268 PHYSIOGRAPHY OF CENTRAL-ASIAN- DESERTS AND OASES. 
and there with low monadnocks and bordered by the Alai and Peter-the-Great 
Range. But to attain even that stage of maturity in the heart of a great moun- 
tain region; to erode what in Pliocene time must have been a region of colossal 
ranges to its metamorphic cores, must have taken vastly longer than all three suc- 
ceeding cycles of erosion taken together. The sum total of these later cycles has 
resulted in no more than an immature dissection of the ancient topography, 
and, though for our purpose they should be termed erosion cycles, they are by 
no means comparable to that which closed the Pliocene and should be regarded as 
mere phases of a Quaternary striving towards base-level. We shall find corre- 
sponding phases of Quaternary erosion over other regions and term them cycles 
for the sake of a tentative correlation. 

Fig. 445.—A Bridge over the Third-cycle Terrace in Karategin. 
Terraces of the second stage lie about half-way up the valley sides, but are 
found only at rare intervals, usually where tributaries join, and badly preserved 
because the third-stage valley-floor has widened to nearly obliterate the transition. 
But those of the third stage are in remarkable preservation and form the great 
feature of Karategin, the spacious plains and gentle slopes of its oases. Broadly 
speaking, it gives a concave sweep to the valley bottom, for the most part 4 miles 
across and traversed by the present river channel, about half a mile wide, of rec- 
tangular section, varying up to nearly 300 feet in depth. 
At Damburachi (junction with the Muk Su), this stage widens into a trian- 
gular junction-terrace* of over 30 square miles area, traversed by abandoned 
distributary channels of the Muk Su between 200 and 300 feet above stream. Two 

*A terrace in the angle or junction-spur where two rivers join. I venture to offer ‘‘junction-terrace”’ 
and ‘‘junction-spur” as terms I have found essential. 
