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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Middle<br />
Proterozoic<br />
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c<br />
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p<br />
Upper<br />
Ordovician<br />
Middle<br />
Ordovician<br />
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w m<br />
o a<br />
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p<br />
K<br />
ita<br />
Rickenbach<br />
Dolomite<br />
Ju<br />
tla<br />
(n<br />
o<br />
t<br />
dolomite<br />
sandy<br />
(Rickenbach)<br />
limestone,<br />
shale,<br />
(Jutland)<br />
chert<br />
quartzite, conglomerate<br />
arkosic<br />
(Hardyston)<br />
metasedimentary rocks including <strong>the</strong><br />
quartz<strong>of</strong>eldspathic and calcareous<br />
sodic gneissic and granitoid<br />
highly<br />
amphibolite<br />
rocks;<br />
water occurs along<br />
Ground<br />
surfaces, joints, faults,<br />
bedding<br />
cavities, intergranular<br />
solution<br />
and o<strong>the</strong>r openings<br />
spaces,<br />
water occurs in joints,<br />
Ground<br />
foliation surfaces, solution<br />
faults,<br />
and o<strong>the</strong>r openings.<br />
cavities,<br />
Precambrian rocks are<br />
“The<br />
unproductive aquifers<br />
generally<br />
where <strong>the</strong>y are fractured<br />
except<br />
wea<strong>the</strong>red. The more<br />
or<br />
aquifers <strong>of</strong> <strong>the</strong><br />
productive<br />
are <strong>the</strong> glacial deposits<br />
Highlands<br />
some <strong>of</strong> <strong>the</strong> Paleozoic<br />
and<br />
Table One - Proterozoic and Paleozoic Rock in <strong>Morris</strong> <strong>County</strong><br />
h<br />
d<br />
Hydrogeologic<br />
Predominant Lithology<br />
a<br />
Stratigraphic Unit<br />
Characteristics<br />
slate, siltstone, graywacke<br />
Martinsburg Formation<br />
limestone,<br />
Jacksonburg Limestone<br />
argillaceous<br />
)<br />
limestone<br />
p<br />
u<br />
ic<br />
o<br />
v<br />
r<br />
o<br />
g<br />
r<br />
dolomite,<br />
e<br />
p<br />
u<br />
ia<br />
n<br />
ic<br />
v<br />
r<br />
d<br />
o<br />
S<br />
Ontelaunee limestone<br />
y<br />
, n<br />
Formation<br />
(Ontelaunee,<br />
tin Epler)<br />
its<br />
n<br />
ita<br />
u<br />
e K<br />
Epler<br />
p f<br />
lip o<br />
Formation<br />
k r<br />
t<br />
a<br />
p d<br />
n<br />
eekmantownGroup B p<br />
u<br />
o<br />
r<br />
g<br />
r<br />
e<br />
ic<br />
tin<br />
n<br />
y<br />
n<br />
r<br />
e<br />
dolomite, calcareous sandstone<br />
p<br />
Allentown Dolomite<br />
n<br />
n<br />
Leithsville Formation<br />
dolomite, calcareous shale<br />
n<br />
e<br />
r<br />
Hardyston Quartzite<br />
granite, quartz syenite, syenite,<br />
Byram Intrusive Suite, Lake Hopatcong Intrusive<br />
quartz monzonite, monzonite, and<br />
Suite,<br />
granodiorite<br />
Mount Eve Granite<br />
Metasedimentary rocks<br />
Franklin and Wildcat Marbles<br />
Losee Metamorphic Suite<br />
sedimentary rocks.”*<br />
Sources: New Jersey Geological Survey, In<strong>for</strong>mation Circular 1, 1990;<br />
*NJGS, Geologic Map <strong>of</strong> NJ, 1984.<br />
53<br />
Ground Water