[2] Several processes can cause the floor of a depression to become more resistant to erosion than its surrounding slopes and uplands: A classic example of inverted relief is Table Mountain, Tuolumne County, California.
These Miocene lava flows filled this ancient river valley with a thick sequence of potassium-rich trachyandesite lavas that are significantly more resistant to erosion than the Mesozoic siltstone and other rock in which the valley was cut.
[5] Another example is Table Mountain, Cape Town, where the original high ridges of resistant quartzitic sandstone of the Cape Fold Belt were eroded away first, exposing less resistant rock, which eroded faster, leaving the original valley bottom at the top of the residual mountain.
[4] Inverted relief in the form of sinuous and meandering ridges, which are indicative of ancient, inverted fluvial channels, is argued to be evidence of water channels on the Martian surface in the past.
[6][7][8][2][9][10] An example is Miyamoto Crater, which was proposed in 2010 as a potential location to be searched for evidence of life on Mars.