834 THE GEOGRAPHICAL SIGNIFICANCE OF FLOODS. 



{27) Take, R. S. — [a] Hanging Valleys in the Finger Lake Region of 

 Central New York. American Geologist, xxxiii. 1904, pp. 271-291. 



(&) Lake Cayuga a Rock Basin. BnlL Geol. Soc. Am. v. 1S94, pp. 



339-356. 



(28) Taek, R. S. and Maktix, L. — (a) Glaciers and Glaciation of Yakutat 

 Bay, Alaska. Bull. Amer. Geog. Soc. xxxviii. 1906, pp. 145-167. 



(29) Turner, H. W.— The Pleistocene Geology of the South-Central Nevada, 

 with especial Reference to the Origin of Y'osemite Valley. Proc. Cal. 

 Acad. Sci. 3rd Series, Geology, i. 1900, pp. 261-321. 



(30) Westgate, Lewis G. — The Twin Lakes Glaciated Area, Colorado. 

 Journ. Geology, xiii. 1905, pp. 285-312. 



(31) WiLLCOx, OswiN W. — The Viscous versus the Granular Theory of 

 Glacial Motion. Quoted from Review in Geographical Journal, xxix. 

 1907, pp. 559-560. 



EXPLANATION OF PLATES XLIV-XLV. 



Plate xliv. 



The Junction of the Arthur and Cleddau Rivers, Milford Sound. Note 

 the wonderful undercutting as shown on the cliffs to the right hand of 

 picture. 



Plate xlv. 



Preservation Lilet. Glacial diffluences appear to be associated with 

 weak glacial corrasion, as evidenced by islands. Contrast with Plate xliv., 

 in which a marked caiion-conversence is shown. 



