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In the study area, geologically, it should be thought the engineering bedrock is composed of Bornova melange and seismic bedrock unit is composed of Menderes massif.
Route 174 is located along a large mapped sedimentary bedrock unit, known as the Marcellus Formation.
NY 174 is located along a geological feature known as a mapped sedimentary bedrock unit, known as the Marcellus Formation.
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These units border isolated circular bedrock units described as second unit below.
Nonetheless, groundwater occurrence in the study area can be categorized under two main units: area with highly weathered and/or fractured bedrock units and area with poorly weathered/sparsely fractured bedrock units.
Based on observations on amplitude data in different polarization modes, we observe three different bedrock units (Figs. 2a d, 5).
Based on the available radar data products, it is not possible to distinguish different lithologies in the larger area but it is possible to clearly separate bedrock units from unconsolidated materials based on the respective radar backscatter with high radar reflectance for bedrock units and low reflectance for unconsolidated material.
Usually, massive unfractured lithologic units in Basement Complex setting has little influence on groundwater availability except in cases with secondary porosity through the development of weathered overburden and fractured bedrock units, which form potential groundwater zones.
Assessment of previous studies revealed that the hydrogeological setting of the study area is characterized by weathered saprolite units with varied thickness over the different bedrock units such as porphyritic granites, granite-gneiss, migmatite, pegmatite and quartz-schist settings.
Purple colors represent high (on a relative scale) radar reflectance in HH polarization, yellow colors show high reflectance values also in HV polarization indicating exposed bedrock units; center of impact structure located at 24°24′E, 24°34′N.
Variables included multiple level variables geologic provinces, lithochemistry (of bedrock units), and bedrock units (surficial geology)—as well as geochemical and geographic factors associated with the occurrence of arsenic in New England aquifers.
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