Volcanic Mountains: These are formed through the accumulation of volcanic material, such as lava and ash, from volcanic eruptions. Examples include Mount St. Helens and Mount Fuji.
Block Mountains: These are created when large blocks of the Earth'scrust are uplifted and tilted along faults. The Sierra Nevada mountains are an example of block mountains.
Continental Collision: When two continental plates collide, the crust is compressed and folded, leading to the formation of large fold mountains.
Uplift and Erosion: The uplift of large regions of the Earth'scrust, followed by erosion, can result in the formation of mountain ranges over millions of years.
Study Guide
Here are some key points to remember when studying mountain building:
Understand the different types of mountains and the processes that lead to their formation.
Plan and conduct an investigation to gather evidence to compare the structure of substances at the bulk scale to infer the strength of electrical forces between particles.