Geology
Great Baddow lies to the south east to central Chelmsford, on higher ground that is thought to mark the edge of the main ice mass during the Anglian glaciation. An outcrop of glacial sand and gravel 3 km long and 0.8 km wide is located beneath the village, which used to be extracted from several pits in the area, including Beehive Pit (now beneath Harbeard Tye), Baddow Hall Pit (now beneath Baden-Powell Close), to the south of the A1114 Princes Road (now in the grounds of Moulsham High School) and on what is now an area of open land off Waterson Vale. Smaller pits were also located off the Galleywood Road (near what is now Hollywood Close) and off Pitt Chase. The area is overlain with head, while the lower levels of the sand and gravel are mixed with London Clay. A Sarsen stone from the Beehive Pit used to stand outside The Beehive pub.
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