Page:Transactions of the Geological Society, 1st series, vol. 4.djvu/100

 of the Lead-mine district, that I have given the account of them under a separate section. This part of the country has been explored for coal by Mr. Buddle, and it is chiefly from his pamphlet that I have derived the following information.

In the vicinity of Wark, 15 miles south-west of Tweedmouth, the beds consist of marl, micaceous sandstone, and slate-clay; and about a quarter of a mile below Coldstream, in the north bank of the river, the strata are

These measures dip to the east at an angle of 5 or 6 degrees.

At Lenel quarry, half a mile below Coldstream on the northern bank of the Tweed, the strata are,

At Bingham or Spring-Hill, north of the Tweed, the following is the order of the strata.