The Craven fault, for instance, extends for upward of thirty miles, and along this line the vertical displacement of the strata varies from 600 to 3,000 feet.
Craven-en faila, adibidez, 30 miliatik gora hedatzen da, eta lerro honetan zehar dauden estratuen mugimendu bertikala 600 oinetik 3.000ra doa.