File:Grossman et al 2011 skagit shallow stratigraphy.pdf

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Grossman_et_al_2011_skagit_shallow_stratigraphy.pdf(file size: 77.01 MB, MIME type: application/pdf)



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Citation

Grossman, E.E., George, D.A., and Lam, Angela, 2011. Shallow stratigraphy of the Skagit River Delta, Washington, derived from sedimentparticles of clay, silt, sand, gravel, or cobble, transported by water, are called sediment. cores: U.S. Geological Survey Open File Report 2011-1194, 123 p., available at http://pubs.usgs.gov/of/2011/1194/.

Analysis

  • Describes changes in sedimentparticles of clay, silt, sand, gravel, or cobble, transported by water, are called sediment. character in Skagit Bay at the South Fork, including increased deposition of sand and progradation of the delta since settlement, suggesting that current flood flows transport sand bedload into the bay, and that this is different than historical processes which created a laminated mud environment. Pcereghino]]

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current23:46, 27 July 2012 (77.01 MB)Pcereghino (Talk | contribs)
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