{"@context":"http://iiif.io/api/presentation/2/context.json","@id":"https://repo.library.stonybrook.edu/cantaloupe/iiif/2/manifest.json","@type":"sc:Manifest","label":"A suggestion for anticipating alterations in wave action on shores consequent upon changes in water depths in harbors and coastal waters","metadata":[{"label":"dc.contributor.other","value":"Preservation Department, Stony Brook University Libraries"},{"label":"dc.description","value":"39 p. : ill., diagrams; 28 cm. Bibliography"},{"label":"dc.format","value":"Serialized Monograph"},{"label":"dc.format.medium","value":"Electronic resource"},{"label":"dc.identifier.uri","value":"http://hdl.handle.net/1951/61617"},{"label":"dc.language.iso","value":"en_US"},{"label":"dc.relation.ispartofseries","value":"Special report (State University of New York at Stony Brook. Marine Sciences Research Center);27"},{"label":"dc.rights","value":"Stony Brook University"},{"label":"dc.subject","value":"Ocean waves -- New York Bay."},{"label":"dcterms.contributor","value":"Torre, F. Jason"},{"label":"dcterms.dateAccepted","value":"2015-04-24T14:29:36Z"},{"label":"dcterms.dateSubmitted","value":"2015-04-24T14:29:36Z"},{"label":"dcterms.description","value":"from the introduction, \"The most important fact to keep in mind is that ocean surface waves, like any waves, transmit energy.  In the end, that energy, whose original source was the energy of the wind, is expended on the shore where it plays an important role in coastal erosion. The direction in which the wave energy is transmitted and which part of the coastline it will attack depends on the wave length and the depth of the water in which it runs. . .\""},{"label":"dcterms.isFormatOf","value":"A suggestion for anticipating alterations in wave action on shores consequent upon changes in water depths in harbors and coastal waters / Blair Kinsman ... [et al.].  Stony Brook : State University of New York, Marine Sciences Research Center, 1979."},{"label":"dcterms.issued","value":"1979"},{"label":"dcterms.provenance","value":"Made available in DSpace on 2015-04-24T14:29:36Z (GMT). No. of bitstreams: 3\nSpecial Report 27.pdf.jpg: 3005 bytes, checksum: 80f7e1618e0877ed6e99d0b4dd6239c8 (MD5)\nSpecial Report 27.pdf.txt: 91624 bytes, checksum: 0a069e8f9948676d86bcc438c2a217ac (MD5)\nSpecial Report 27.pdf: 40702396 bytes, checksum: 5fa38d916c67899907979e5e49722bea (MD5)\n  Previous issue date: 1979"},{"label":"dcterms.publisher","value":"Stony Brook, NY"},{"label":"dcterms.title","value":"A suggestion for anticipating alterations in wave action on shores consequent upon changes in water depths in harbors and coastal waters"}],"description":"This manifest was generated dynamically","viewingDirection":"left-to-right","sequences":[{"@type":"sc:Sequence","canvases":[{"@id":"https://repo.library.stonybrook.edu/cantaloupe/iiif/2/canvas/page-1.json","@type":"sc:Canvas","label":"Page 1","height":1635,"width":1239,"images":[{"@type":"oa:Annotation","motivation":"sc:painting","resource":{"@id":"https://repo.library.stonybrook.edu/cantaloupe/iiif/2/56%2F95%2F21%2F56952110916549330369837527276349464503/full/full/0/default.jpg","@type":"dctypes:Image","format":"image/jpeg","height":1635,"width":1239,"service":{"@context":"http://iiif.io/api/image/2/context.json","@id":"https://repo.library.stonybrook.edu/cantaloupe/iiif/2/56%2F95%2F21%2F56952110916549330369837527276349464503","profile":"http://iiif.io/api/image/2/level2.json"}},"on":"https://repo.library.stonybrook.edu/cantaloupe/iiif/2/canvas/page-1.json"}]}]}]}