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 shows ^graded bedding^
Picture No
13625183
Media ID
43158964
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5241px x 3461px
(16.9MB)
Credit
Fletcher & Baylis /Science Source/ www.ardea.com
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NA
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Ardea Picture Library
Picture No
13625183
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SCS-90074417
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Alaskan Bedding Beds Complex Cove Duke Graded Halls Igneous Intrusion Intrusions Layered Minerals Olivine Peridotite Petrology Pyroxene Sedimentary Type Ultramafic
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