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    Cape Cod's Sole Source Aquifer

     

    Physical Setting

    Geology of Cape Cod - StrahlerCape Cod is a sand and gravel remnant of the last continental deglaciation that occurred from 15,000 to 20,000 years ago. As shown at right, the Cape is a series of broad, gently sloping outwash plains that are truncated by long linear moraine deposits found along the present day Route 6/MidCape Highway and Route 28/MacArthur Boulevard. The glacial deposits are approximately 150 to 900 feet thick from Buzzards Bay to Provincetown. The glacial deposits are generally coarse to medium sand but grade to finer materials at depth. The coarse sands are extremely permeable, making for a high-yielding groundwater system.

     

    The groundwater of Cape Cod is bounded at the top by the water table, which is ubiquitous across the Cape -- a sharp transition zone between fresh and marine water at the shore and bedrock below. The groundwater system is recharged solely from precipitation, at a rate of 27 inches per year (approximately 60% of precipitation). 

     

    Cape Cod's Groundwater Flow Dynamics

    The groundwater system is in dynamic equilibrium between recharge and discharge to the surrounding marine waters and flows at approximately 1 foot per day due to gravity. Because groundwater located further inland has greater distances to travel to get to the shore, the accumulation of recharge over the ages mounds up. The mounds of groundwater are relatively thin and convex and therefore are referred to as "lenses" of groundwater. Six separate lenses comprise the Cape Cod aquifer system.

     

    water table

    The topographic lines of the aquifer, referred to as "water table contours," are used by hydrogeologists to plot the exact flow of groundwater. Over the years this effort has lead to the use of complex groundwater models to predict and answer many questions about how the aquifer responds to new stresses such as pumping and the discharge of wastewater.

    The Cape Cod Aquifer is extremely susceptible to contamination from various land uses and activities. The aquifer has been seriously impacted from military activities, gas stations, landfills, and a host of other activities. These examples have lead to multiple strategies to protect the aquifer at all levels of government and have spawned a vigorous industry for the assessment and clean-up of contaminated groundwater. The groundwater of Cape Cod is fairly well protected except for impacts from the prevalence of residential septic systems.

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