Approximate Ground-water-level Contours, April 1981, for the Soquel-Aptos Area, Santa Cruz County, California PDF Download

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Approximate Ground-water-level Contours, April 1981, for the Soquel-Aptos Area, Santa Cruz County, California

Approximate Ground-water-level Contours, April 1981, for the Soquel-Aptos Area, Santa Cruz County, California PDF Author: Richard M. Bloyd
Publisher:
ISBN:
Category : Groundwater
Languages : en
Pages : 18

Book Description
Ground-water levels in selected wells were measured in the Soquel-Aptos, Calif., area in April 1981. On the basis of these measurements approximate ground-water-level contours were constructed. The general direction of ground-water movement in the Soquell-Aptos area is from the ridges in the northern part of the area, toward the adjacent canyons, and then southward toward the ocean. Ground-water pumping has caused ground-water levels to decline below sea level in the Capitola area, in the area just to the west and northwest of aptos, and in isolated local areas southwest of Rio Del Mar. Ground-water levels in the northern part of the area away from the seacoast have not declined much over time.

Approximate Ground-water-level Contours, April 1981, for the Soquel-Aptos Area, Santa Cruz County, California

Approximate Ground-water-level Contours, April 1981, for the Soquel-Aptos Area, Santa Cruz County, California PDF Author: Richard M. Bloyd
Publisher:
ISBN:
Category : Groundwater
Languages : en
Pages : 18

Book Description
Ground-water levels in selected wells were measured in the Soquel-Aptos, Calif., area in April 1981. On the basis of these measurements approximate ground-water-level contours were constructed. The general direction of ground-water movement in the Soquell-Aptos area is from the ridges in the northern part of the area, toward the adjacent canyons, and then southward toward the ocean. Ground-water pumping has caused ground-water levels to decline below sea level in the Capitola area, in the area just to the west and northwest of aptos, and in isolated local areas southwest of Rio Del Mar. Ground-water levels in the northern part of the area away from the seacoast have not declined much over time.

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