Evaluation of Boulder Deposits Linked to Late Neogene Hurricane Events
Contributions in this collection discuss storm deposits dating from Neogene time between 23 and 1.8 million years ago, as well as the last 1.8 million years, including the Pleistocene and Holocene. As today, past hurricane events were responsible for the erosion of rocky shorelines due to the impact...
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Format: | Electronic Book Chapter |
Language: | English |
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Basel, Switzerland
MDPI - Multidisciplinary Digital Publishing Institute
2021
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Online Access: | DOAB: download the publication DOAB: description of the publication |
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001 | doab_20_500_12854_77068 | ||
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024 | 7 | |a 10.3390/books978-3-0365-2579-2 |c doi | |
041 | 0 | |a eng | |
042 | |a dc | ||
072 | 7 | |a GP |2 bicssc | |
100 | 1 | |a Johnson, Markes E. |4 edt | |
700 | 1 | |a Ledesma-Vázquez, Jorge |4 edt | |
700 | 1 | |a Johnson, Markes E. |4 oth | |
700 | 1 | |a Ledesma-Vázquez, Jorge |4 oth | |
245 | 1 | 0 | |a Evaluation of Boulder Deposits Linked to Late Neogene Hurricane Events |
260 | |a Basel, Switzerland |b MDPI - Multidisciplinary Digital Publishing Institute |c 2021 | ||
300 | |a 1 electronic resource (180 p.) | ||
336 | |a text |b txt |2 rdacontent | ||
337 | |a computer |b c |2 rdamedia | ||
338 | |a online resource |b cr |2 rdacarrier | ||
506 | 0 | |a Open Access |2 star |f Unrestricted online access | |
520 | |a Contributions in this collection discuss storm deposits dating from Neogene time between 23 and 1.8 million years ago, as well as the last 1.8 million years, including the Pleistocene and Holocene. As today, past hurricane events were responsible for the erosion of rocky shorelines due to the impact of storm waves, in addition to flood deposits due to heavy rainfall after big storms, resulting in landfall. The former typically resulted in coastal boulder deposits (CBDs) and the latter in coastal outwash deposits (CODs). Study locations covered by this treatment include three within the confines of Mexico's Gulf of California and three in the northeast Atlantic Ocean, including the Canary Islands and Azores, as well as the coast of Norway. Rock types canvassed in these studies are dominated by igneous rocks that include surface flows such as andesite and basalt as well as surface exposures of plutonic rocks that originated deep below the surface such as granite and near-mantle rocks like low-grade chromite. These rock types reflect a range in rock density, which has an effect on the ability of storm waves to degrade rocky shores in the production of CBDs. The site-specific studies in this collection also share an application treating the shape of boulders resulting from shore erosion. The collection is introduced by a survey covering Neogene CODs registered in the geological literature and a concluding paper focused on the use of satellite images as a means for detecting previously unrecognized coastal storm deposits. | ||
540 | |a Creative Commons |f https://creativecommons.org/licenses/by/4.0/ |2 cc |4 https://creativecommons.org/licenses/by/4.0/ | ||
546 | |a English | ||
650 | 7 | |a Research & information: general |2 bicssc | |
653 | |a bibliography | ||
653 | |a large clasts | ||
653 | |a Miocene | ||
653 | |a Pliocene | ||
653 | |a rocky shore | ||
653 | |a storm | ||
653 | |a tsunami | ||
653 | |a barrier boulder deposits | ||
653 | |a hurricane storm surge | ||
653 | |a hydrodynamic equation | ||
653 | |a Gulf of California (Mexico) | ||
653 | |a remote sensing | ||
653 | |a bouldering tourism | ||
653 | |a Iberian Peninsula | ||
653 | |a Mediterranean | ||
653 | |a Indonesia | ||
653 | |a Central America | ||
653 | |a coastal boulder deposits | ||
653 | |a storm surge | ||
653 | |a hydrodynamic equations | ||
653 | |a Holocene | ||
653 | |a Pleistocene | ||
653 | |a MIS 5e (Marine Isotope Substage 5e) | ||
653 | |a NE Atlantic Ocean | ||
653 | |a storm waves | ||
653 | |a western North America | ||
653 | |a coastal storm deposits | ||
653 | |a high-latitude settings | ||
653 | |a upper pleistocene | ||
653 | |a marine isotope substage 5e | ||
653 | |a North Atlantic Ocean | ||
653 | |a coastal erosion | ||
653 | |a Marine Isotope Substage 5e | ||
653 | |a Gulf of California | ||
653 | |a n/a | ||
856 | 4 | 0 | |a www.oapen.org |u https://mdpi.com/books/pdfview/book/4686 |7 0 |z DOAB: download the publication |
856 | 4 | 0 | |a www.oapen.org |u https://directory.doabooks.org/handle/20.500.12854/77068 |7 0 |z DOAB: description of the publication |