The Sabine Uplift has been ably described by several authors since Harris, whose ideas have been recently summarized by Sidney Powers1 before this Association. These authorities are all of the opinion that the uplift is limited to that large geanticlinal fold whose axis extends in a northwest-southeast direction between Caddo and Bull Bayou. Powers assumes that other structural highs such as Homer and Monroe are of independent origin. With these ideas the present writer cannot wholly agree, and in support of his differing conclusions submits the two maps accompanying this paper (Figs. 1 and 2).
Figure 1...
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