The above remarks apply more particularly to topographic maps.
Topographic belts of the state, in an irregular line running W.
The eastern boundary of the plains is more climatic than topographic. The line of 20 in.
Five topographic divisions of the island are fairly marked.
The most notable topographic feature is the roughly circular mountain area of north-eastern New York known as the Adirondack mountains (q.v.).
The Blue Ridge escarpment, a striking topographic feature in Virginia and the Carolinas, extends into Georgia along the north-eastern border of this belt, but is less strongly developed here than elsewhere, dying out entirely towards the south-west.
A topographic map (i: 126,000) embracing the whole of western Russia, with Poland and the country of the Don Cossacks, is designed to be extended over the whole empire.
Lupus, Topographic von Syrakus (Strassburg, 1887); P. Orsi, in Atti del congresso di scienze storiche, v.
Of the Catskills, although including only a small portion of the state, there are a number of different topographic features, due to the belts of different rock structure which cross the state from S.W.
This region presents no striking topographic features except the numerous small lakes which occupy the hollows created by the continental ice-sheet.
See the separate articles on the states, and also the following references: - Topographic maps and Geologic Folios of the United States Geological Survey; Bailey Willis, "The Northern Appalachians," and C. W.
The surface presents few striking topographic features, and may be subdivided into three vast plains or prairie tablelands rising one above the other from E.
The small triangular section of the coastal plain in New Jersey north of Delaware Bay deserves separate treatment because of the development there of a pectiliar topographic feature, which throws light on the occurrence of the islands off the New England coast, described in the next paragraph.
Subsequent erosion has changed the details of topography on an extensive scale, and subsequent deformative movements have renewed large topographic features where erosion had destroyed those developed by the close of the Miocene.
See Prahl, Chronika der Stadt Kiel (Kiel, 1856); Erichsen, Topographic des Landkreises Kiel (Kiel, 1898); H.
There are within the state four distinct topographic belts - the Appalachian, the Highlands, the Triassic Lowland and the Coastal Plain.
South-east of the Kittatinny Valley, and parallel with it, lies the second topographic belt, the Highlands.
The' four topographic belts of the state correspond very closely to the outcrops of its geological formations; the rocks of the Appalachian belt being of Palaeozoic age; the formation of the Highlands, Archaean; that of the Triassic Lowland, Triassic; that of the irregular hills of the Coastal Plain, Cretaceous and Tertiary.
This eastern tableland, though really very rugged and mountainous, seems to have few striking topographic features when compared with the more broken area to the W.
Gilbert, Geschichte and Topographic der Stadt Rom im Altertum (1883-1885); and ROME: Ancient History.
Four floral regions lying in north to south belts across the state, and closely corresponding to - though in boundaries by no means coinciding with - its great topographic divisions are distinguished in the regions of the Missouri border, the prairies, sand-hills and foot-hills.
The Great Basin is not, as its name implies, a topographic cup. Its surface is of varied character, with many independent closed basins draining into lakes or "playas," none of which, however, has outlet to the sea.
The results have been published on a scale of 1:25,000 (776 sheets, since 1866), 1:50,000 (Topographic and Military Map, 62 sheets, 1850-1864, and a Waterstaatskaart, 1864-1892), and 1:200,000 (Topographical Atlas, 21 sheets, 1868-1871).
During the current cycle of erosion, several of the faults, whose scarps had been worn away in the previous cycle, have been brought to light again as topographic features by the removal of the weak strata along one side of the fault line, leaving the harder strata on the other side in relief; such scarps are known as fault-line scarps, in distinction from the original fault scarps.