hollow, in a beautiful wheat-ground, enclosed on all sides by slightly ascending and fertile heights. This cloister also possesses settlements in the neighbouring districts. The soil is decomposed slate clay. The marl which is found in this mineral formation, and which, as yet undecomposed, slowly crumbles, makes the earth loose and extremely fertile. The land continues to rise until you come to Tirschenreuth, and the waters flow against you, to fall into the Egra and the Elbe. From Tirschenreuth it descends southwards, and the streams run toward the Danube. I can very rapidly form an idea of a country as soon as I know by examination which way even the least brook runs, and can determine the river to whose basin it belongs. By this means, even in those districts of which it is impossible to take a survey, one can, in thought, form a connection between lines of mountains and valleys. From the last-mentioned place begins an excellent road formed of granite. A better one cannot be conceived; for, as the decomposed granite consists of gravelly and argillaceous earths, they bind excellently together, and form a solid foundation, so as to make a road as smooth as a threshing-floor. The country through which it runs looks so much the worse: it also consists of a granite-sand, lies very flat and marshy, and the excellent road is all the more desirable. And as, moreover, the roads descend gradually from this plane, one gets on with a rapidity that strikingly contrasts with the general snail's pace of Bohemian travelling. The enclosed billet will give you the names of the different stages. Suffice it to say, that, on the second morning, I was at Ratisbon; and so I did these twenty-four miles[1] and a half in thirty-nine hours. As the day
- ↑ A German mile is exactly equal to four English geographical, and to rather more than four and a quarter ordinary miles. The distance in the text may therefore be roughly set down as one hundred and four miles English.—A. J. W. M.
