* Near ancient or modern riverbeds: Sandstone is formed from the accumulation of sand grains, which rivers often carry and deposit.
* Beaches: Beaches are another common location for sand deposition, leading to the formation of sandstone.
* Deserts: Deserts are often windswept, with sand dunes that can eventually solidify into sandstone.
* Ancient lake beds: Lakes can also accumulate sediment, including sand, which can harden into sandstone over time.
* Coastal areas: Coastal areas are exposed to both water and wind, making them ideal for the formation of sandstone.
In general, sandstone forms in environments where sand is transported and deposited by wind or water.
