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
13625182
Media ID
43152740
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5247px x 3449px
(20.1MB)
Credit
Fletcher & Baylis /Science Source/ www.ardea.com
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NA
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Ardea Picture Library
Picture No
13625182
Contributor Ref
SCS-90074416
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Bedding Beds Duke Graded Igneous Intrusion Intrusions Layered Minerals Olivine Peridotite Petrology Pyroxene Sedimentary Ultramafic
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