Past, Present, Future Erosion at Locke Island

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Description

This report describes and documents the erosion that has occurred along the northeast side of Locke Island over the last 10 to 20 years. The principal cause of this erosion is the massive Locke Island landslide complex opposite the Columbia River along the White Bluffs, which constricts the flow of the river and deflects the river's thalweg southward against the island.

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Creation Information

Bjornstad, Bruce N. August 8, 2006.

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This report is part of the collection entitled: Office of Scientific & Technical Information Technical Reports and was provided by UNT Libraries Government Documents Department to Digital Library, a digital repository hosted by the UNT Libraries. More information about this report can be viewed below.

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Description

This report describes and documents the erosion that has occurred along the northeast side of Locke Island over the last 10 to 20 years. The principal cause of this erosion is the massive Locke Island landslide complex opposite the Columbia River along the White Bluffs, which constricts the flow of the river and deflects the river's thalweg southward against the island.

Physical Description

PDFN

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  • Report No.: PNNL-15941
  • Grant Number: AC05-76RL01830
  • DOI: 10.2172/890730 | External Link
  • Office of Scientific & Technical Information Report Number: 890730
  • Archival Resource Key: ark:/67531/metadc882592

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Creation Date

  • August 8, 2006

Added to The UNT Digital Library

  • Sept. 21, 2016, 2:29 a.m.

Description Last Updated

  • Nov. 30, 2016, 4:14 p.m.

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Citations, Rights, Re-Use

Bjornstad, Bruce N. Past, Present, Future Erosion at Locke Island, report, August 8, 2006; Richland, Washington. (digital.library.unt.edu/ark:/67531/metadc882592/: accessed September 24, 2017), University of North Texas Libraries, Digital Library, digital.library.unt.edu; crediting UNT Libraries Government Documents Department.