Earth Features and Their Meaning: An Introduction to Geology for the Student and the General ReaderHobbs, William Herbert
Science
Earth Features and Their Meaning: An Introduction to Geology for the Student and the General Reader
Hobbs, William Herbert
Geology; Physical geography
=The shelf ice of the ice age.=—Shelf ice, such as we have become
familiar with in Antarctica as a marginal snow-ice terrace floating
upon the sea, no doubt existed during the ice age above the Gulf of
Maine (see Fig. 324, p. 298), and perhaps also over the deep sea to the
westward of Scotland. Though the inland ice probably covered the North
Sea, and upon the American side of the Atlantic the Long Island Sound,
both these basins are so shallow that the ice must have rested upon the
bottom, for neither is of sufficient depth to entirely submerge one of
the higher European cathedrals.
[Illustration:
FIG. 344.—Outline map of the front of the Green Bay lobe of the latest
continental glacier of the United States. Drumlins in solid black,
moraines with diagonal hachure, outwash plains and the till plain or
ground moraine in white (after Alden).]
=Character profiles.=—All surface features referable to continental
glaciers, whether carved in rock or molded from loose materials,
present gently flowing outlines which are convex upward (Fig. 345). The
only definite features carved from rock are the _roches moutonnées_,
with their flattened shoulders, while the hillocks upon moraines and
kames, and the drumlins as well, approximate to the same profile. The
esker in its cross sections is much the same, though its serpentine
extension may offer some variety of curvature when viewed from higher
levels.
[Illustration: FIG. 345.—Character profiles referable to continental
glacier.]
READING REFERENCES FOR CHAPTER XXII
General:—
JAMES GEIKIE. The Great Ice Age. 3d ed. London, 1894, pp. 850, maps 18.
CHAMBERLIN and SALISBURY. Geology, vol. 3, 1906, pp. 327-516.
FRANK LEVERETT. The Illinois Glacial Lobe, Mon. 38, U. S. Geol. Surv.,
1899, pp. 817, pls. 34; Glacial formations and Drainage Features of
the Erie and Ohio Basins, Mon. 41, _ibid._, 1902, pp. 802, pls. 25;
Comparison of North American and European Glacial Deposits, Zeit. f.
Gletscherk., vol. 4, 1910, pp. 241-315, pls. 1-5.
Former glaciations previous to Ice Age:—
A. STRAHAN. The Glacial Phenomena of Paleozoic Age in the Varanger
Fjord, Quart. Jour. Geol. Soc., London, vol. 53, 1897, pp. 137-146,
pls. 8-10.
BAILEY WILLIS and ELIOT BLACKWELDER. Research in China, Pub. 54,
Carnegie Inst. Washington, vol. 1, 1907, pp. 267-269, pls. 37-38.
A. P. COLEMAN. A Lower Huronian Ice Age, Am. Jour. Sci. (4), vol. 23,
1907, pp. 187-192.
W. M. DAVIS. Observations in South Africa, Bull. Geol. Soc. Am., vol.
17, 1906, pp. 377-450, pls. 47-54.
DAVID WHITE. Permo-Carboniferous Climatic Changes in South America,
Jour. Geol., vol. 15, 1907, pp. 615-633.
Driftless and drift areas:—
T. C. CHAMBERLIN and R. D. SALISBURY. Preliminary Paper on the
Driftless Areas of the Upper Mississippi Valley, 6th Ann. Rept. U. S.
Geol. Surv., 1885, pp. 199-322, pls. 23-29.
R. D. SALISBURY. The Drift, its Characteristics and Relationships,
Jour. Geol., vol. 2, 1894, pp. 708-724, 837-851.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account