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dc.contributor.authorPaine, J.G.en_US
dc.contributor.authorMorton, R.A.en_US
dc.contributor.otheren_US
dc.date.accessioned2010-02-15T16:51:25Z
dc.date.available2010-02-15T16:51:25Z
dc.date.issued1989en_US
dc.identifier.urihttp://hdl.handle.net/1969.3/19375
dc.description50 p.en_US
dc.description.abstractThe purposes of this study were (1) to quantify recent (1974 to 1982) movement of Texas shorelines and vegetation lines by analysis of aerial photographs; (2) to place this movement in historical (pre-1974) context; and (3) to examine the influence of environmental variables such as storms, sea level, subsidence, and sediment supply on the movement of coastal boundaries. Shorelines and vegetation lines predominantly retreated between 1974 and 1982, a period of few tropical cyclones, relative sea-level stability, average fluvial discharge, and average rainfall. Erosion was most rapid at the Brazos-Colorado and Rio Grande fluvial-deltaic headlands and along south Padre Island. The most significant geological event affecting the Texas coast between 1974 and 1982 was Hurricane Allen, which made landfall north of Brownsville in 1980. Relatively little net shoreline movement during the study period indicates that Texas shorelines had generally recovered from this storm by 1982. Net vegetation retreat on the upper Texas coast increased southward from an average of 25 ft. between Sabine Pass and Bolivar Roads to 90 ft on Matagorda Peninsula. This net loss, primarily due to Hurricane Allen, indicates that little recovery of the vegetation line occurred during the first two years after the storm. Relatively low net vegetation-line retreat on the middle Texas coast implies that retreat caused by Allen (up to 100 ft in this area) encountered vegetation-line advance between 1974 and Allen landfall. The pre-Allen advance probably represents a combination of (1) normal vegetation-line advance in an area of adequate sediment supply and (2) vegetation recovery from Hurricane Celia, which crossed the middle Texas coast in 1970. Between 1974 and 1982, the Texas Gulf shoreline retreated slowly as a result of low storm incidence and relative sea-level stability. Erosion rates after 1982 will probably be higher, possibly approaching levels of the mid-1960's to mid 1970's, because of landfall of hurricanes such as Alicia in 1983 and increasing rates of relative sea-level rise since 1982. Continued reduction of sediment supply and construction and maintenance of reservoirs, jetties, and navigation channels will also contribute to higher erosion rates.en_US
dc.description.urihttp://gbic.tamug.edu/request.htmen_US
dc.publisheren_US
dc.relation.ispartofseries1612.00en_US
dc.relation.urien_US
dc.subjectbarrier islandsen_US
dc.subjectcoastal processesen_US
dc.subjectgeological hazardsen_US
dc.subjecthurricanesen_US
dc.subjectcoastal erosionen_US
dc.subjectprogradationen_US
dc.subjectcoastal zoneen_US
dc.titleShoreline and vegetation-line movement, Texas Gulf Coast, 1974-1982.en_US
dc.typeBooken_US
dc.placeen_US
dc.seriesUniv. Tex. Bur. Econ. Geol. Rep. 89-1.en_US
dc.vol-issueen_US
dc.geo-codeTexas coasten_US
dc.geo-codeBolivar Peninsulaen_US
dc.geo-codeBolivar Roadsen_US
dc.geo-codeSabine Passen_US
dc.locationGBIC Collectionen_US
dc.scaleen_US
dc.latitudeen_US
dc.longitudeen_US
dc.contract-noen_US
dc.notesen_US
dc.degreeen_US
dc.acquisition-srcen_US
dc.description-otheren_US
dc.universityen_US
dc.historyen_US
dc.call-noGB459.25 P38 1989 GBAYen_US


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