The majority of buildings in the area are houses from the 20th century, but there are a few buildings, landmarks, and objects that date from the 16th century, in addition to Bramall Hall which dates from the 14th century. In particular, there are many Victorian buildings in several places across the area. The local drift geology is mostly glacial boulder clay, as well as glacial sands and gravel. For many years the clay has been used for making bricks and tiles.