Explain how the valleys and mountains ranges r formed

Valleys and mountain ranges are formed through the process of tectonic activity. Tectonic activity refers to the movement and interaction of Earth's lithospheric plates, which are large sections of the Earth's crust and upper mantle.

One way valleys are formed is through the process of erosion. The movement of water, such as rivers and streams, gradually wears away the rock and soil, creating a deep channel known as a valley. The force of water flow also plays a role in shaping valleys. Over time, erosion by glaciers, wind, and other natural elements can contribute to the formation and shaping of valleys.

Mountain ranges, on the other hand, are primarily formed through tectonic plate collisions and movements. There are three main types of tectonic plate interactions that lead to mountain formation:

1. Convergent boundaries: When two tectonic plates collide head-on, they create enormous pressure. The intense compression forces the edges of the plates to buckle and fold, resulting in the formation of mountain ranges. For example, the Himalayas were formed when the Indian Plate collided with the Eurasian Plate.

2. Divergent boundaries: At divergent plate boundaries, two tectonic plates move away from each other. This movement causes the Earth's crust to crack and create gaps. Molten rock, known as magma, rises up to fill these gaps, cooling and forming new crust. This process, called seafloor spreading, leads to the formation of underwater mountain ranges, like the Mid-Atlantic Ridge.

3. Transform boundaries: At transform plate boundaries, two tectonic plates slide horizontally past each other. The movement along these transform faults can cause rocks to break and grind against each other, resulting in the formation of valleys. The San Andreas Fault in California, USA, is an example of a transform boundary with associated mountain ranges and valleys.

It is important to note that the formation of valleys and mountain ranges is a complex and ongoing process that takes millions of years. The interactions between tectonic plates, erosion, and various natural forces shape the Earth's surface, ultimately leading to the creation of these landforms.