0 N ↑ Assignment: Use the potentiometric data for the wells (circles, height in fet above an arbitrary datum such as sea level) to contour the groundwater surface. Draw arrows showing the direction of regional groundwater flow based on this potentiometric map. Note the red dashed line is the concentration of total dissolved solids. Blanco 300 Kilometers 1 1 500 390 1 TEXAS Map Area 390 1000- O 360 Blanco River 400 355 O Gulf of Mexico 340 PVS 342 315 327 325 Canyon Lake 326 3170 310 333 345 5 Kilometers Dripping Springs 370 Jacobs Well 320 290 10 321 278 275 Wünberley O250 Barton Creek 265 282 1000 240 220 San Marcos Springs Colorado River 240 220 240 220 200 O220 190 O 170 180 Buda AUSTIN Barton 160Spring Saline Edwards Aquifer Zone -180- Edwards Pot. Surface (m-msl) -300- Trinity Pot. Surface (m-msl <-500- Total Dis- solved Solids (mg/l) Spring Edwards Aquifer u-unconfined C=confined Trinity Aquifer (undívided)
0 N ↑ Assignment: Use the potentiometric data for the wells (circles, height in fet above an arbitrary datum such as sea level) to contour the groundwater surface. Draw arrows showing the direction of regional groundwater flow based on this potentiometric map. Note the red dashed line is the concentration of total dissolved solids. Blanco 300 Kilometers 1 1 500 390 1 TEXAS Map Area 390 1000- O 360 Blanco River 400 355 O Gulf of Mexico 340 PVS 342 315 327 325 Canyon Lake 326 3170 310 333 345 5 Kilometers Dripping Springs 370 Jacobs Well 320 290 10 321 278 275 Wünberley O250 Barton Creek 265 282 1000 240 220 San Marcos Springs Colorado River 240 220 240 220 200 O220 190 O 170 180 Buda AUSTIN Barton 160Spring Saline Edwards Aquifer Zone -180- Edwards Pot. Surface (m-msl) -300- Trinity Pot. Surface (m-msl <-500- Total Dis- solved Solids (mg/l) Spring Edwards Aquifer u-unconfined C=confined Trinity Aquifer (undívided)
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
Section: Chapter Questions
Problem 1LR
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Question
From the given potentiometric map, it is very much clear that the groundwater in general flows from west to east as the discharge area is in the east and also the elevations of potentiometric surfaces of different wells tend to decrease from west to east side of the map. So you should draw arrows along the potentiometric data for wells (identified by circles on the map) showing eastward direction to describe the overall trend of regional groundwater flow.
can you draw it for me?
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