they are formed by volcanic processes that give rise to a rock resistant to erosion
Valleys, escarpments, gorges, inselbergs, caves.
Inselbergs are steep sided hills that rise above a surrounding relatively flat plain. They appear to form because the rock making up the inselberg is more resistant to erosion than the rocks that once made up the surrounding plain.
inselbergs
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An inselberg is an isolated hill or mountain that rises abruptly from a flat surrounding plain, typically composed of hard rock that is more resistant to weathering and erosion than the surrounding rock. Inselbergs are commonly found in arid and semi-arid regions.
These are called inselbergs, which are isolated rock hills or small mountains that rise abruptly from a flat surrounding landscape. They are typically formed through the differential weathering and erosion of the surrounding softer rocks.
Warm and wet conditions in tropical regions favor the development of deep weathering. The combination of high temperatures and abundant rainfall accelerates chemical weathering processes, leading to the breakdown of rocks over time. Additionally, the presence of vegetation can enhance weathering through root action and organic acid release.
Inselbergs in the desert are formed through a process called differential weathering, where softer surrounding rock erodes over time, leaving behind a more resistant rocky outcrop. These rocky outcrops then become exposed due to further erosion from wind and water, creating the characteristic isolated hill-like formations seen in desert landscapes.
The main difference between etchplanation and pediplanation is at the second stage of their granite weathering processes. At the second stage of the etchplanation weathering process, exhumation occurs downwards, weathering granite vertically - resulting in steep sided granite landforms such as inselbergs or tors. For the pediplanation process however, exhumation occurs laterally, forming usually broad and gently sloping land surfaces. Accompanying the pediplanation process are usually river erosion processes, thus further widening the valley and even forming extensive plains (pediplanes).
Australia is a vast continent with a huge range of different types of territory. As an island continent, it has many beaches. Along the eastern coast is the Great Dividing Range, which extends from the far north down to Victoria, ending in the west of Victoria. In the southeast, this range features Australia's highest point, Mt Kosciuszko, among the Australian Alps, which feature significant snowfalls in winter. There is a great variety of forests, bushland, rainforests, deserts, mountains and plains. Even the deserts vary from gibber plains to sandy deserts to arid ats of land dotted with saltbush and bluebush. Inland Australia is very dry, mostly flat, and characterised by salt lakes, some of which are below sea level. Some mountains - inselbergs as well as mountain ranges - rise up from the desert plains, and these are mostly treeless.
essentially there are 2 disticnt typessubdivided into 5 catergories ; of desert according to the landscapes :Sand desert --- a wavy sand sea Stony desert --- gravel surfaces Rock desert--- bare rock surfaces with huge pavement that kept clear of sand or gravel by wind Plateau desert --- rocky plateaux , deeply eroded wadis, buttes or inselbergs (for details, please refer to Action of Rain) Mountain desert--- bare and arid arrays of jagged rock peaks ( The above landscapes can be found quite close to each other, like the desert complex in North America )Clarification:Science classifies deserts as either hot(Sahara, Mojave) or cold (Atacama, Antartica). Either desert may exhibit the landforms mentioned in the previous answer.