File:Agate (Tertiary; Agate Bay, King George Island, South Shetland Islands) 1.jpg

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English: Agate from the Tertiary of Antarctica. (~3.8 centimeters across at its widest)

"Agate" is a rockhound/collector term for cavities in rocks (usually sedimentary rocks such as limestone or igneous rocks such as basalt) that have been partially or completely filled with irregularly concentric layers of microcrystalline, fibrous quartz (chalcedony - SiO2). Agate is quartz.

The Antarctic agate seen here is from King George Island in the South Shetland Islands. Geologically, the South Shetlands are part of the Antarctic Peninsula, but have been separated by back-arc rifting, which formed the Bransfield Basin (Bransfield Strait). The agate is a cavity filling derived from Tertiary-aged volcanic rocks on the island - principally basalt and andesite lava flows. In Admiralty Bay, the Agat Point Dike, composed of basaltic andesite, also contains agate masses.

Locality: Agate Bay, King George Island, South Shetland Islands, north of the Antarctic Peninsula
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Source https://www.flickr.com/photos/47445767@N05/50886045592/
Author James St. John

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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/50886045592. It was reviewed on 2 February 2021 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

2 February 2021

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current16:33, 2 February 2021Thumbnail for version as of 16:33, 2 February 20212,283 × 1,508 (2.42 MB)Ser Amantio di Nicolao (talk | contribs)Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/50886045592/ with UploadWizard

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