Layered ultramafic, Duke Island, Alaska
The layered ultramafic on Duke Island, Alaska has mineral cumulate layers that resemble the bedding of sedimentary rocks despite being in an igneous intrusion. This photo is of clinopyroxene spherules
Picture No
13625180
Media ID
43167348
Size
5277px x 3450px
(15.6MB)
Credit
Fletcher & Baylis /Science Source/ www.ardea.com
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NA
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Ardea Picture Library
Picture No
13625180
Contributor Ref
SCS-90074414
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Complex Cove Duke Halls Igneous Intrusion Intrusions Layered Minerals Olivine Peridotite Petrology Pyroxene Ultramafic
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