Study of erosion along Homer spit and vicinity, Kachemak Bay, Alaska

This is a progress report on the Homer Spit Beach Erosion Study. Information is presented regarding the rapid acceleration of the erosion processes due to the subsidence of the Homer Spit during the 27 March 1964 earthquake. The effect on existing groins both before and after the quake are discussed...

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Main Authors: Gronewald, G.J. (author), Duncan, W.W. (author)
Other Authors: TU Delft
Format: Report
Language:English
Published: ASCE 1965
Subjects:
Online Access:http://resolver.tudelft.nl/uuid:bd319f75-9c5a-4ee2-bcfc-f9c2bf2fe535
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spelling fttudelft:oai:tudelft.nl:uuid:bd319f75-9c5a-4ee2-bcfc-f9c2bf2fe535 2023-07-30T04:04:33+02:00 Study of erosion along Homer spit and vicinity, Kachemak Bay, Alaska Gronewald, G.J. (author) Duncan, W.W. (author) TU Delft 1965-10-01 http://resolver.tudelft.nl/uuid:bd319f75-9c5a-4ee2-bcfc-f9c2bf2fe535 en eng ASCE Proceedings Santa Barbara specialty conference http://resolver.tudelft.nl/uuid:bd319f75-9c5a-4ee2-bcfc-f9c2bf2fe535 (c) 1965 ASCE TLN100100 erosion spit earthquake report Text 1965 fttudelft 2023-07-08T20:20:10Z This is a progress report on the Homer Spit Beach Erosion Study. Information is presented regarding the rapid acceleration of the erosion processes due to the subsidence of the Homer Spit during the 27 March 1964 earthquake. The effect on existing groins both before and after the quake are discussed. Immediately after the quake, emergency measures were required to prevent wave and high water damage to existing structures on the Spit. The results concerning the effectiveness of these measures are presented for evaluation, along with the basic data gathered for the erosion study and some of the problems encountered. Report Kachemak Alaska Delft University of Technology: Institutional Repository Spit The ENVELOPE(-55.491,-55.491,-61.480,-61.480) The Spit ENVELOPE(170.217,170.217,-71.300,-71.300)
institution Open Polar
collection Delft University of Technology: Institutional Repository
op_collection_id fttudelft
language English
topic TLN100100
erosion
spit
earthquake
spellingShingle TLN100100
erosion
spit
earthquake
Gronewald, G.J. (author)
Duncan, W.W. (author)
Study of erosion along Homer spit and vicinity, Kachemak Bay, Alaska
topic_facet TLN100100
erosion
spit
earthquake
description This is a progress report on the Homer Spit Beach Erosion Study. Information is presented regarding the rapid acceleration of the erosion processes due to the subsidence of the Homer Spit during the 27 March 1964 earthquake. The effect on existing groins both before and after the quake are discussed. Immediately after the quake, emergency measures were required to prevent wave and high water damage to existing structures on the Spit. The results concerning the effectiveness of these measures are presented for evaluation, along with the basic data gathered for the erosion study and some of the problems encountered.
author2 TU Delft
format Report
author Gronewald, G.J. (author)
Duncan, W.W. (author)
author_facet Gronewald, G.J. (author)
Duncan, W.W. (author)
author_sort Gronewald, G.J. (author)
title Study of erosion along Homer spit and vicinity, Kachemak Bay, Alaska
title_short Study of erosion along Homer spit and vicinity, Kachemak Bay, Alaska
title_full Study of erosion along Homer spit and vicinity, Kachemak Bay, Alaska
title_fullStr Study of erosion along Homer spit and vicinity, Kachemak Bay, Alaska
title_full_unstemmed Study of erosion along Homer spit and vicinity, Kachemak Bay, Alaska
title_sort study of erosion along homer spit and vicinity, kachemak bay, alaska
publisher ASCE
publishDate 1965
url http://resolver.tudelft.nl/uuid:bd319f75-9c5a-4ee2-bcfc-f9c2bf2fe535
long_lat ENVELOPE(-55.491,-55.491,-61.480,-61.480)
ENVELOPE(170.217,170.217,-71.300,-71.300)
geographic Spit The
The Spit
geographic_facet Spit The
The Spit
genre Kachemak
Alaska
genre_facet Kachemak
Alaska
op_relation Proceedings Santa Barbara specialty conference
http://resolver.tudelft.nl/uuid:bd319f75-9c5a-4ee2-bcfc-f9c2bf2fe535
op_rights (c) 1965 ASCE
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