Publisher's Synopsis
Excerpt from Brachiopoda and Lamellibranchiata of the Raritan Clays and Greensand Marls of New Jersey
The outcropping edge of these formations is thin, so that in many places the underlying red sandstone is exposed in the inequalities Of the surface, or is easily reached in digging. This, of course, must leave the edge somewhat irregular, and in one place in Middlesex County, north of the Raritan, the red sandstone rises in a considerable hill south Of this line, and is entirely surrounded by the white clays Of this later formation.
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