. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology; Zoology. hill: geology of Jamaica. 35 distance to the west tliereof. At Port Maria the same plain is visible both on the mainland and on Cabaretta Island, shown in Plate XIII. Fig. 1, which has been but lately severed from it. This level is largely, if not entirely, composed of the old Pliocene marginal sediments of the sea which have been raised to their present position by epeirogenic S£A LSrSL Figure 12. Elevated Reefs, North The Elevated Reef Levels. â These are more fully described in a later ch
. Bulletin of the Museum of Comparative Zoology at Harvard College. Zoology; Zoology. hill: geology of Jamaica. 35 distance to the west tliereof. At Port Maria the same plain is visible both on the mainland and on Cabaretta Island, shown in Plate XIII. Fig. 1, which has been but lately severed from it. This level is largely, if not entirely, composed of the old Pliocene marginal sediments of the sea which have been raised to their present position by epeirogenic S£A LSrSL Figure 12. Elevated Reefs, North The Elevated Reef Levels. â These are more fully described in a later chapter.â¢"â They are three in number, approximating 15, 25, and 60 feet above the sea, respectively. Only the lowest of these has any consider- able extent. These benches are usually composed of single strata, no- where over 50 feet in thickness, made up of coral heads in situ and. 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 Harvard University. Museum of Comparative Zoology. Cambridge, Mass. : The Museum
Size: 4863px × 514px
Photo credit: © Book Worm / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookauthorha, bookcentury1800, bookdecade1860, booksubjectzoology
