The Chandeleur Islands ( French: Îles Chandeleur) are a chain of uninhabited barrier islands approximately 50 miles (80 km) long, located in the Gulf of Mexico, marking the outer boundary of the Chandeleur Sound. They form the easternmost point of the state of Louisiana, United States and are a part of the Breton National Wildlife Refuge. They are an important migrating point for many birds on their way south, and are a prime marsh and forest wildlife area.
The islands were named when explorer, Pierre Le Moyne d'Iberville, was sailing in search of the mouth of the Mississippi River along the Gulf Coast. He christened the islands on the eve of Fête de la Chandeleur—also known as Candlemas, a Christian feast day—on February 1, 1700. 
Prior to destruction by a hurricane in 1915 there was a fishing settlement on the islands, and even earlier there had been farming on the islands. The Chandeleur Island Light, built in 1895, stood as a landmark and recognizable location for mariners at sea and pilots flying over the Gulf of Mexico.  The islands were constantly eroded and changed by wave action, and most dramatically after the storm surges following hurricanes.
The islands have been generally shrinking and migrating landward since the late 19th century. A survey in the 1980s estimated that they would be in existence for about three more centuries. Before 1996, the seaward front of the islands lost about 20–30 feet of land each year, mostly replaced at the rear. From 1996 to 2004, the loss rate grew to about 300 feet (91 m) per year. In 1998, Hurricane Georges destroyed the islands and left the lighthouse in the middle of the ocean, and the barrier islands only just recovered when Hurricane Katrina struck in 2005.
However, the combined effect of Hurricane Dennis and Hurricane Katrina in 2005 reduced the island to shoals or sub-surface formations, and toppled the Chandeleur Island Light. Powerful storms can produce changes that would otherwise have taken many years. A study released in 2006 by geologists from the University of New Orleans shows that the usual sand and sediment patterns that rebuilt the islands after big storms have not been restored since Katrina reworked the area. There is also evidence of unprecedented landslides on the seafloor on the side toward the Gulf of Mexico, potentially allowing stronger waves with greater erosional impact to reach the islands.[ citation needed] Numerical models developed by other marine geologists indicate the islands could be mostly submerged within decades due to sea level rise, isolation from Mississippi River delta sediment, mud foundations, sediment transport issues, and damaging storms. 
- Pilkey, Orrin H.; Mary Edna Fraser (2003). A Celebration of the World's Barrier Islands. Columbia University Press. p. 120. ISBN 0-231-11970-4.
- Chandeleur Island Lighthouse, Louisiana at Lighthousefriends.com Archived August 6, 2013, at the Wayback Machine
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- Moore, Laura J.; Patsch, Kiki; List, Jeffrey H.; Williams, S. Jeffress (2014). "The potential for sea-level-rise-induced barrier island loss: Insights from the Chandeleur Islands, Louisiana, USA". Marine Geology. 355: 244–259. doi: 10.1016/j.margeo.2014.05.022. ISSN 0025-3227.
- "Chandeleur Islands". NASA Earth Observatory. Archived from the original on 2006-10-01. Retrieved 2006-05-03.
- "Chandeleur Islands said not rebuilding". Boston.com. August 2, 2006. Retrieved 2006-08-03.
- "EAARL-B Coastal Topography—Chandeleur Islands, Louisiana, 2012: Seamless (Bare Earth and Submerged)". Retrieved 2015-10-27.
- Terrano, Joseph F.; Flocks, James G.; Smith, Kathryn E. L. (2016). "Analysis of shoreline and geomorphic change for Breton Island, Louisiana, from 1869 to 2014". doi: 10.3133/ofr20161039. ISSN 2331-1258.
|Wikimedia Commons has media related to Chandeleur Islands.|
- Post-Ivan September 18, 2004 photo
- Change in the Length of the Middle Section of the Chandeleur Islands Oil Berm, November 17, 2010, through September 6, 2011 - USGS
- Change in the Length of the Northern Section of the Chandeleur Islands Oil Berm, September 5, 2010, through September 3, 2012 - USGS