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 · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high

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Page 1:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 2:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 3:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 4:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 5:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 6:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 7:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 8:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 9:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 10:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 11:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 12:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 13:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 14:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 15:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 16:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 17:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 18:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 19:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 20:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 21:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 22:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 23:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 24:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 25:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 26:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 27:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 28:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 29:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 30:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 31:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 32:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 33:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 34:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 35:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 36:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 37:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 38:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 39:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 40:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 41:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 42:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 43:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 44:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 45:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 46:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 47:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high
Page 48:  · somewhat less desertic than today (Scharlau, 1958). The differences might have been enough for the existence of large inland lakes where sandy or clay regions often with high

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