Barrier islands represent a complex coastal system that includes a number of different sedimentary depositional environments; nearshore zone, beach, dunes, washover fans, marshes, tidal flats, estuaries, lagoons, and tidal inlets. The morphodynamics of these fragile coastal systems provide a further complication to this coastal type. Although barrier islands comprise only 15% of the world's coastline, they have received a far greater proportion of attention from the scientific and engineering community, and more recently, from coastal managers and environmentalists. Modern barrier islands are arguably the most expensive and most vulnerable of all coastal environments. Pressure from developers for residential, industrial, and recreational development has caused most of our barriers to become significantly impacted by human activity, especially over the past few decades. These pres sures have led to extensive preservation of natural barriers through efforts from all levels of government and also by private organizations. Governments have also formed coastal management programs that help to control any future de velopment with the intent being to keep human activity compatible with barrier island morphodynamics. In order to devise appropriate coastal zone management programs, it is necessary to have a comprehensive understanding of the morpho dynamics of barrier island systems. This volume provides comprehensive details on barrier island morphology, sediment distribution, and the process-response mechanisms that cause changes to both. These are the important aspects of barrier systems that can provide important input into the development and implementation of coastal management programs.
"I know of no similar work (in scope, content and orientation). That is why we are all waiting so anxiously for this volume to be completed. Its perspective is unique." Charles Finkel, Editor to the Journal of Coastal Research
Dunes, ebb tidal deltas, beachrock, barrier islands and spits are present along the northern coast. ing sector, extending from Touros to the RN/Ceará (CE) border (Vital 9.2 Geological and Geomorphological Coastal Setting The eastern ...
... The Black Sea (ID 14.), there is a relationship between elevation and age with those located at greater depths being the oldest. This broad relationship is likely a function of post-glacial SLR. The drowned barrier preserved in the Black ...
Barrier Islands from the Gulf of St. Lawrence to the Gulf of Mexico
This book will help you explore the origins of coastal features, such as barrier islands, sand beaches and coastal dunes.
This symposium series has an enviable international reputation for its quality, and so the contributions represent the latest developments in the field.
Barrier Islands
This book, first published in 1973, presents the papers from the 3rd Binghamton Geomorphology Symposium.
Consisting of almost 270 subject entries in an easy-to-use format, this volume covers the physical, chemical, and biological characteristics of estuaries.
This unique richly-illustrated account of the landforms and geology of the world’s coasts, presented in a country-by-country (state-by-state) sequence, assembles a vast amount of data and images of an endangered and increasingly populated ...