The measurements were made with an aneroid barometer and must be regarded
as only approximately correct.
The deposit of asphalt at the Lithocarbon Rubber Company's mine is in the
Anacacho limestone. The asphalt-bearing horizon corresponds with the upper part
of No. 6, above.
The following is a compilation from a large number of sections
made along Turkey Creek, beginning at Cline Mountain, in the Brack
Fig. 4.—Section of the Anacacho Mountains, Kin. ney County.
ett quadrangle, and extending to
Wagon Top Butte, in the Uvalde
quadrangle.
('ampliation, of sections along Turkey Creek.
32
11;: 1,1.. 164.
RIO GRANDE COAL FIELDS OF TEXAS.
II. Anacacho formation —Continued. Feet.
2. Soft material containing fragments of a very large Inoeeramus 5 1. Thin, very hard, brown, siliceous ledge 3 or 4
Total Anacacho beds 279
I. Austin chalk: '
3. Hard brownish limestone, containing many Gryphcea aucellu 5
2. Hard chalky limestone 10
1. Unexposed—to bottom of arroyo 20
Total Austin chalk exposed 35
Total Anacacho beds 279
Total here exposed 314
F Hard gray limestone. This lime-
Feet.
stone is coarsely granular, loose
textured, and possesses a very rough, honeycombed, weath- ered surface. It contains an
undetermined species of Radi-
olites or Sphferulites
10
Thinly laminated, hard or marly
limestone
20
Ledges of gray limestone, with
honeycombed surface, but not
so hard as the uppermost lime- stone. This bed is not well
exposed, so that Ltsdetail could not 1 >e determined
: j»o
Hard, dark-brown, granular
limestone
3
Light-colored, yellowish, granu- lar limestone in hard, thick
ledges. This bed contains specimens of a large Exogyra
and a Radiolite; also some
pebbles of white and yellow
quartz
7
15. Thinly bedded limestone, becoming a thinly laminated, firm, calcareous shale.
15
14. Laminated yellow calcareous marl
50








