File:Komatiite pebble- & BIF pebble-bearing polymict conglomerate (Timiskaming Conglomerate, Neoarchean, -2.674 Ga; Kirkland Lake, Ontario, Canada) (14851526200).jpg

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

Original file(1,341 × 1,224 pixels, file size: 1.22 MB, MIME type: image/jpeg)

Captions

Captions

Add a one-line explanation of what this file represents

Summary

[edit]
Description

Polymict conglomerate (6.0 cm across) having pebbles of komatiite and banded iron formation from the Timiskaming Conglomerate (Neoarchean, <2.674 billion years) at Kirkland Lake, Ontario, Canada.

Komatiite pebble = dark green clast with criss-crossing blackish needle structures (spinifex texture) at upper right.

BIF pebble = dark red clast at left.


This is the most amazing conglomerate I’ve ever seen. This is the Timiskaming Conglomerate of Ontario, Canada. It’s a polymict conglomerate, which means it consists of pebbles of many different lithologies (rock types). Apart from the striking colors and shapes, this polymict conglomerate is especially spectacular for the presence of pebbles of rare rock types. The sample shown here includes pebbles of the rare ultramafic extrusive igneous rock komatiite. The komatiite pebbles are easily recognizable based on their spinifex texture (long, needle-shaped crystals). There’s also a small clast of banded iron formation.

The Timiskaming Conglomerate is a fluvial to alluvial fan deposit. Its clasts are a wonderful variety of Archean rock types, including intrusive igneous rocks (diorites, anorthosites), extrusive igneous rocks (basalts, komatiites, dacites, rhyolites), sedimentary rocks (graywackes, siltstones, cherts), and other clasts such as vein quartz and even pyrite pebbles (Gray & Hutchinson, 2001).

The komatiite pebble is consistent with eastern Ontario’s Pyke Hill Komatiite (2.710 to 2.718 billion years).

Unit & Age: Timiskaming Conglomerate, upper Neoarchean, <2.674 billion years.

Locality: Kirkland Lake, northeastern Timiskaming District, eastern Ontario, southeastern Canada.


Reference Cited:

Gray, M.D. & R.W. Hutchinson. 2001. New evidence for multiple periods of gold emplacement in the Porcupine Mining District, Timmins area, Ontario, Canada. Economic Geology 96: 453-475.
Date
Source Komatiite pebble- & BIF pebble-bearing polymict conglomerate (Timiskaming Conglomerate, Neoarchean, <2.674 Ga; Kirkland Lake, Ontario, Canada)
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@N05/14851526200. It was reviewed on 29 February 2024 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

29 February 2024

File history

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

Date/TimeThumbnailDimensionsUserComment
current16:30, 29 February 2024Thumbnail for version as of 16:30, 29 February 20241,341 × 1,224 (1.22 MB)SeichanGant (talk | contribs)Transferred from Flickr via #flickr2commons

There are no pages that use this file.

Metadata