ountains. Just before entering the plains, the Helung
Kiang passes through one of its wildest gorges, a mere crevice between
vertical walls several hundred feet high. The road winds to the top of one
of the cliffs in zigzags cut in the solid rock. From the temple of Kitau
Kwan, which stands at the top of the cliff, there is a magnificent view of
the Plain, and no traveller would omit this, the most notable feature
between the valley of the Wei and Ch'eng-tu-fu. It is, moreover, the only
piece of level ground, of any extent, that is passed through between those
two regions, whichever road or track be taken. (_Richthofen_, MS. Notes.)

[In the _China Review_ (xiv. p. 358) Mr. E.H. Parker, has an article on
_Acbalec Manzi_, but does not throw any new light on the subject.--H.C.]

NOTE 2.--Polo's journey now continues through the lofty mountainous region
in the north of Sze-ch'wan.

The dividing range Ta-pa-shan is less in height than the T'sing-ling range,
but with gorges still more abrupt and deep; and it would be an entire
barrier to communication but for the care with which the road, here also,
has been formed. But this road, from Han-chung to Ch'eng-tu fu, is still
older than that to the north, having been constructed, it is said, in the
3rd century B.C. [See supra.] Before that time Sze-ch'wan was a closed
country, the only access from the north being the circuitous route down the
Han and up the Yang-tz'u. (Ibid.)

[Mr. G.G. Brown writes (_Jour. China Br. R. As. Soc._ xxviii. p. 53):
"Crossing the Ta-pa-shan from the valley of the Upper Han in Shen-si we
enter the province of Sze-ch'wan, and are now in a country as distinct as
possible from that that has been left. The climate which in the north was
at times almost Arctic, is now pluvial, and except on the summits of the
mountains no snow is to be seen. The people are ethnologically
different.... More even than the change of climate the geological aspect is
markedly different. The loess, which in Shen-si has settled like a pall
over the country, is here absent, and red sandstone rocks, filling the
valleys between the high-bounding and intermediate ridges of palaeozoic
formation, take its place. Sze-ch'wan is evidently a region of rivers
flowing in deeply eroded valleys, and as these find but one exit, the deep
gorges of Kwei-fu, their disposition takes the form of the innervations of
a leaf springing from a solitary stalk. The country between the branching
valleys i