Abstract
Flood basalt flows of the Columbia River Basalt Group commonly exhibit well-developed colonnade and entablature structures formed during cooling of individual flows. A model is decribed that can be used to explain the occurrence of repeated entablature and colonnade by considering the effects of intermittent inundation.-after Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1144-1155 |
| Number of pages | 12 |
| Journal | Geological Society of America Bulletin |
| Volume | 97 |
| Issue number | 9 |
| DOIs | |
| Publication status | Published - 1986 |