Mountain is created when two continental plates push together at a convergent boundary.
Mountains are created when lava pushes the crust upward but hardens before exploding onto the surface. The domes are battered by wind and rain, which sculpts peaks and valleys. Examples are the Adirondack Mountains in New York and the Black Hills in South Dakota. Similar to dome mountains, plateau mountains are created when tectonic plates collide and push the earth upward without folding or faulting. After then, wear and erosion form them.
When tectonic plate tensions cause the Earth's surface to split and fault, forcing rock blocks up and down, other kinds of mountains are created. The Sierra Nevada in California and Nevada, the Tetons in Wyoming, and the Harz Mountains in Germany are a few examples of fault-block mountains.
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