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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Western The <strong>County</strong><br />
Toward <strong>the</strong> western part <strong>of</strong> <strong>the</strong> county is <strong>the</strong> band <strong>of</strong> glacial deposits lying within <strong>the</strong> Long Valley region.<br />
This aquifer system is an important source <strong>of</strong> ground water in a region which is steadily increasing its demand.<br />
6<br />
A recently published study investigated <strong>the</strong>se valley-fill aquifers and <strong>the</strong> underlying carbonate-rock spanning<br />
<strong>the</strong> valleys <strong>of</strong> <strong>the</strong> Lamington River, Rockaway River, Green Pond Brook, Drakes Brook, and South Branch<br />
<strong>of</strong> <strong>the</strong> Raritan River.<br />
The Lamington River Valley (Figure 5) stretching from Picatinny Arsenal southwardly to Califon (Hunterdon<br />
<strong>County</strong>) contains confining clay layers remnant from glacial Lake Succasunna. These impermeable deposits<br />
separate <strong>the</strong> confined aquifer from <strong>the</strong> unconfined aquifer present in <strong>the</strong> valleys.<br />
The underlying carbonate-rock aquifer is <strong>of</strong> <strong>the</strong> Leithsville Formation. Its varied water supply capability is<br />
linked to enhanced secondary porosity caused by wea<strong>the</strong>ring and resultant solution opening <strong>of</strong> primary<br />
fractures, joints, or bedding planes. Productive wells have been located in <strong>the</strong> valleys <strong>of</strong> Drakes Brook, <strong>the</strong><br />
South Branch Raritan River and<br />
<strong>the</strong> Lamington River. Where<br />
Hardyston Quartzite underlies<br />
<strong>the</strong> carbonate-rock aquifer,<br />
supply is mainly appropriate<br />
<strong>for</strong> domestic use.<br />
In <strong>the</strong> nor<strong>the</strong>rn parts <strong>of</strong> <strong>the</strong> study<br />
area <strong>the</strong> Green Pond<br />
Conglomerate aquifer overlies<br />
<strong>the</strong> carbonate-rock aquifer.<br />
O<strong>the</strong>r than in low-lying areas,<br />
this aquifer does not produce<br />
significant amounts <strong>of</strong> water.<br />
The valley fill deposits, however,<br />
are more permeable and<br />
productive than those to <strong>the</strong><br />
south.<br />
Areas relying on water supply<br />
from Precambrian crystalline<br />
rocks benefit from intersecting<br />
fractures, especially those<br />
wea<strong>the</strong>red-induced.Yields<br />
generally are small but are<br />
adequate <strong>for</strong> domestic supply.<br />
Source: U.S.G.S., Water-<strong>Resource</strong>s<br />
Investigations Report 93-4157, 1996.<br />
Figure 5 - Lamington River Valley<br />
6<br />
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A <strong>Natural</strong> <strong>Resource</strong> <strong>Management</strong> <strong>Guide</strong><br />
<strong>for</strong> <strong>the</strong> <strong>County</strong> <strong>of</strong> <strong>Morris</strong> 63