Because both ranges are the result of two geologic plates "crashing" at each other. In the case of the Himalayas, they are the result of the Indian subcontinent crashing into the Eurasian Plate, and for the Sierra Madre Occidental, they result from the Pacific Plate moving northwards with respect of the North American Plate.
The Himalayas are Fold Mountains
andes and himalayas
young fold mountains are like Himalayas, the Alps and man other.
The three tallest fold mountains in the world are Mount Everest in the Himalayas, K2 in the Karakoram Range, and Kangchenjunga, also in the Himalayas.
The Himalayas are Fold Mountains
When two continents collide, mountains called "fold mountains" are formed. This process is known as orogeny, and examples of such mountains include the Himalayas and the Alps. The collision forces the rocks to compress and fold, creating vast mountain ranges.
Rocky Mountains, Andes Mountains, Alps, Himalayan Mountains, Appalachian Mountains
The Himalayas are a young, fold mountain range formed by the collision of the Indian and Eurasian tectonic plates. They are known for their high peaks, including Mount Everest, and are home to a diverse range of ecosystems and cultures.
Fold mountains are commonly found at convergent plate boundaries, where tectonic plates collide and push against each other, causing the Earth's crust to fold and create mountain ranges. Examples of fold mountains include the Himalayas, the Andes, and the Alps.
The Jura Mountains and the Zagros Mountains are examples of the fold mountains. The fold mountain is formed as a result of the effects if the folding on layers within the upper part of the crust of the earth.
The Himalayas are known to be youngfold mountains. Young, because these have been formed relatively recently in the earth's history, compared to older mountain ranges like the Aravallis in India, and the Appalachian in the USA. They are known as fold mountains because the mountains extend for 2500 km in length in a series of parallel ridges or folds.
The Himalayas are among the youngest fold mountains in the world, formed around 40-50 million years ago as a result of the collision between the Indian Plate and the Eurasian Plate. These mountains are still actively rising due to ongoing tectonic activity in the region.