The drift-thickness map of Ohio depicts the thickness and distribution of glacially derived sediments (called drift) and post-glacial stream sediments overlying the buried bedrock surface. This map was produced by subtracting bedrock-surface elevations from land-surface elevations to produce a residual map of drift thickness. Colors portray thickness intervals of glacial and modern sediments, which can range up to several hundred feet.
The bedrock-surface component is one of the products resulting from a multiyear effort by the Ohio Department of Natural Resources, Division of Geological Survey, to map the bedrock geology of Ohio. Bedrock-topography maps are required to determine the relief on the bedrock surface beneath thick layers of glacial drift. These maps were created for all 788 7½-minute topographic quadrangles in the state as part of a process to produce accurate bedrock-geology maps for glaciated portions of Ohio and for those areas beyond the glacial boundary where valleys are infilled with sediment. Data concentration and contour intervals on the original, hand-drawn bedrock-topography maps vary widely across the state in response to changing geologic and topographic conditions. During the course of mapping, over 162,000 data points were interpreted for bedrock-surface elevation and in some cases drift thickness. These points were plotted on maps and used as control for the bedrock-topography lines.
Courtesy of Donovan Powers, Ohio Department of Natural Resources, Division of Geological Survey.
Map Book Page [PDF]
Donovan M. Powers and E. Mac Swinford
Columbus, Ohio, USA
ArcGIS Desktop, Adobe Photoshop, and Adobe Illustrator
HP Designjet 5500 ps (ultra violet ink)
Ohio Department of Natural Resources (Division of Geological Survey, Division of Water, Division of Mineral Resources Management), Ohio Department of Transportation, Ohio County Engineers, and U.S. Geological Survey