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Encyclopedia Britannica



CHILTERN HILLS, or THE CHILTERNS

This article appears in Volume V06, Page 163 of the Encyclopedia Britannica.

Encyclopedia Britannica - Main :: CHA-CHR
CHILTERN HILLS, or THE CHILTERNS , a range of chalk hills in England, extending through part of Oxfordshire, Buckinghamshire and Bedfordshire. Running from S.W. to N.E., they form a well-marked escarpment north-westward, while the
south
 -eastern slope is long. The name of Chilterns is applied to the hills between the Thames in the neighbourhood of Goring161
and the headwaters of its tributary the Lea between Dunstable and Hitchin, the crest line between these points being about 55 M. in length. But these hills are part of a larger chalk system, continuing the line of the White Horse Hills from Berkshire, and themselves continued eastward by the
East
  Anglian
ridge
 . The greatest
elevation
  of the Chilterns is found in the centre from Watlington to Tring, where heights from 8oc o 85o ft. are frequent. Westward towards the Thames gap the
elevation
  falls away but little, but eastward the
East
  Anglian
ridge
  does not often exceed 500 ft., though it continues the northward escarpment across
Hertfordshire
 . There are several passes through the Chilterns, followed by main roads and railways converging on London, which lies in the basin of which these hills form part of the northern rim. The most remarkable passes are those near Tring, Wendover and Prince's Risborough, the floors of which are occupied by the gravels of former rivers. The Chilterns were formerly covered with a forest of beech, and there is still a local
supply
  of this
wood
  for the manufacture of chairs and other articles in the neighbourhood of Wycombe.


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