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2. Three formations, each 25 m thick, overlie one another. Constant velocity vertical flow occurs across the formations with h = 120 m at the top, and h = 100 m at the bottom. Calculate h at the two internal boundaries. The values of K are 1 x 104 m/s for the top unit, 5 x 104 m/s for the middle, and 1 x 103 m/s for the bottom unit.

2. Three formations, each 25 m thick, overlie one another. Constant velocity vertical flow occurs across the formations with h = 120 m at the top, and h = 100 m at the bottom. Calculate h at the two internal boundaries. The values of K are 1 x 104 m/s for the top unit, 5 x 104 m/s for the middle, and 1 x 103 m/s for the bottom unit.

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
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2. Three formations, each 25 m thick, overlie one another. Constant velocity vertical flow occurs across the formations with h = 120 m at the top, and h = 100 m at the bottom. Calculate h at the two internal boundaries. The values of K are 1 x 104 m/s for the top unit, 5 x 104 m/s for the middle, and 1 x 103 m/s for the bottom unit.
Transcribed Image Text:2. Three formations, each 25 m thick, overlie one another. Constant velocity vertical flow occurs across the formations with h = 120 m at the top, and h = 100 m at the bottom. Calculate h at the two internal boundaries. The values of K are 1 x 104 m/s for the top unit, 5 x 104 m/s for the middle, and 1 x 103 m/s for the bottom unit.
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