File:Murnpeowie meteorite.jpg

From Infogalactic: the planetary knowledge core
Jump to: navigation, search
Original file(929 × 715 pixels, file size: 132 KB, MIME type: image/jpeg)

Summary

Murnpeowie Meteorite - this spectacular, 2520 pound iron meteorite was found in the South Australian Outback in 1909. The mass has a well-preserved, dark-colored, outer surface with nice regmaglypts (surface cavities). Iron meteorites exposed at Earth's surface oxidize & rust relatively quickly. Given the fresh nature of Murnpeowie, it's been estimated that it fell to Earth within five years of it being found.

This rock is an octahedrite, dominated by kamacite & taenite. Sample material cut away for analysis (see dark orangish-colored area at upper left of meteorite) has shown that the Widmanstätten structure commonly seen in octahedrites is not well preserved in Murnpeowie. This has been inferred to be evidence for a significant heating event at some time in the rock's history.

(SAM Met 30A, South Australian Museum, Adelaide, Australia)

Location: South Australian Outback between Lake Callabonna and Lake Blanche, NE by E of Mt. Hopeless, near the Strzelecki Track, eastern South Australia.

Licensing

Lua error in package.lua at line 80: module 'strict' not found.

File history

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

Date/TimeThumbnailDimensionsUserComment
current05:39, 5 January 2017Thumbnail for version as of 05:39, 5 January 2017929 × 715 (132 KB)127.0.0.1 (talk)<p>Murnpeowie Meteorite - this spectacular, 2520 pound iron meteorite was found in the South Australian Outback in 1909. The mass has a well-preserved, dark-colored, outer surface with nice regmaglypts (surface cavities). Iron meteorites exposed at Earth's surface oxidize & rust relatively quickly. Given the fresh nature of Murnpeowie, it's been estimated that it fell to Earth within five years of it being found. </p> <p>This rock is an octahedrite, dominated by kamacite & taenite. Sample material cut away for analysis (see dark orangish-colored area at upper left of meteorite) has shown that the Widmanstätten structure commonly seen in octahedrites is not well preserved in Murnpeowie. This has been inferred to be evidence for a significant heating event at some time in the rock's history. </p> <p>(SAM Met 30A, South Australian Museum, Adelaide, Australia) </p> <p>Location: South Australian Outback between Lake Callabonna and Lake Blanche, NE by E of Mt. Hopeless, near the Strzelecki Track, eastern South Australia. </p>
  • You cannot overwrite this file.

The following 4 pages link to this file: