File:Burnham Overy Staithe Norfolk - geograph.org.uk - 1093986.jpg

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Burnham_Overy_Staithe_Norfolk_-_geograph.org.uk_-_1093986.jpg (640 × 480 pixels, file size: 49 KB, MIME type: image/jpeg)

Captions

Captions

Burnham Overy Staithe Norfolk

Summary

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Description
English: Burnham Overy Staithe Norfolk The tidal creek has changed considerably over the last 40 years, it appears to be narrower and shallower owing to the effects of an increase in the silt levels. This is apparent along much of this part of the North Norfolk Coast where the effects of erosion are evident.
Date Unknown date
Source From geograph.org.uk
Author Mary Kallagher
Attribution
(required by the license)
InfoField
Mary Kallagher / Burnham Overy Staithe Norfolk / 
Mary Kallagher / Burnham Overy Staithe Norfolk
Camera location52° 57′ 53.7″ N, 0° 44′ 42″ E  Heading=247° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location52° 57′ 53.1″ N, 0° 44′ 39″ E  Heading=247° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

Licensing

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w:en:Creative Commons
attribution share alike
This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: Mary Kallagher
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  • attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
  • share alike – If you remix, transform, or build upon the material, you must distribute your contributions under the same or compatible license as the original.

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Date/TimeThumbnailDimensionsUserComment
current13:40, 24 February 2011Thumbnail for version as of 13:40, 24 February 2011640 × 480 (49 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Burnham Overy Staithe Norfolk The tidal creek has changed considerably over the last 40 years, it appears to be narrower and shallower owing to the effects of an increase in the silt levels. This i

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