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(GP/GT) for Additional Water Supply in the Lower Rio Grande

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1-2<br />

1. <strong>GP</strong>/<strong>GT</strong> Fairways<br />

In<strong>for</strong>mation provided by Mr. R. W. Rodgers, Professor of Geology at U.T./Pan American,<br />

Ed<strong>in</strong>burg, Texas. The identity of each letter presented <strong>in</strong> this overlay is as below:<br />

A -<br />

B -<br />

C -<br />

D -<br />

Coastal Miocene Trend(<strong>in</strong>cludes prospective reservoirs studied under recent USDOE<br />

Contract No. 2069)<br />

<strong>Lower</strong>-Sal<strong>in</strong>ity Frio Trend<br />

Frio-Vicksburg Trend<br />

Vicksburg Trend<br />

Professor Rodgers has qualitatively ranked <strong>the</strong> overall potential of <strong>the</strong>se Fairways as shown<br />

below:<br />

Fairway<br />

A<br />

B<br />

C<br />

D<br />

Rank<strong>in</strong>i<br />

Medium<br />

Medium<br />

High<br />

Low<br />

2. Productive Zones of MUdly/Moderately Brackish Groundwater<br />

Most of <strong>the</strong> <strong>in</strong><strong>for</strong>mation ,utilized <strong>in</strong> this layer was obta<strong>in</strong>ed from Figures 5 and 12 of <strong>the</strong> TWDB<br />

Report No. 316 entitled: "Evaluation of Groundwater Resources <strong>in</strong> <strong>the</strong> <strong>Lower</strong> <strong>Rio</strong> <strong>Grande</strong> Valley,<br />

Texas" (1990). Figure 5 is entitled: "Approximate Productive Areas of The Major Sources of<br />

Groundwater <strong>in</strong> <strong>the</strong> <strong>Lower</strong> <strong>Rio</strong> <strong>Grande</strong> Valley" and Figure 12 is entitled: "Chemical Quality of<br />

<strong>Water</strong> <strong>in</strong> <strong>the</strong> Evangel<strong>in</strong>e and Chicot Aquifers". The approximate configuration of <strong>the</strong> 5,000<br />

mg/l.TDS contour l<strong>in</strong>e was taken from Figure 7 of <strong>the</strong> Texas Department of <strong>Water</strong> Resources<br />

Report No. 279, entitled: "Occurrence and Quality of Groundwater <strong>in</strong> <strong>the</strong> Vic<strong>in</strong>ity of<br />

Brownsville, Texas (1983)". Figure 7 is entitled: "Dissolved Solids Concentration <strong>in</strong> <strong>Water</strong> from<br />

The Deep Zone". Copies of several of <strong>the</strong>se Figures are enclosed <strong>in</strong> this Report.<br />

The identity of each number presented <strong>in</strong> this overlay is as follows:<br />

(1) - Upper Part of Chicot Aquifer: Alluvial Deposits of <strong>the</strong> <strong>Rio</strong> <strong>Grande</strong> (Recent and<br />

Pleistocene)<br />

(2) ~ Middle Part of Chicot Aquifer: Beaumont Formation (pleistocene)<br />

(3) - <strong>Lower</strong> Part of Chico Aquifer and Evangel<strong>in</strong>e Aquifer: Lissie Formation (pleistocene) and<br />

Goliad Formation (pliocene)<br />

(4) - Oakville Sandstone(Miocene).<br />

3. Population Densities<br />

Base Maps of Cameron and Hidalgo Counties were utilized to represent <strong>the</strong> population densities<br />

of both <strong>in</strong>corporated and Colonia areas of each county. It is our understand<strong>in</strong>g that <strong>the</strong>se maps<br />

were <strong>the</strong> basis <strong>for</strong> <strong>the</strong> <strong>in</strong><strong>for</strong>mation <strong>in</strong> <strong>the</strong> TWDB Report entitled: "<strong>Water</strong> and Wastewater <strong>for</strong> <strong>the</strong><br />

Colonias of <strong>the</strong> <strong>Lower</strong> <strong>Rio</strong> <strong>Grande</strong> Valley of Texas"

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