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Additional info for A Handbook of Asia Minor: Volume I. General: C.B. 847A

Sample text

By this time the river has taken a north-westerly trend and still further down the valley it bends west to join the northern branch. The upper reaches of the united river are known as the The stream now enters the mountains and its valley becomes gradually narrower and the sides steeper. Gereniz Chai. few tributaries. Before long it is A short distance below a swift current. with unfordable, In this stagci it receives PHYSICAL GEOGRAPHY 54 the right-bank village of Assar the river enters a narrow Some miles lower down it is swelled by an important This stream comes in on the tributary, the Karanfyl Chai.

The forest here is not light and scattered as in the Mediterranean region, but close, with large tree trunks and, in places, with a thick undergrowth of deciduous oaks. Generally spealdng, non-coniferous evergreens are unimportant. The predominating trees are a variety of pine and the beech. The whole region is essentially a wooded area, with large belts of virgin forest. (5) Lying between the areas already described and stretch- ing eastwards towards the central plateau is a region of rolling uplands and plains which may be described as an area of transition to the central plateau.

Passing be observed : beyond the Menavgat uniform alluvial plain, stoneless, and said to be largely under water in winter. There is no information regarding the height of this plain above sea-level, but it is not considerable. and marshy fiat in several places, 2. West of the Ak Su, this plain is dominated by a terrace with a sharply-marked perpendicular escarpment, which stands 100 ft. above the lower plain. This terrace forms a stony plateau, which extends from the sea to merge in the mountains to the north.

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A Handbook of Asia Minor: Volume I. General: C.B. 847A by Great Britain Admiralty

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