Tidal inlet development and migration in Isles Dernieres Barrier Island Arc, Louisiana
- Geological Survey, Menlo Park, CA (USA)
- Geological Survey, St. Petersburg, FL (USA)
The Isles Dernieres barrier arc formed about 420 years ago in response to the abandonment of the Bayou Petit Caillou delta of the Mississippi River. Over the past 100 years, the arc has undergone rapid erosion, with much of the Gulf shorelines retreating more than 1 km (10 m/year). Today, the island area is less than 25% of what it was 100 years ago. Most of this areal loss is from a narrowing of the islands as both the bay and Gulf shorelines retreated. A significant portion, however, is due to development of two large tidal inlets that segmented the 32 km long arc into three groups of islands from what was a nearly continuous island in 1890. The presence of these inlets and two recently formed smaller ones alters longshore transport and island erosion patterns. To predict the future of the Isles Dernieres, the authors must understand the history and processes of tidal inlet development.
- OSTI ID:
- 5140768
- Report Number(s):
- CONF-8910221--
- Journal Information:
- AAPG Bulletin (American Association of Petroleum Geologists); (USA), Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (USA) Vol. 73:9; ISSN AABUD; ISSN 0149-1423
- Country of Publication:
- United States
- Language:
- English
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