They are best formed in dry climates.
Dry Climate
mechanical weathering
by my sharp turds
the sharp rocks and high cliffs.
one animal is the moantain goat.another would be a bobcat :p
the sharp rocks and high cliffs
Glaciers that feature steep cliffs are often found in mountainous regions, particularly in areas like the Himalayas, the Andes, and the Alps. These steep cliffs, known as ice cliffs or seracs, are formed by the dynamic processes of glacial movement and melting. As glaciers flow down valleys, they can carve out sharp ridges and steep faces, creating dramatic landscapes. Notable examples include the Greenland Ice Sheet and the Patagonian Ice Field, where towering ice formations can be observed.
== == No, some rocks are quite dull from weathering processes.
Yes, horn peaks are typically characterized by steep cliffs. They are formed through glacial erosion, which shapes their distinctive sharp, pointed summits and steep sides. These features are often found in mountainous regions where glacial activity has significantly influenced the landscape. Horn peaks are visually striking and often attract climbers and hikers.
Weathering tends to attack the outermost layer of a rock, known as the rock surface or rind, most rapidly. This layer is more exposed to the elements and is therefore more susceptible to weathering processes such as erosion, chemical weathering, and physical weathering.
---- Land forms can be made by many different forces in nature. Land forms like sand dunes are formed by wind. sharp rocks are formed by water eroding them making them sharp. Land forms can also form by weathering. Weathering is were water seeps into rock and the water freezes making the rock expand and crack. Roots can also cause weathering by roots from plants growing into rock and making the rock crack and split. ----
Before weathering, the landscape likely featured rugged, sharp-edged rock formations, with steep cliffs and minimal soil cover. It would have been characterized by a lack of vegetation, exposing bare rock and gravel surfaces, and water bodies might have been more confined. Over time, weathering processes would have softened these features, creating smoother contours and allowing soil and plant life to develop.