Sandstone, limestone, and conglomerate cobbles are found in a streambed in New York State where the surrounding bedrock is composed of shales and siltstones. The most likely explanation for the presence of these cobbles is that they were
weathered from the surrounding bedrock
formed when shale and siltstone bedrock were eroded
transported to this area from another region
metamorphosed from shale and siltstone
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Sandstone, limestone, and conglomerate cobbles are found in a streambed in New York State where the...
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