Carl Linnaeus, The Lapland Journey, translated by Peter Graves (Edinburgh: Lockharton Press, 1995), p. 32.

Uppland, 13/05/1732, ¶54:

The bank on the north side of the river is quite perpendicular and I was amazed that it could remain so clean cut. I perceived that this was because there was clay mixed in with the sand. It would not have been possible to make it any steeper even by artificial means. There were horizontal lines that appeared to mark how deep the water had cut down year by year.