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About: Bay mud     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatFisheries, within Data Space : dbpedia.org associated with source document(s)

Type: Thingyago:BodyOfWater109225146yago:Estuary109274500yago:Fishery103350880yago:GeographicPoint108578706yago:Location100027167yago:Object100002684yago:PhysicalEntity100001930yago:Point108620061yago:Workplace104602044yago:YagoGeoEntityyago:YagoLegalActorGeoyago:YagoPermanentlyLocatedEntityyago:Thing100002452yago:WikicatEstuariesyago:WikicatFisheries New Facet based on Instances of this Class

Bay mud consists of thick deposits of soft, unconsolidated silty clay, which is saturated with water; these soil layers are situated at the bottom of certain estuaries, which are normally in temperate regions that have experienced cyclical glacial cycles. Example locations are Cape Cod Bay, Reserve in Shanghai, China, Banc d'Arguinpreserve in Mauritania, The Bristol Channel in the United Kingdom, Mandø Island in the Wadden Sea in Denmark, Florida Bay, San Francisco Bay, Bay of Fundy, Casco Bay, Penobscot Bay, and Morro Bay. Bay mud manifests low shear strength, high compressibility and low permeability, making it hazardous to build upon in seismically active regions like the San Francisco Bay Area.