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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

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