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that low relief was dissected during the following three uplifts with their erosion
cycles. It is gratifying to find corroboration of this threefold division of uplift
in the structural deformations of plain-deposits derived therefrom. There are
three rows of uptilted piedmonts ranging parallel to the Alai Mountains, as the
three respective marginal deformations corresponding to the threefold uplift
both in magnitude and degree of subsequent erosion. It is further interesting
to find that these three belts of uplifted piedmont, which converge towards the
mountains opposite Khokand, near the western or lower end of the basin, widen
eastward to include a considerable area of the eastern end of the plains, where
deposition has necessarily been much heavier, as that portion lies before a vast
mass of high-uplifted mountains. Another feature affected by this process and
characteristic of the Fergana plains, especially on their Alai side, is the threefold,
and sometimes fourfold, division of distributary systems. Larger streams descend-
ing from the Alai cross all three belts of uptilted piedmont, having cut down as
they were uplifted, and apportion their depositions over areas between them,
some escaping beyond the last to spread towards the middle of the basin. Each
stream, therefore, gives rise to from two to four successive groups of delta-oases,
thus giving an interesting variation of type I a of my classification. In several
instances a stream escapes from its first delta in two or more distributaries to
form other deltas beyond, so that the intervening uplifted ridge of piedmont has
been dissected by two or more channels separated by many miles (fig. 465).

The oldest belt of uptilted piedmonts bordering the Alai Mountains probably
contains products of the first erosion cycle and was thus upheaved during the
uplift which caused the breaking up of its peneplain stage. On the Terek trail
between Osh and Gulcha it attains a height of over 3,000 feet above the present
Gulcha River flood-plain. There it is a mass of loosely cemented conglomerates
with confused dips, and of which the old surmounting piedmont topography has
nearly disappeared. The later upheavals of plain-deposits rarely rise more than
a few hundred feet above present deposition.

Where we approached the northern margin of the Fergana plains in the regions
of Chust and Khojent, only one belt of uptilted piedmont was observed, probably
because the mountains on that side are much lower and doubtless have been so
in the past. This one belt, however, is of especial interest as it can be traced
all the way from Namangan to Khojent, a distance of about 140 miles, and crosses
the Syr Darya, which has cut down as it was uplifted.

From the standpoint of hydrography alone, the Fergana basin expresses
the same series of cyclical events deduced from the topography and structure
of its mountains and plains. In the mountains larger streams join at oblique
angles and generally inherit the courses held before the first uplift of the low
relief then drained by them. Their smaller tributaries contrast with this rule
by joining the larger nearly at right angles and have come to be since that uplift.
We have seen how streams descending from the Alai split into distributary systems
in a manner determined by the marginal deformations of the plains and that
feature may be recognized with a glance at the hydrography on a large-scale
Russian map.