The town stands on a sandy plain, and there are sand dunes within the city limits.
The moon peeked shyly over the dunes and moved searching fingers of dim light across the dunes.
When the ache had left her legs numb, and her breath was no longer coming in gasps, they started out again - across sand dunes - up and down.
The latter is fringed throughout its whole length by a chain of dunes, which rise in places to a height of nearly 200 ft.
In many places longitudinal dunes are found exceeding a day's journey in length, the valleys between which take three or four hours to cross; but the most striking feature of the Nafud are the high crescent-shaped sand-hills, known locally as falk or falj, described by Blunt and Huber, who devoted some time to their investigation.
For vei Lmple, the sand dunes of North America and those of western am rope are widely separated in geographical position and there- ge~ e in floristic composition, yet they are related by common rai:
Domburg is pleasantly situated at the foot of the dunes on the west side of the island, and in modern times has become a popular but primitive watering-place.
End of the island is filled with sand dunes ranging in height from 50 to 75 ft.
She watched the dunes anxiously for Bordeaux.
The sun turned the dunes orange red and then quickly sank, leaving them in pre-moon darkness.
Cassie followed, eyeing the dunes suspiciously.
His eyes constantly roved over the dunes and his rifle lay across his lap, ready for use.
Above St Louis, pierces the dunes at flood time and reaches the sea, 50 m.
Farther south-east, a line of sand dunes, covering the ruins of ancient villas, marks the coastline of the Roman period.
North of that river the coast is low-lying and bordered by sand-lunes, to which succeed on the Strait of Dover the cliffs in the neighborhood of the port of Boulogne and the marshes and sand-dunes of Flanders, with the ports of Calais and Dunkirk, the latter the principal French port on the NOrth Sea.
The tower of Notre Dame, dating from 1180, is a landmark across the dunes, and the church behind it, although a shell, merits inspection.
Thus, associ- 1~e] ions of Agropyrum (Triticum) junceum, of Carex arenaria, of ~ ~nmophila (Psamma) arenaria, and of other plants occur on sa rid dunes: the associations are related by the general identity ph the habitat conditions, namely, the physiological dryness f d the loose soil; but they are separated by differences in f~1
The whale avi of associations on the sand dunes constitutes a plant ~
In relation to the latter theory, it is pointed out that some markedly calcicole species occur on sand dunes; but this may be due to the lime which is frequently present in dune sand as well as to the physical dryness of the soil.
Consists of a narrow strip of low sand dunes, within which is a broad channel terminating to the E.
Off the west coast, which is very irregular, lie the islands of Riigen, Usedom and Wollin; the coast of Farther Pomerania is smooth in outline and is bordered with dunes, or sandbanks.
The natural division into dunes, geest grounds, and clay and low fen holds for South as well as for North Holland.
From the coast it is intercepted by a lone line of dunes, which it fails to pierce and is thus deflected southwards, flowing in this direction for nearly 170 m.
The chapel of Notre-Dame des Dunes possesses a small image, which is the object of a well-known pilgrimage.
In 1658 Turenne's victory of the Dunes gave it into the hands of the French and it was ceded to England.
South of this point the coast curves outwards and is broken by peninsulas and indentations; to the north it is concave and bordered in many places by dunes and lagoons.
They were built up by the gradual accumulation of mud deposits in a shallow bay, separated by dunes from the North Sea.
On the well-wooded fringe of the dunes on the west side of the island are the two villages of Renesse and Haamstede, the seats in former days of the two powerful lordships of the same name.
Owing to the great extent of the Nafud desert, the formation of sand-dunes is exemplified on a proportionate scale.
Though perhaps subject to slight changes in the course of years, there is no doubt that these dunes are practically permanent features; the more prominent ones serve as landmarks and have well-known distinctive names.
Of Limassol, among sandy hills and sand-dunes, which perhaps explain its name in Greek (ti t aOos, sand).
The coast-line extends in a double curve from south-west to northeast, and is formed by a row of sand dunes, 171 m.
In the north and south, however, this line is broken by the inlets of the sea which form the Frisian and the South Holland and Zeeland islands respectively; but the dunes themselves are found continued along the seaward side of these islands, thus indicating the original continuity of the coast-line.
The breadth of the dunes naturally varies greatly, the maximum width of about 4375 Yds.
The steepness of the dunes on the side towards the sea is caused by the continual erosion, probably traceable, in part at least, to the channel current (which at mean tide has a velocity of 14 or 15 in.
This alteration of coast-line appears at Loosduinen, where the moor or fenland formerly developed behind the dunes now crops out on the shore amid the sand, being pressed to the compactness of lignite by the weight of the sand drifted over it.
Again, the remains of the Roman camp Brittenburg or Huis to Britten, which originally lay within the dunes and, after being covered by them, emerged again in 1520, were, in 1694, 1600 paces out to sea, opposite Katwijk; while, besides Katwijk itself, several other villages of the west coast, as Domburg, Scheveningen, Egmond, have been removed further inland.
The tendency of the dunes to drift off on the landward side is prevented by the planting of bent-grass (Arundo arenaria), whose long roots serve to bind the sand together.
Westerland, one of the most frequented sea-bathing places of Germany, lies on the west side of the island, separated from the sea, which is seldom perfectly calm, by a chain of sand dunes, across which board walks lead to the beach.
Two miles north of this place along the dunes is Zeebrugge, the point at which the new ship-canal from Bruges enters the North Sea.
There are three natural divisions - foreshore and sand-dunes, inner dunes and the geest grounds, and low fens and clay lands.
The dunes form the great natural barrier against the sea behind which the province lies secure.