File:Proglacial lacustrine rhythmitic argillite (varvite) (Konnarock Formation, Neoproterozoic, ~750 Ma; Grassy Branch Outcrop - Rt. 603 roadcut, Smyth County, Virginia, USA) 1 (30435477952).jpg

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

Original file(4,000 × 3,000 pixels, file size: 4.83 MB, MIME type: image/jpeg)

Captions

Captions

Add a one-line explanation of what this file represents

Summary

[edit]
Description

Proglacial lacustrine rhythmitic argillite from the Precambrian of Virginia, USA.

The Snowball Earth Glaciations during the Neoproterozoic were the most significant ice ages that Earth ever experienced - two or three of them occurred in succession. The most extreme models describing Snowball Earth have glacial ice completely covering all continents and all oceans, even at the equator. Some models, called “Slushball Earth”, have Earth’s equatorial oceanic areas not completely frozen over. Each Snowball Earth Glaciation was followed by a super-greenhouse climate. The resulting sedimentary record of these “freeze-fry” events typically consists of glacial tillites and overlying cap carbonates. These units are preserved at many localities on Earth.

The rock shown above has well-preserved horizontal laminations in argillite (= a very low-grade metamorphic rock formed by slight alteration of shale). Note that the laminations are rhythmic in their thicknesses. These are rhythmites. Published research has identified these sediments as proglacial lacustrine turbidites - they appear to be varves. Varves are common sedimentary units in Pleistocene proglacial lake settings. This is a Snowball Earth equivalent. The rhythmicity reflects seasonal changes (summer-winter-summer-winter, etc.). Demonstrable annual layering is scarce in the sedimentary rock record.

Stratigraphy: Konnarock Formation, Neoproterozoic, ~750 Ma

Locality: Grassy Branch Outcrop - roadcut on the northern side of Rt. 603, just downstream from the Big Laurel Creek-Grassy Branch confluence, west of the town of Troutdale & east of the town of Konnarock, southern Smyth County, southwestern Virginia, USA (36º 40.900’ North latitude, 81º 33.988’ West longitude)
Date
Source Proglacial lacustrine rhythmitic argillite (varvite) (Konnarock Formation, Neoproterozoic, ~750 Ma; Grassy Branch Outcrop - Rt. 603 roadcut, Smyth County, Virginia, USA) 1
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@N05/30435477952. It was reviewed on 24 June 2017 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-2.0.

24 June 2017

File history

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

Date/TimeThumbnailDimensionsUserComment
current17:45, 24 June 2017Thumbnail for version as of 17:45, 24 June 20174,000 × 3,000 (4.83 MB)Ser Amantio di Nicolao (talk | contribs)Transferred from Flickr via Flickr2Commons

There are no pages that use this file.

Metadata