COAST RECORDS OF THE RISE OR FALL OF LAND 259 



notched cliff or the double sea arch may appear in the landscape. 

 Upon a submerged coast the most significant lines in the view 

 are those of the rock islet and the steep-walled fjord. 



SUBSIDENCE: 



A IM O 



LATER ELEVATION. 



o use i DEMO c. 



FIG. 290. Character profiles in coast landscapes where there has been either 

 elevation or depression. 



READING REFERENCES FOR CHAPTER XIX 

 General : 



SIR CH. LYELL. Principles of Geology, vol. 2, pp. 180-197. 

 ED. SUESS. The Face of the Earth, Clarendon Press, Oxford, 1906, vol. 



2, Chapters i and xiv, pp. 1-29, 535-556. 



ROBERT SIEGER. Seenschwankungen und Strandverschiebungen in Scan- 

 dinavien, Zeit. d. Gesell. f. Erdk., Berlin, vol. 28, 1893, pp. 1-106, 

 393-688, pi. 7. 



Elevated shore lines : 

 F. B. TAYLOR. The Highest Old Shore Line of Mackinac Island, Am. 



Jour. Sci., vol. 43, 1892, pp. 210-218. 

 THOMAS L. WATSON. Evidences of Recent Elevation of the Southern 



Coast of Baffins Land, Jour. GeoL, vol. 5, 1897, pp. 17-33. 

 J. W. GOLDTHWAIT. The Abandoned Shore Lines of Eastern Wisconsin. 



Bull. 17, Wis. Geol. and Nat. Hist. Surv., 1907, pp. 134, pis. 1-37. 



Evidences of depression : 



W. B. SCOTT. Introduction to Geology, New York, 1907, pp. 33-36. 

 W J McGEE. The Gulf of Mexico as a Measure of Isostaoy, Am. 

 Jour. Sci. (3), vol. 44, 1892, pp. 177-192. 



