File:Yooperlite (sodalite syenite) (Lake Superior shoreline, Upper Peninsula of Michigan, USA) 10.jpg

From Wikimedia Commons, the free media repository
Jump to navigation Jump to search

Original file(3,199 × 2,431 pixels, file size: 1.83 MB, MIME type: image/jpeg)

Captions

Captions

Add a one-line explanation of what this file represents

Summary[edit]

Description
English: Yooperlite cobble from the Holocene of Michigan, USA.

"Yooperlite" is a rockhound term for beach clasts of syenite containing orange-fluorescing sodalite. They are found along gravelly beaches of Lake Superior, principally along the northern shoreline of Michigan's Upper Peninsula (= "U.P." - people who live there are "Yoopers").

Syenite is a potassium feldspar-rich, quartz-poor, coarsely-crystalline (phaneritic), intrusive igneous rock. Other minerals occur with the feldspar, such as dark-colored pyroxene and amphibole, and often nepheline.

Yooperlite is a sodalite-bearing syenite. Sodalite is a feldspathoid mineral having the chemical formula Na4(Al3Si3)O12Cl - sodium chloro-aluminosilicate. It is often bluish-colored (see: www.flickr.com/photos/jsjgeology/albums/72157714493738277), but in yooperlite, it's light- to grayish-colored. Under ultraviolet light (black light), the sodalite in yooperlite rocks glows bright orange.

Published research (Lauglin et al., 2018) indicates that yooperlites can be sourced to the Coldwell Alkaline Complex, along the northern Lake Superior shoreline in Ontario. The Coldwell Complex includes sodalite syenites having orange-fluoresceing hackmanite, a variety of sodalite. Pleistocene glaciers likely eroded Coldwell Complex rocks and deposited them on the American side of Lake Superior.

Fluorescence occurs as a result of short-wavelength UV radiation, long-wavelength UV radiation, or x-rays bombarding atoms. This causes electron excitation, but the electrons do not remain in an energetically excited state. They quickly give off energy and resume their normal energy levels. If the electron energy release is in the visible spectrum of light, a mineral glows, or fluoresces.

Geologic provenance: likely center 2 of Ontario's Coldwell Alkaline Complex, late Mesoproterozoic, 1.108 Ga

Locality: unrecorded / undisclosed site along the southern shore of Lake Superior, Upper Peninsula of Michigan, USA


Reference cited:

Laughlin et al. (2018) - A new find of fluorescent sodalite from Michigan's Upper Peninsula. Mineral News 34(5): 1-3. (www.yooperlites.com/img/Yooperlite_Sodalite_Discovery_Pap...)
Date
Source https://www.flickr.com/photos/47445767@N05/52948288852/
Author James St. John

Licensing[edit]

w:en:Creative Commons
attribution
This file is licensed under the Creative Commons Attribution 2.0 Generic license.
You are free:
  • to share – to copy, distribute and transmit the work
  • to remix – to adapt the work
Under the following conditions:
  • 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.
This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/52948288852. It was reviewed on 6 June 2023 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

6 June 2023

File history

Click on a date/time to view the file as it appeared at that time.

Date/TimeThumbnailDimensionsUserComment
current13:17, 6 June 2023Thumbnail for version as of 13:17, 6 June 20233,199 × 2,431 (1.83 MB)Ser Amantio di Nicolao (talk | contribs)Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/52948288852/ with UploadWizard

There are no pages that use this file.

Metadata