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Summary
Hornfelses, rocks that have been baked by an igneous intrusion, are a common feature of w:Sourland Mountain. Here, a hornfels cliff displays metamorphosed w:argillite. The argillite typical of the area and this formation is usually gray in color, while the resulting hornfelsed argillite appears darker and more fine grained.
Photo taken by me.
Licensing
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I, the copyright holder of this work, release this work into the public domain. This applies worldwide. In some countries this may not be legally possible; if so: I grant anyone the right to use this work for any purpose, without any conditions, unless such conditions are required by law. |
File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 19:29, 17 May 2009 | | 1,944 × 2,592 (1.7 MB) | Lithium6ion | Hornfels, sedimentary rocks that have been baked by an igneous intrustion, are a common feature of Sourland Mountain. Here, a hornfel cliff displays metamorphosed argillite. The argillite typical of the area and this formation usually is gra |
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