Mgrre_Thinsections_Mgrre_13_79,
2021
Western Michigan University
Mgrre_Thinsections_Mgrre_13_96,
2021
Western Michigan University
Mgrre_Thinsections_Mgrre_14_20,
2021
Western Michigan University
Mgrre_Thinsections_Mgrre_60_9,
2021
Western Michigan University
Mgrre_Thinsections_Mgrre_92_23,
2021
Western Michigan University
Mgrre_Thinsections_Moc_01_79,
2021
Western Michigan University
Mgrre_Thinsections_Moc_01_93,
2021
Western Michigan University
Mgrre_Thinsections_Moc_02_14,
2021
Western Michigan University
Mgrre_Thinsections_Moc_03_029,
2021
Western Michigan University
Mgrre_Thinsections_Moc_05_24,
2021
Western Michigan University
Mgrre_Thinsections_Mgrre_12_165,
2021
Western Michigan University
Mgrre_Thinsections_Mgrre_90_20,
2021
Western Michigan University
Mgrre_Thinsections_Mgrre_39_24,
2021
Western Michigan University
Mgrre_Thinsections_Moc_05_45,
2021
Western Michigan University
Mgrre_Thinsections_08-A_72,
2021
Western Michigan University
Mgrre_Thinsections_Moc_10_75,
2021
Western Michigan University
Mgrre_Thinsections_Moc_10_34,
2021
Western Michigan University
Mgrre_Thinsections_Moc_10_46,
2021
Western Michigan University
Factors Controlling Longshore Variations Of Beach Changes Induced By Tropical Storm Eta Along Pinellas County Beaches, West-Central Florida,
2021
University of South Florida
Factors Controlling Longshore Variations Of Beach Changes Induced By Tropical Storm Eta Along Pinellas County Beaches, West-Central Florida, Francesca Luisa Toledo Cossu
USF Tampa Graduate Theses and Dissertations
Tropical Storm Eta impacted the coast of west-central Florida from November 11 to 12, 2020, and generated high waves over elevated water levels for over 20 hours. A total of 148 beach and nearshore profiles, spaced about 300 m apart, were surveyed one to two weeks before and one to eight days after the storm to examine the beach changes along four barrier islands, including Sand Key, Treasure Island, Long Key and Mullet Key. Storm waves superimposed on elevated water levels reached the toe of dunes, causing modest dune erosion as well as overwash in some areas. Most of the …
Late Miocene Unroofing Of The Inner Lesser Himalaya Recorded In The Nw Himalaya Foreland Basin,
2021
Louisiana State University and Agricultural and Mechanical College
Late Miocene Unroofing Of The Inner Lesser Himalaya Recorded In The Nw Himalaya Foreland Basin, Elise Marie Exnicios
LSU Master's Theses
Testing models that link climate and solid Earth tectonics requires independent erosional, structural and climatic histories. Two well preserved stratigraphic sections of the Himalayan foreland basin are exposed in NW India. The Jawalamukhi (13–5 Ma) and Joginder Nagar sections (21–13 Ma) are dated by magnetostratigraphy and span a period of significant climate change and tectonic evolution. We use detrital zircon U-Pb dating and apatite fission track analyses to reconstruct changes in the patterns of erosion and exhumation in this area from the Early Miocene to Pliocene. The provenance of the foreland sediments shows that since at least ~21 Ma the …
