File:Diatomite (Monterey Formation, Miocene; diatomite quarry just south of Lompoc, California, USA) (16843717495).jpg
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[edit]DescriptionDiatomite (Monterey Formation, Miocene; diatomite quarry just south of Lompoc, California, USA) (16843717495).jpg |
Diatomite from the Miocene of California, USA. (6.8 cm across) Sedimentary rocks form by the solidification of loose sediments. Loose sediments become hard rocks by the processes of deposition, burial, compaction, dewatering, and cementation. There are three categories of sedimentary rocks: 1) Siliciclastic sedimentary rocks form by the solidification of sediments produced by weathering & erosion of any previously existing rocks. 2) Biogenic sedimentary rocks form by the solidification of sediments that were once-living organisms (plants, animals, micro-organisms). 3) Chemical sedimentary rocks form by the solidification of sediments formed by inorganic chemical reactions. Most sedimentary rocks have a clastic texture, but some are crystalline. Diatomite, or diatomaceous earth, is a uncommon but distinctive biogenic sedimentary rock - it is whitish, powdery, and very lightweight. It seems quite soft, but the individual particles making up the rock are siliceous (opaline silica), having a hardness around 6 on the Mohs Scale. This makes diatomaceous earth a wonderful mild abrasive. It is mined for use in a wide variety of products. Most people encounter diatomites everyday as one of the ingredients in toothpaste (the opaline silica scrapes away foreign material from tooth surfaces). Diatomites form by the accumulation of numerous diatom skeletons in lake or marine settings. Diatoms are very small, unicellular, photosynthetic organisms (Kingdom Protista, Phylum Bacillariophyta). Some call them “algae”, but they’re not. Some call them “plants”, but they’re not. They’re protists. Diatoms make a two-part skeleton composed of opal (opaline silica, SiO2·nH2O). The diatom skeleton is called a frustule (see example photo - <a href="http://www.astrographics.com/GalleryPrints/Display/GP2131.jpg" rel="nofollow">www.astrographics.com/GalleryPrints/Display/GP2131.jpg</a>). Diatom frustules are usually rounded or elongated, and the two parts of the skeleton nest into each other, like a large petri dish over a slightly smaller petri dish. Careful examination of fossil diatoms typically requires use of a scanning electron microscope (SEM). Diatomites contain immense numbers of many different species of fossil diatoms. The appearance of diatomite closely resembles chalk. Chalk is calcareous, and will bubble in acid - diatomite won’t do that. Chalk is also noticeably heavier than diaomite. Diatomite and chalk also resemble kaolinite, a clay mineral. Kaolinite will not bubble in acid. It also has an earthy feel and an earthy smell, especially when wet. Kaolinite becomes noticeably sticky when wet. Stratigraphy: Monterey Formation, Miocene Locality: diatomite quarry just south of the town of Lompoc, Santa Barbara County, southern California, USA |
Date | |
Source | Diatomite (Monterey Formation, Miocene; diatomite quarry just south of Lompoc, California, USA) |
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@N05/16843717495 (archive). It was reviewed on 4 November 2019 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
4 November 2019
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current | 14:41, 4 November 2019 | 1,023 × 857 (1.14 MB) | Ainz Ooal Gown (talk | contribs) | Transferred from Flickr via #flickr2commons |
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Width | 1,023 px |
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Height | 857 px |
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Pixel composition | RGB |
Orientation | Normal |
Number of components | 3 |
Horizontal resolution | 375 dpi |
Vertical resolution | 375 dpi |
Software used | Adobe Photoshop Elements 13.0 (Macintosh) |
File change date and time | 21:32, 15 March 2015 |
Exif version | 2.21 |
Color space | sRGB |
Unique ID of original document | 4603BD39E757D29C6F9DC6D8D3312B15 |
Date and time of digitizing | 17:27, 15 March 2015 |
Date metadata was last modified | 17:32, 15 March 2015 |