| Year | 1953 |
|---|---|
| Journal | Bulletin of Marine Science of the Gulf and Caribbean |
| Volume | 3 |
| Number | 1 |
| Pages | 55-69 |
| Type | article in journal |
| Language | English |
| Id | 48799 |
Abstract
Intense erosion of calcareous shore rocks in the coral seas produces a thoroughly honeycombed, brittle rock. Examples of this erosion on the Florida Keys are described. Physio-chemical solution of calcium carbonate is considered only of local importance in intertidal erosion. It is suggested that the activities of boring and burrowing organisms are a major factor in this erosion.
Last change: 22.2.2024