No CrossRef data available.
We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.
Published online by Cambridge University Press: 01 May 2009
The general question of the rise of older rocks beneath the Cretaceous beds of south-eastern England is now so familiar to geologists that there is no need to discuss it here: it is enough to note that the Secondary beds (beneath the Gault) thin northward, for many miles, from the axis of the Weald. The practical application of our knowledge of the subject is however in its infancy, and our knowledge stops short at the Wealden axis; for we do not know what happens south of it.
A paper read to the Brit. Assoc. at Leeds, and printed in the Yorkshire Post (and other newspapers), and in the Brighton Magazine (October, 1890). Some slight additions and corrections are now made.
1 A paper read to the Brit. Assoc. at Leeds, and printed in the Yorkshire Post (and other newspapers), and in the Brighton Magazine (October, 1890). Some slight additions and corrections are now made.