Oriskany Sandstone is a geological formation primarily found in the northeastern United States, particularly in New York and Pennsylvania. It dates back to the Devonian Period, around 400 million years ago, and is known for its fine to medium-grained texture. This sandstone is primarily composed of quartz and is often characterized by its light color, ranging from white to yellowish. The formation is significant for its role in natural resource extraction, particularly in the production of natural gas and oil. Additionally, the Oriskany Sandstone serves as an important aquifer, providing groundwater in various regions. Its unique properties make it a subject of interest for geologists and environmental scientists.