...the North, where it is not known to extend with certainty beyond the limits of the Chesapeake area. Within the State of Maryland the strata cover the...deposits of coarse gravel, through which is scattered a light colored sandy loam, the whole at times cemented by hydrous iron oxide into a more or less compact...

...stratified, and often change rapidly within narrow limits. Toward the ancient shore line the deposits are of coarse gravel, through which is scattered a light-colored sandy loam, the whole cemented at times by hydrous iron oxide into a more or less compact conglomerate. The eastward extension...

...stratified, and often change rapidly within narrow limits. Toward the ancient shore line the deposits are of coarse gravel, through which is scattered a light-colored sandy loam, the whole cemented at times by hydrous iron oxide into a more or less compact conglomerate. The eastward extension...

...stratified, and often change rapidly within narrow limits. Toward the ancient shore-line the deposits are of coarse gravel, through which is scattered a light-colored sandy loam, the whole cemented at times by hydrous iron oxide into a more or less compact conglomerate. The eastward extension...

...stratified and often change rapidly within narrow limits. Toward the ancient shore line the deposits are coarse gravel, through which is scattered a light-colored sandy loam, the whole cemented at times by hydrous iron oxide into a more or less compact conglomerate. The eastward extension...