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.
Heat waves blurred the dunes around them.
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.
Of Limassol, among sandy hills and sand-dunes, which perhaps explain its name in Greek (ti t aOos, sand).
End of the island is filled with sand dunes ranging in height from 50 to 75 ft.
Large areas of moving sands exist near Enotayevsk, where high dunes or barkhans have been formed.
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.
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 ~
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.
At the foot of the dunes are the old towns and villages of Sassenheim, close to which are slight remains of the ancient castle of Teilingen (12th century), in which the countess Jacoba of Bavaria died in 1433.
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.
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:
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.
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.
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.
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.
Operations On Land The contemporary military history of Europe included, first, the war between France and Spain, 1654-59, usually called the Spanish Fronde, of which the most notable incident was the great battle of the Dunes fought on the 14th of June 1658 between the French and English under Turenne and the Spaniards under Conde, in which a contingent of Cromwell's soldiers bore a conspicuous part.
Not far from the Kum-kol lakes there is a drift-sand area, though the dunes are stationary.
The great advance in the interpretation of land forms now makes it possible to introduce as thoroughly explanatory a description of these fertile plains as of forms earlier familiar, such as sand dunes, deltas and sea cliffs.
A wonderful series of these forms occurs in southern Utah, where in passing northward from the Carboniferous platform one ascends in succession the Vermilion Cliffs (Triassic sandstones), the ViThite Cliffs (Jurassic sandstones, of remarkably cross-bedded structure, interpreted the dunes of an ancient desert), and finally the Pink Cliffs (Eocene strata of fluviatile and lacustrine origin) of the high, forested plateaus.
Its coarser phases are closely associated with dunes in many places, and locally the bess makes a considerable part of the dune material.
This building, erected in the 15th century amid the barren dunes bordering the east shore of the estuary near its mouth, in place of a more ancient oratory, was long buried beneath drifts of sand.
Formed partly by alluvium carried down by perennial streams from the mountains of Lebanon and Galilee, and fringed by great sand-dunes which the sea throws up, Phoenicia is covered with a rich and fertile soil.
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.
In the depressions of the dunes and on' the geest grounds at their foot, small woods have been planted in places, and in this sheltered strip market-gardening and horticulture are practised.
The Y, which was formerly an inlet of the Zuider Zee, was drained, and the North Sea ship canal was formed in its stead (1865-1876), and carried through the dunes to Ymuiden.
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.
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.
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.
Above St Louis, pierces the dunes at flood time and reaches the sea, 50 m.
Cromwell furnished 6000 men with a fleet to join in the attack upon Spain in Flanders, and obtained as reward Mardyke and Dunkirk, the former being captured and handed over on the 3rd of October 1657, and the latter after the battle of the Dunes on the 4th of June 1658, when Cromwell's Ironsides were once more pitted against English royalists fighting for the Spaniards.
Plants of sand-dunes, whether in maritime or inland e.
Physically and physiologically dry habitats, with the accompanying plant communities of sand dunes and sandy heaths with little humus in the soil.
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.
Sand-dunes cover large tracts on the shores of the Baltic. No traces of marine deposits are found higher than loo or 150 ft.
To pass Cook Strait and land in the middle province of South Island is to pass from Portugal to Switzerland, a Switzerland, however, with a seacoast that in the east centre is a dull fringe of monotonous sand dunes or low cliffs.
Arcachon is situated on the southern border of the lagoon of Arcachon at the foot of dunes covered with splendid pine-woods.
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.
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.