Shelf Sandstones of the Deep Wilcox Trend, Central Texas Gulf Coast

Author(s):  
Jeffrey A. May
Palaios ◽  
1990 ◽  
Vol 5 (4) ◽  
pp. 346 ◽  
Author(s):  
Linda S. Albertzart ◽  
Bruce H. Wilkinson

1982 ◽  
Vol 23 (2) ◽  
pp. 163-176
Author(s):  
Christa J. Carvajal

When “the floodgates of emigration from Europe were opened by the political upheavals on the continent in 1848 … Texas was the goal of the thousands of refugees who fled from the turmoil.” Throughout the following decade, waves of German immigrants were thrust onto the shores of the Texas Gulf Coast at Indianola and eventually spread over much of Southwestern and Central Texas.


Author(s):  
Jens Figlus ◽  
Katherine Anarde ◽  
Timothy Dellapenna ◽  
Philip Bedient

The COAstal STorm Rapid Response (COASTRR) system has been implemented to measure hydro-dynamic, morphodynamic, and sedimentary processes occurring along coastlines during storm impact and subsequent recovery. Relatively few measurements are available to evaluate the physical processes shaping coastal systems during extreme storm events, nor to assess post-storm system recovery (e.g. Sherwood et al., 2014). Prior to landfall of Hurricane Harvey, instruments to collect high-resolution in-situ hydrodynamic measure-ments across two different barrier island transects on the upper Texas Gulf Coast were deployed before and recovered after the storm. Hurricane Harvey struck the central Texas Gulf Coast as a Category 4 storm on August 25, 2017 causing severe infrastructure damage and erosion near its landfall location but generating mostly accretional features at the two field sites on Hog Island and Follets Island, respectively, which were located more than 160 miles northeast of Harvey’s landfall location.


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