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Stratigraphic Test Well, Nantucket Island, Massachusetts.

机译:地层测试井,马萨诸塞州南塔克特岛。

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The U.S. Geological Survey, in cooperation with the Massachusetts Water Resources Commission and the Nantucket Conservation Foundation, continuously cored 514 m of sediment and volcanic rock in a Stratigraphic and Water-Quality Test. Stratified sediments were divided texturally into three zones: the upper zone (0-128 m) contains mostly coarse sand and gravel; the middle zone (128-349 m)contains mostly silty clay and a few beds of sand and silt; and the lower zone (349-457 m) contains soft, unconsolidated, clayey sand. Below the lower zone, as a polite, composed mostly of clay, grades abruptly downward at 470 m into partially altered basalt that extends to the bottom of the hole at 514 m. Fossils are sparse throughout the cores, but Pleistocene, Eocene, and Upper Cretaceous assemblages were identified.

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