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RI0012D. Geology of the Blacklands Experimental Watershed, Near Waco, Texas - Downloadable PDF

RI0012D

RI0012D. Geology of the Blacklands Experimental Watershed Near Waco, Texas, by H. R. Blank, N. L. Stoltenberg, and H. H. Emmerich. 46 p., 1 figure, 4 plates, 1 map, 1952. doi.org/10.23867/RI0012D. Downloadable PDF. To purchase this publication in book format, please order RI0012.

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RI0012D. Geology of the Blacklands Experimental Watershed Near Waco, Texas, by H. R. Blank, N. L. Stoltenberg, and H. H. Emmerich. 46 p., 1 figure, 4 plates, 1 map, 1952. doi.org/10.23867/RI0012D. Downloadable PDF.

To purchase this publication in book format, please order RI0012.


ABSTRACT
The Blacklands Experimental Watershed, a hydrologic research project of the Soil Conservation Service located about 15 miles southeast of Waco, Texas, is underlain by marls and chalks belonging to the Taylor group of the Gulf series of the Cretaceous system, which, in conformity with the general structure of the Gulf Coastal Plain, dip east-southeastward at an angle a little steeper than the general slope of the land surface.


The lowest strata cropping out in the experimental watershed are part of the Wolfe City member of the Taylor marl and consist of about 110 feet of sandy marl containing numerous small lenses of hard calcareous sandstone. They are transitional upward into about 40 feet of silty marl, in which the sand or silt is too fine to be visible to the unaided eye.


Overlying the silty marl is a stratum of hard chalk, 8 to 25 feet thick, belonging to the Pecan Gap member of the Taylor marl. There is some evidence that the chalk—silty marl contact is an unconformity. This contact is the only easily identified stratigraphic marker in the experimental area. The chalk is hard enough to have some effect on the topography and the soil depth and brittle enough to influence greatly the distribution of the ground water.


The chalk is transitional upward into 90 to 100 feet of highly calcareous marl. Near the southeast corner of the experimental area this marl grades upward into another zone of about 13 feet of soft chalk, which in turn passes transitionally upward into additional highly calcareous marl. Remnants of an upland gravel, consisting merely of pebbles and cobbles scattered in the soil, occur on a few of the hilltops in the southwest corner of the experimental area and probably belong to the Uvalde (Pliocene?) formation. The valleys of Brushy Creek and its principal tributaries are partly filled with terrace alluvium consisting entirely of transported marl mixed with sand and pebbles and believed to be Pleistocene in age. Near the present stream channels there are also deposits of Recent alluvium consisting chiefly of transported soil.


Partial chemical analyses and mechanical analyses of the acid-insoluble residues bring out some of the differences between the Wolfe City, Pecan Gap, and alluvial formations, as well as differences between the oxidized and unweathered rocks. The intimate relation between the rocks and the distribution of the soil series is discussed.


The boundary between the Pecan Gap lower chalk and the Wolfe City silty marl is traced from Big Creek near Mart through the experimental watershed to Brazos River southwest of Marlin. It is shown that most of the chalk outcrops in this region described by other investigators correspond to the less definite upper chalk rather than to this lower zone. The Pecan Gap belt of outcrop as shown on the [U.S. Geological Survey’s 1937] geologic map of Texas (Darton et al., 1937) is too narrow and too far east to include both these chalks. At some places it has been based on the lower zone, at others on the upper.


Keywords: Blacklands Experimental Watershed, chalk, marl, Pecan Gap formation, Texas, Waco area, Wolfe City formation


CONTENTS

Abstract

Introduction

     Location and history

     Acknowledgments

General features of the experimental watershed

     Climate and agriculture

     Geology

     Topography
     Drainage

Rocks of the experimental watershed
     Areal distribution of the geologic units

     Wolfe City member of Taylor marl
         Divisions
         Sandy marl
         Silty marl

     Pecan Gap member of Taylor marl
           Lower chalk

           Lower highly calcareous marl

           Upper chalk

           Upper highly calcareous marl

     Alluvial and colluvial deposits

           Classification

          Upland gravel (Uvalde formation)

           Terraces of the Brazos River

           Terrace alluvium along Brushy Creek and adjacent streams

           Recent alluvium

     Decayed rock and soils

           Decay of the rocks

           Relation between parent rocks and soils

           Concretions and similar bodies
     Analytical data

     Structural features

Pecan Gap chalks in the adjacent regions


References

Appendix

     Well data

         Hole 694

         Hole 1000

         Hole 1010

         Hole 1011

         Hole 1012

         Hole 1020

Index

FIGURE
1. Index map of Texas showing location of the Blacklands Experimental Watershed



PLATES

I. Geologic map of Blacklands Experimental Watershed, near Waco, Texas
II. Boundary between Pecan Gap and Wolfe City formations in parts of McLennan and Falls counties, Texas
III. Contact of Pecan Gap chalk with Wolfe City silty marl, showing soft white calcium carbonate leached from the chalk and deposited in crevices in the marl
IV. Contact of Pecan Gap chalk with Wolfe City silty marl. Chalk overlain by alluvium


TABLES

1. Geologic units at the Blacklands Experimental Watershed
2. Description of samples analyzed
3. Partial chemical analyses of rock materials
4. Mechanical analyses of insoluble residues from acid treatment of rock materials


Citation
Blank, H. R., Stoltenberg, N. L., and Emmerich, H. H., 1952, Geology of the Blacklands Experimental Watershed Near Waco, Texas: The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations No. 12, 46 p. doi.org/10.23867/RI0012D.