Mountains:
* Major Mountain Ranges: These are the most prominent, often reaching thousands of feet. Examples include the Himalayas, the Andes, the Rockies, and the Alps.
* Isolated Peaks: These are single mountains that stand alone, often formed by volcanic activity or tectonic uplift. Examples include Mount Fuji in Japan, Mount Kilimanjaro in Tanzania, and Mount Shasta in California.
* Hills: These are smaller than mountains but still rise significantly above their surroundings. Often, hills are formed by erosion, folding, or faulting of the Earth's crust.
Plateaus:
* Tablelands: These are broad, flat-topped areas that are elevated above their surroundings. They are often formed by volcanic activity or by erosion of uplifted areas.
* Mesa: These are smaller than tablelands, with a flat top and steep sides. Often formed by erosion of sedimentary rock.
* Butte: These are even smaller than mesas, with a steep, often conical shape. They are usually formed by erosion of resistant rock.
Other Landforms:
* Volcanoes: These are conical landforms formed by the eruption of lava and ash. Some volcanoes can reach heights of thousands of feet.
* Canyons: These are deep, narrow valleys that are often carved by rivers. Some canyons can be hundreds or even thousands of feet deep.
* Escarpments: These are steep cliffs or slopes that mark a change in elevation. They can be formed by faulting, erosion, or volcanic activity.
Important Note: The exact definition of what constitutes a "peak" above 200 feet can vary depending on the context. Some sources may use different elevation thresholds.
