6 ([return])
[ Darwin, "Voyage of the Beagle," chapter 14, and a much fuller account in the same author's "Geological Observations on the Volcanic Islands and Parts of South America Visited during the Voyage of H.M.S. Beagle," chapter 9.]
7 ([return])
[ For a full discussion of the evidence for and against continental elevation and subsidence in general, and as affecting the British Isles and Scandinavia in particular, see Sir A. Geikie's Presidential Address to the Geological Society for 1904 (" Proceedings of the Geological Society"' volume 60, 1904, pages 80 to 104.). Here it is shown that the oldest raised beaches of Scotland are pre-glacial, and the same also holds for the south of Ireland.]
8 ([return])
[ The argument here employed is fallacious, since the mere existence of a distinct beach implies a pause in the movement and a long continuance at one level. It is impossible to form any estimate of the lapse of time necessary for the building up of a beach-terrace. We can only, in some cases, obtain a measure of the time that elapsed between the formation of two successive beaches, as in this instance.]
9 ([return])
[ The "strand lines," or raised beaches of Norway, have given rise to much discussion, of which a summary will be found in the address cited in Note 7.]
10 ([return])
[ A considerable number of skulls and skeletons of the Neanderthal type have now been found in different parts of Southern Europe, extending from Belgium to Gibraltar and Croatia, and it is now known that this type of skull is associated with flint implements of Mousterian Age. (See Note 12.)]