Kensworth Chalk Pit, Geological Site of Special Scientific Interest in Kensworth, England
Kensworth Chalk Pit is a chalk quarry in Bedfordshire that contains expansive white mineral deposits and steep cliff faces throughout the site. The exposed walls reveal multiple geological layers that span millions of years of Earth's history.
Extraction operations at this location began several centuries ago, extracting chalk for construction and industrial use that shaped the local landscape. This long-term quarrying activity exposed deep subsurface layers and defined the region's geography.
Local educational institutions conduct field studies at this location to teach students about geological formations, fossilization processes, and environmental changes over time.
The site is not open to the public as it remains an active quarry operation. Access requires special permission for research or educational visits, arranged directly with the responsible authorities.
The location serves as the stratotype for the Kensworth Nodular Chalk Member, making it a reference point for studying Upper Cretaceous formations. This scientific designation makes it a key location for geologists researching rocks from this particular time period.
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