1,550 miles from the Arctic Ocean to the Ural River in Kazakhstan, separating the two continents.
Two continents collided to form the Himalayan mountain range in Asia. The collision between the Indian Plate and the Eurasian Plate continues to push the Himalayas upwards, making them one of the youngest and tallest mountain ranges in the world.
which two continents are separated by the Ural mountain range
The Himalayas
Africa and North America
it is divided by the Himalayas mountain range (Asia/Europe)
The Ural Mountains separate Europe and Asia.
The north-south trending mountain range that is part of the traditional boundary between Europe and Asia is the Ural Mountains. These mountains stretch over 1,550 miles from the Arctic Ocean to the Ural River in Kazakhstan, separating the two continents.
Two continents collided to form the Himalayan mountain range in Asia. The collision between the Indian Plate and the Eurasian Plate continues to push the Himalayas upwards, making them one of the youngest and tallest mountain ranges in the world.
A major mountain range in Europe is the Alps. In North America, two major mountain ranges are the Appalachian Mountains and the Rocky Mountains.
The Himalayas mountain range is formed by the collision of the Indian Plate with the Eurasian Plate. This collision has created some of the tallest peaks in the world, including Mount Everest.
Both the Urals and the Caucuses separate Europe and Asia.
A low point on a ridge between two mountain peaks is called a saddle. A low level separating two mountains is called a valley.
Two continents that are currently colliding are the Indian Plate and the Eurasian Plate, resulting in the formation of the Himalayan mountain range. This collision has been ongoing for millions of years and is a geologically active region prone to earthquakes and mountain-building processes.