ECONOMIC GEOLOGY OF THE TRIASSIC-JURASSIC AGE
HARTFORD FAILED-RIFT BASIN, SOUTHERN NEW
ENGLAND
ALTAMURA, R.J.1, Department of Geosciences, The
Pennsylvania State University, University Park, PA
16802
Earliest organized mining of rock of the Hartford basin was in 1689
for building stone. Redbeds (red and brown arkosic sandstones) were
excavated for use as dimension stone during the period from 1689 to
present with a heyday in the mid- to late 19th century. C.U. Shepard
in his 1837 economic geology survey of Connecticut, reported an
annual production of 500 tons of processed lime from a 30 - 45 cm
thick limestone beds in quarries located in marly shales of the Shuttle
Meadow Formation adjacent to the Talcott flow near the
Berlin/Southington, CT town lines. P.D. Krynine stratigraphically
correlated this limestone deposit with another in North Branford, CT
that was also excavated for lime. These limestone beds are up to 5-m
thick, and also occur at the base of the Shuttle Meadow Formation.
These beds are finely banded (0.5 - 3 cm), the bedding planes being
marked by an accumulation of mica flakes. At the type locality at the
Coe's quarry, the beds are 4-m thick. At least a portion of the unit has
recently been reinterpreted to be metasomatically altered basalt.
Tholeiitic basalt has been quarried in the basin for some time
for use as road metal and aggregate. Most of the production has been
from basalt that was excavated in the Hartford and Pomperaug basins.
Sedimentary and igneous rocks of the Newark Supergroup were
excavated for utilitarian commodities, such as building stone, lime,
and trap rock that were made available to a developing population.
Other economic deposits associated with the Hartford rift are
those classified as hydrothermal in origin. Recent work on the
Lantern Hill silicified fault near North Stonington, CT indicates that
faulting and hydrothermal fluid activity associated the rifting of
Pangea in southern New England began in the Middle Triassic prior to
deposition of the first Newark Supergroup sediments (i.e. the Late
Triassic New Haven Arkose) into the basin. These early normal faults
appear to have been dominated by hydrothermal fluids that contained
mostly dissolved silica. Several silicified zones similar to Lantern
Hill occur in the footwall of the eastern border fault (EBF) of the
Hartford rift and to the east, but not on the west side of the rift. The
Mesozoic quartz was excavated at Lantern Hill for use as filtration
medium and industrial sand. Typical annual sales of the quartz at
Lantern Hill were approximately 3 million dollars at the time of the
closing of the operation in 1994.
Later in the evolution of the rift basin, during the eruption of
flood basalts, copper was deposited in stratiform deposits in the
Shuttle Meadow Formation beneath the massive Holyoke Basalt.
Chalcopyrite and bornite were excavated here during colonial times at
copper mines near Simbury, Connecticut. Their origin has been
interpreted to have been associated with circulating fluids driven by
heat associated with emplacement of the Holyoke flow. Barite occurs
in veins that like the copper are inferred by many to have originated
from basaltic melts emplaced into the sedimentary stack. Copper was
mined in the 19th century along the western border of the rift near
Bristol, CT and along the EBF in Manchester, CT. Vein barite and
galena occur in many places in the basin, emplaced in redbeds and
basalts. Significant mining occurred in the 19th century at Loudville,
MA, where veins emplaced along border faults produced 12.5 ounces
of silver per ton of processed galena. Argentiferous galena was also
mined from veins along the EBF near Middletown, CT. Origin of
these hydrothermal deposits was apparently not associated with local
emplacement of basaltic melts and a basin-wide circulation system is
envisaged.
Exploration for oil had been conducted in the Pomperaug
basin around 1890, a drill hole was spudded in the Hartford basin near
the village of Forestville, CT, and in the mid-1980's Texaco ran
seismic traverses along and across the Hartford basin as part of a
modern exploratory program. It is not uncommon to find bitumen in
these rocks. Coal is reported to have been excavated in the 19th
century near the towns of Berlin and Windsor.
1Present Address: Dept. of Geology & Planetary Sciences, University
of Pittsburg, Johnstown, PA 15904
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