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The Geomorphology of British Guiana

By: Bracewell, S.
Material type: ArticleArticleDescription: 463 - 469 pp ; Illustration.Subject(s): Geomorphology -British - Guiana In: Geological magazine : Vol. 78 Iss. 1-6 Year. 1941Summary: (1) There is no evidence of the alignment of the Essequibo with the edge of a deep ocean basin. (2) The Essequibo River is not a well-defined dividing line between two geological provinces. (3) The Essequibo River does not mark the former locality of a coast line; it is not parallel to a tectonic depression. (4) The “fault-line coast” criteria described are not restricted to the area west of the Essequibo, and even if they were, this would not necessarily be evidence of a tectonic break along die Essequibo. There are a number of other controversial statements in the paper. I have attempted to deal only with the chief points raised in the four arguments referred to
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Bound Journal Collection 550 GEO (Browse shelf) Available 002564

(1) There is no evidence of the alignment of the Essequibo with the edge of a deep ocean basin.

(2) The Essequibo River is not a well-defined dividing line between two geological provinces.

(3) The Essequibo River does not mark the former locality of a coast line; it is not parallel to a tectonic depression.

(4) The “fault-line coast” criteria described are not restricted to the area west of the Essequibo, and even if they were, this would not necessarily be evidence of a tectonic break along die Essequibo.

There are a number of other controversial statements in the paper. I have attempted to deal only with the chief points raised in the four arguments referred to

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