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File:Omarama Clay Cliffs.jpg

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Summary

Description
English: The Clay Cliffs are huge sharp pinnacles and ridges with deep, narrow ravines separating them. The Clay Cliffs are made of layers of gravel and silt, deposited by rivers flowing from glaciers existing 1-2 million years ago. Compared to the nearby mountains, which are 250 million years old, the Clay Cliffs are relatively new. Today the gravel and silt layers can be seen as sloping bands as the strata have been tilted since their deposition 1-2 million years ago.
Date
Source https://www.flickr.com/photos/volvob12b/10218851153/
Author Bernard Spragg. NZ
Camera location44° 29′ 18.76″ S, 169° 52′ 17.89″ E Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

Licensing

Creative Commons CC-Zero This file is made available under the Creative Commons CC0 1.0 Universal Public Domain Dedication.
The person who associated a work with this deed has dedicated the work to the public domain by waiving all of their rights to the work worldwide under copyright law, including all related and neighboring rights, to the extent allowed by law. You can copy, modify, distribute and perform the work, even for commercial purposes, all without asking permission.

This image was originally posted to Flickr by Bernard Spragg at https://flickr.com/photos/88123769@N02/10218851153 (archive). It was reviewed on 31 March 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-zero.

31 March 2019

VI seal

This image has been assessed under the valued image criteria and is considered the most valued image on Commons within the scope: Closeup of Omarama Clay Cliffs. You can see its nomination here.

Captions

Omarama Clay Cliffs

Items portrayed in this file

depicts

12 October 2013

44°29'18.762"S, 169°52'17.893"E

image/jpeg

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Date/TimeThumbnailDimensionsUserComment
current23:52, 31 March 2019Thumbnail for version as of 23:52, 31 March 20192,172 × 1,449 (2.05 MB)BoothsiftUser created page with UploadWizard

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