Thermal Stress Anisotropy governs how erosion and the resulting rocks deposits are shaped. It smooths the terrain while eroding. Low values keep the original terrain intact for the most part, while high values create stronger talus at the expense of eroding the original terrain. For example, sharp peaks get eroded heavily with high stress values.
The image below shows a simplified version of how Thermal Stress Anisotropy affects a terrain.
|Duration||Duration of the thermal erosion process.|
|Strength||Strength of the thermal erosion process.|
|Anisotropy||Thermal erosion's anisotropy that affects how rock is affected, and deposits formed. See the Anisotropy section for details.|
|Talus Angle||Angle of the talus (deposits).|
|Talus Settling||Settling of sediments in the talus.|
|Fine Detail||Enable rocky debris in the talus.|
|Debris Size||Size of the rocky debris in the talus. Available when Fine Detail is turned On|
|Real Scale||Use the scale defined in the terrain. Disable to access addtional options and modify erosion's physics.|
|Terrain Scale||Scale of the terrain. Available when Real Scale is turned Off|
|Feature Scale||Scale of the largest feature in the terrain.|
|Verticality||Height of the terrain.Available when Real Scale is turned Off|