Fossils are typically formed in environments with sedimentation, which means that the remains of an organism are covered by layers of sediment (like sand, mud, or volcanic ash). Dry places often lack this continuous deposition of sediment.

While fossils can form in dry environments under specific conditions, there isn't a specific term for the process in dry places. Here's why:

* Dry environments often lack the necessary conditions for fossilization. Rapid decomposition, erosion by wind and water, and lack of burial all contribute to the difficulty of fossilization in deserts and other arid regions.

* If fossils are found in dry environments, they likely formed in a different location. They might have been transported by water or wind to their final resting place after being buried in a wetter environment.

Here's what *can* happen in dry environments:

* Mummification: In exceptionally dry conditions, the remains of an organism can dehydrate rapidly and be preserved through a process called mummification. This is more common for soft tissues than bones.

* Trace fossils: Footprints, burrows, and other traces of an organism's activity can be preserved in dry environments, especially if they are filled with sediment and protected from erosion.

So, while there isn't a specific term for fossil formation in dry places, we can say that fossilization is less likely in these environments due to the lack of the necessary conditions.