Layered ultramafic, Duke Island, Alaska
The layered ultramafic rock 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
13625179
Media ID
43167336
Size
5301px x 3427px
(15.1MB)
Credit
Fletcher & Baylis /Science Source/ www.ardea.com
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NA
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Ardea Picture Library
Picture No
13625179
Contributor Ref
SCS-90074413
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Duke Igneous Intrusion Intrusions Layered Minerals Olivine Peridotite Petrology Pyroxene Ultramafic
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