A Natural Resource Management Guide for the County of Morris A ...
A Natural Resource Management Guide for the County of Morris A ...
A Natural Resource Management Guide for the County of Morris A ...
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Geologic History <strong>of</strong> <strong>Morris</strong> <strong>County</strong><br />
Introduction<br />
This inventory <strong>of</strong> <strong>Morris</strong> <strong>County</strong>'s environmental features begins with geology because, indeed, it describes<br />
<strong>the</strong> substrate upon which subsequent layers <strong>of</strong> soil, water, vegetation, wildlife habitat and microclimates have<br />
evolved. An understanding <strong>of</strong> geologic history contributes to an understanding <strong>of</strong> human settlement patterns,<br />
transportation routes, and <strong>the</strong> location <strong>of</strong> certain economic activities. Current application <strong>of</strong> this<br />
understanding can be made in rectifying and preventing <strong>the</strong> problems associated with <strong>the</strong>se assorted land uses,<br />
e.g., depleted aquifers, mine shaft-related cave-ins, sinkholes, and radon hot spots.<br />
Ancient History<br />
The processes that produced <strong>the</strong> geologic structures underlying <strong>Morris</strong> <strong>County</strong> have been operating <strong>for</strong> over<br />
one billion years. The landscape that we see is <strong>the</strong> result <strong>of</strong> cyclical mountain building, erosion, rock relocation<br />
into valleys, metamorphosis, and recycled rock being thrust up into mountains again.<br />
Primitive rivers carved channels in <strong>the</strong> rock, <strong>for</strong>ming deep valleys, only to have <strong>the</strong>ir direction reversed in<br />
response to <strong>the</strong> changing tilt <strong>of</strong> <strong>the</strong> land mass or <strong>the</strong> blockage <strong>of</strong> old drainage ways by erosional deposition.<br />
Seas have advanced across <strong>the</strong> land surface, and <strong>the</strong>n retreated. The climate has changed from tropical to<br />
arctic and back to temperate as <strong>the</strong> landmass itself has drifted nearer <strong>the</strong>n far<strong>the</strong>r from <strong>the</strong> equator. Glaciers<br />
have descended from <strong>the</strong> north, covered more than half <strong>the</strong> county, and <strong>the</strong>n melted back; <strong>the</strong>ir passage<br />
radically reshaping <strong>the</strong> landscape and trapping <strong>the</strong> groundwater that serves us today.<br />
Geologic history is traditionally divided according to <strong>the</strong> duration <strong>of</strong> time needed to <strong>for</strong>m recognizable rock<br />
units. The longest such division is commonly known as an Era. Eras are <strong>the</strong>n subdivided into Periods.<br />
Periods may be fur<strong>the</strong>r subdivided into Epochs. Table 1, on <strong>the</strong> following page, provides an overview <strong>of</strong> this<br />
chronology. As you continue to read, refer to <strong>the</strong> corresponding <strong>for</strong>mations depicted on <strong>the</strong> bedrock geology<br />
map Plate 1. The variations within this geologic base have contributed to <strong>the</strong> environmental diversity specific<br />
to <strong>the</strong> county.<br />
9<br />
Geologic History <strong>of</strong> <strong>Morris</strong> <strong>County</strong>