File:Lodestone (Magnet Cove Complex, mid-Cretaceous, 96-102 Ma; Perovskite Hill, Magnet Cove, Arkansas, USA) 2.jpg
Original file (1,693 × 1,361 pixels, file size: 1.27 MB, MIME type: image/jpeg)
Captions
Summary
[edit]DescriptionLodestone (Magnet Cove Complex, mid-Cretaceous, 96-102 Ma; Perovskite Hill, Magnet Cove, Arkansas, USA) 2.jpg |
English: Lodestone from the Cretaceous of Arkansas, USA
Magnetite is Fe3O4, a moderately common iron oxide mineral and the # 2 iron ore mineral. It has a metallic luster, dark gray to black color and streak, a hardness of 6 on the Mohs Hardness Scale, has no cleavage, is moderately heavy for its size, and often forms octahedral crystals. Magnetite is readily identified - a magnet will stick to it, hence the name. Two pieces of magnetite will not stick to each other, nor will they attract objects such as staples or paper clips. Lodestone is a "variety" of magnetite that actually does attract iron-bearing objects - lodestone is referred to as a "natural magnet". Published analysis of lodestone samples has shown that this material is actually not a variety of magnetite - it's a rock having intergrown magnetite with polarity and maghemite (= Fe2.67O4, iron oxide with iron vacancies in the molecular structure); hematite may be present (Fe2O3, also iron oxide). Titanomagnetite-bearing rocks may also be lodestones. The degree of magnetization can vary within a sample. Lodestones have a slightly different color than magnetite samples and they only occur at or near the land surface - usually at elevationally high outcrops. Lightning strikes are thought to be the magnetization charging mechanism. Supposedly, being exposed to a strong magnet / magnetic field for a while can make magnetite act like a lodestone - in other words, artificial lodestone. This small sample consists of weathered, intergrown magnetite octahedrons. It comes from central Arkansas' Magnet Cove Complex, a mid-Cretaceous ring dike complex that includes calciocarbonatite, a rare, calcitic igenous rock ("igneous limestone"). This specimen does attract a staple and can be referred to as lodestone. I suspect it is completely natural lodestone. Geologic unit: Magnet Cove Complex, Arkansas Alkaline Province, late Albian to Cenomanian, mid-Cretaceous, 96-102 Ma Locality: Perovskite Hill, Magnet Cove, northern Hot Spring County, central Arkansas, USA Photo gallery of lodestone: www.mindat.org/gallery.php?min=5805 Photo gallery of magnetite: www.mindat.org/gallery.php?min=2538 Locality info.: www.mindat.org/loc-188551.html See info. at: en.wikipedia.org/wiki/Lodestone and www.mindat.org/min-2533.html Lodestone-specific info. mostly summarized from: Wasilewski & Ketetschka (1999) - Lodestones: nature's only permanent magnet - What it is and how it gets charged. Geophysical Research Letter 26: 2275-2278. |
Date | |
Source | https://www.flickr.com/photos/47445767@N05/50991368678/ |
Author | James St. John |
Licensing
[edit]- 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@N05/50991368678. It was reviewed on 2 March 2021 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
2 March 2021
File history
Click on a date/time to view the file as it appeared at that time.
Date/Time | Thumbnail | Dimensions | User | Comment | |
---|---|---|---|---|---|
current | 17:50, 2 March 2021 | 1,693 × 1,361 (1.27 MB) | Ser Amantio di Nicolao (talk | contribs) | Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/50991368678/ with UploadWizard |
You cannot overwrite this file.
File usage on Commons
There are no pages that use this file.
Metadata
This file contains additional information such as Exif metadata which may have been added by the digital camera, scanner, or software program used to create or digitize it. If the file has been modified from its original state, some details such as the timestamp may not fully reflect those of the original file. The timestamp is only as accurate as the clock in the camera, and it may be completely wrong.
Camera manufacturer | Canon |
---|---|
Camera model | Canon PowerShot D10 |
Exposure time | 1/60 sec (0.016666666666667) |
F-number | f/10 |
ISO speed rating | 80 |
Date and time of data generation | 17:07, 28 February 2021 |
Lens focal length | 9.681 mm |
Width | 4,000 px |
Height | 3,000 px |
Bits per component |
|
Pixel composition | RGB |
Orientation | Normal |
Number of components | 3 |
Horizontal resolution | 180 dpi |
Vertical resolution | 180 dpi |
Software used | Adobe Photoshop Elements 18.0 (Macintosh) |
File change date and time | 02:23, 1 March 2021 |
Y and C positioning | Co-sited |
Exif version | 2.21 |
Date and time of digitizing | 17:07, 28 February 2021 |
Meaning of each component |
|
Image compression mode | 3 |
APEX shutter speed | 5.90625 |
APEX aperture | 6.65625 |
APEX exposure bias | −0.66666666666667 |
Maximum land aperture | 3.625 APEX (f/3.51) |
Metering mode | Pattern |
Flash | Flash fired, compulsory flash firing, red-eye reduction mode |
Supported Flashpix version | 1 |
Color space | sRGB |
Focal plane X resolution | 16,460.905349794 |
Focal plane Y resolution | 16,483.516483516 |
Focal plane resolution unit | inches |
Sensing method | One-chip color area sensor |
File source | Digital still camera |
Custom image processing | Normal process |
Exposure mode | Manual exposure |
White balance | Auto white balance |
Digital zoom ratio | 1 |
Scene capture type | Standard |
Lens used | 6.2-18.6 mm |
Date metadata was last modified | 21:23, 28 February 2021 |
Unique ID of original document | 1690E9244C94CB68743285CA4543579A |
IIM version | 24,576 |