They are peculiar in having their altitude dependent on the depth of revived erosion, instead of the amount of faulting, and they are sometimes topographically reversed, in that the revived scarp overlooks a lowland worn on a weak formation in the upheaved fault-block.
The northern part of the western side of the anticline is broken off by a great fault in the valley of the Eden, and the scarp thus formed is rendered more abrupt by the presence of a sheet of intrusive basalt.
Faulting, probably in Pliocene times, lowered the basaltic plateaus to form the basin of Lough Neagh, leaving the eastern scarp at heights ranging up to 1800 ft.
The Lower Lias appears at intervals under the scarp of the basaltic plateaus, and contributes, as in Dorsetshire and Devonshire, to the formation of landslips along the coast.
Such broken material rolling down a uniform scarp would tend to reduce its steepness by the loss of material in the upper part and by the accumulation of a mound or scree against the loti ii er part of the slope.
The western scarp of the acropolis has been sculptured into a number of sepulchres imitating wooden houses with pillared facades, some of which have pediment reliefs and inscriptions in Lycian.
The latter was defended on the north and east by the sea, on the west by a long straight cutting of the rock serving as a scarp on which the wall stood (see below), and on the south by extensive quarries (Freeman ii.
Einseitige Schollengebirge oder Schollenrandgebirge- Scarp or tilted block mountains.
The scarp or steeply inclined slope; this is necessarily of small extent except in the direction of its length.