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. Bulletin of the Geological Society of America. Geology. Figure 1.—Pillowy Surfaces in ellipsoidal Greenstone of the Orca Group (Mesozoic) The lava flow has been exposed by waves near Rocky Point, Prince William Sound, Alaska. Masses range from a few inches to 10 feet in diameter. Photograph from the U. S. Geological Survey. Bulletin 44.], plate viii-A.. Figure 2.—Cross-section showing radial Jointing of the Pillows at the same Locality Masses range from a few inches to 10 feet in diameter. Photograph from the U. S. Geological Survey. Bulletin 443, plate viii-B PILLOW SURFACES OF ELLIPSOIDAL

. Bulletin of the Geological Society of America. Geology. Figure 1.—Pillowy Surfaces in ellipsoidal Greenstone of the Orca Group (Mesozoic) The lava flow has been exposed by waves near Rocky Point, Prince William Sound, Alaska. Masses range from a few inches to 10 feet in diameter. Photograph from the U. S. Geological Survey. Bulletin 44.], plate viii-A.. Figure 2.—Cross-section showing radial Jointing of the Pillows at the same Locality Masses range from a few inches to 10 feet in diameter. Photograph from the U. S. Geological Survey. Bulletin 443, plate viii-B PILLOW SURFACES OF ELLIPSOIDAL  Stock Photo
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. Bulletin of the Geological Society of America. Geology. Figure 1.—Pillowy Surfaces in ellipsoidal Greenstone of the Orca Group (Mesozoic) The lava flow has been exposed by waves near Rocky Point, Prince William Sound, Alaska. Masses range from a few inches to 10 feet in diameter. Photograph from the U. S. Geological Survey. Bulletin 44.], plate viii-A.. Figure 2.—Cross-section showing radial Jointing of the Pillows at the same Locality Masses range from a few inches to 10 feet in diameter. Photograph from the U. S. Geological Survey. Bulletin 443, plate viii-B PILLOW SURFACES OF ELLIPSOIDAL GREENSTONE AND CROSS-SECTION OF RADIAL JOINTING OF PILLOW LAVA. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Geological Society of America. [New York : The Society]