Kitson's work in Tasmania shows that there also the glacial beds may be correlated with the lower or Greta Coal Measures of New South Wales.
One of the richest has been found at Greta in the Hunter river district; it contains an average thickness of 41 ft.
Borrowdale is joined on the east by the bare wild dale of Langstrath, and the Greta joins the Derwent immediately below Derwentwater; the town of Keswick lying near the junction.
In 1803 Southey became a joint lodger with Coleridge at Greta Hall, Keswick, of which in 1812 Southey became sole tenant and occupier.
Lower or Greta Coal Measures, containing an aggregate of about 20 ft.
In the vicinity of the town are Egglestone Abbey, beautifully situated on the Yorkshire bank of the river, Rokeby Park on the same bank, at the confluence of the Greta, and the massive 14th century castle of Raby to the north-east.
The Coal Measures are covered by marine shales with numerous bryozoa; and, on the horizon of the Greta Coal Measures of New South Wales, is a bed of Carboniferous glacial deposits.