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Geology topics

Chester K. Wentworth

Publications and source records attributed to Chester K. Wentworth.

2 recordsLinked to original sources

Third special report of the Hawaiian Volcano Observatory of Hawaii National Park and the Hawaiian Volcano Research Association: Ash formations of the island Hawaii

The purpose of the study was to determine the areal extent of the various volcanic ash formations, to describe them petrographically and to develop means of discriminating them. The ash formations, long known in a general way, had been only casually observed by geologists. Their interpretation and separation from other surficial materials has been much retarded by great differences in the degree of weathering and appearance of the same material in arid and in humid parts of the island. The wide distribution of ash formations in contrast to lava flows led to the hope that they could be discriminated and correlated and used as key horizons to work out the major events in the geologic history. It was believed that critical study of the effects of weathering on the ash formations, together with systematic tracing from regions of typical expression to others where the features were less typical and more obscure, would throw light on the stratigraphic relations and historical significance of the various units.

Hawaii

The shapes of beach pebbles

There is much confusion in geologic literature as to the shapes of fluvial and beach pebbles and the differences between them, if differences exist. Though the contrary has been asserted, most geologists who have written on the subject appear to hold the view that beach pebbles are generally flatter than river pebbles, having discoid, lozenge-shaped, ellipsoid, or oval forms. It is asserted by some that these forms are produced by pushing of the rock fragments to and fro by the waves. Others have considered that the shapes of the original fragments and the inherent structure of the rock are dominant in determining the shapes of beach pebbles, and with this view the writer is in accord. That beach pebbles, even those composed of massive igneous rocks are commonly of a flattened oval form seems certain, as has been stated elsewhere, but this fact is probably to be attributed to the development of such forms from original flat fragments or from rocks of schistose structure or to the segregation of such forms under the peculiar action of the waves, rather than to their production by a specialized wave abrasion.

Connecticut;Massachusetts