You may have to Search all our reviewed books and magazines, click the sign up button below to create a free account.
One of the main impacts of global warming is accelerated sea-level rise: Intergovernmental Panel on Climate Change predictions suggest that the rate of rise could reach as high as 5'10 mm/yr by the end of this century. While it is generally recognized that accelerated sea-level rise will severely impact low-gradient coastlines, scientists are still ill prepared to predict coastal response. A study of seven Gulf Coast estuaries (Mobile Bay and Mississippi Sound, Weeks Bay, Calcasieu Lake, Sabine Lake, Galveston Bay, Matagorda Bay, and Corpus Christi Bay) was aimed at examining their response to past changes in the rate of sea-level rise and climate. The rates of change are of the same magnitude as those predicted for this century. The estuarine response to change has been one of abrupt landward retreat and major reorganization of estuarine environments at decadal time scales. This book should be of interest to scientists and policy makers concerned with future impacts of global warming.
"The result of nearly 20 years of interdisciplinary research, this volume contributes to the archaeological and paleoenvironmental knowledge of an important but lightly investigated, hyperarid coastline at the heart of the Sonoran Desert. Focused on the coast near Puerto Peñasco, Sonora, Mexico, it examines the diverse groups occupying the coast for salt, abundant food sources, and shells for ornament manufacturing"--
This book presents chapters, written by leading coastal scientists, which collectively depict the current understanding of the processes that shape barrier islands and barrier spits, with an emphasis on the response of these landforms to changing conditions. A majority of the world’s population lives along the coast at the dynamic intersection between terrestrial and marine ecosystems and landscapes. As narrow, low-lying landforms, barriers are especially vulnerable to changes in sea level, storminess, the geographic distribution of grass species, and the rate of sand supply—some barriers will undergo rapid changes in state (e.g., from landward migrating to disintegrating), on human time...
"Sea level is rising, and yet Americans continue to develop beaches with little regard. In this volume, a group of coastal geologists discusses the startling saga of ten U.S. East and Gulf Coast shoreline communities (plus Puerto Rico and some western Europe strands) and the problems created by their inevitable interaction with natural processes in this highly dynamic geologic environment. The authors discuss the geologic context of the hazards of each site as the history of societal responses and their environmental impacts. Response to the natural coastal processes that threaten lives and buildings is carried out in a context of local, state and national politics with fixed short-term engineering solutions (beach replenishment, seawalls) generally favored over longer-term approaches (moving back, prohibition of seawalls). This essential GSA Special Paper foreshadows the impending rise of sea level and the myriad of shoreline responses and political controversies it will provoke."--Publisher's description.
Siliciclastic shallow-marine deposits record the interface between land and sea, and its response to a variety of forcing mechanisms: physical process regime, the internal dynamics of coastal and shelfal depositional systems, relative sea level, sediment flux, tectonic setting, and climate. These deposits have long been the subject of conceptual stratigraphic models that seek to explain the interplay between these various forcing mechanisms, and their preservation in the stratigraphic record. This volume arose from an SEPM research conference on shoreline-shelf stratigraphy that was held in Grand Junction, Colorado, on August 24-28, 2004. The aim of the resulting volume is to highlight the development over the last 15 years of the stratigraphic concepts and models that are used to interpret siliciclastic marginal-marine, shallow-marine, and shelf deposits.
A multidisciplinary review of salt marshes, describing how they function and respond to external pressures such as sea-level rise.
Not long after winning their independence from Mexico in 1836, Texans began clamoring for lighthouses. Hundreds of miles of barrier islands, shifting sandbars, and shallow bays made the Texas coast treacherous at a time when few overland routes provided access to the new republic. Beginning in 1852, twenty-eight lighthouses were built along the Texas coastline, on land and over water. Lighthouse service was often a family affair, with husbands, wives, and children working together as keepers and assistants. For nearly 70 years, construction continued as coastal erosion, hurricanes, and wars regularly damaged or destroyed those lighthouses already built. These sentinels of the sea lessened but did not eliminate the chance of shipwreck, so lifesaving stations, manned by able seamen with unsinkable surfboats, were established as well. As Texass lighthouses were gradually automated throughout the 20th century, many were sold to private owners or abandoned. Today, several have been restored, and twoat Aransas Pass and Port Isabelstill function as aids to navigation.--Amazon.come.