23) that not Soult's corps alone, but three French corps, had come through the pass of Banos without opposition; that Soult himself was at Naval Moral, between him and the bridge of Almaraz on the Tagus, and that Cuesta was retreating from Talavera.
Victor had crossed the Tagus, and defeated Cuesta at Medellin (March 28, 1809); but, surrounded by insurgents, he also had halted; Lapisse had joined him, and together they were near Merida, 30,000 strong.
News having been received that Napoleon had suffered a serious check at the battle of Aspern, near Vienna (May 22, 1809), Wellesley next determined - leaving Beresford (20,000) near Ciudad Rodrigo - to move with 22,000 men, in conjunction with Cuesta's Spanish army (40,000) towards Madrid against Victor, who, with 25,000 supported by King Joseph (50,000) covering the capital, was near Talavera.
Cuesta, during the advance up the valley of the Tagus, was to occupy the pass of Banos on the left flank; the Spanish authorities were to supply provisions, and Venegas was to be at Arganda, near Madrid, by the 22nd or 23rd of July; but none of these arrangements were duly carried out, and it was on this that the remainder of the campaign turned.
By the 10th of July Cuesta had joined Wellesley at Oropesa;, and both then moved forward to Talavera, Victor falling back before them: but Cuesta, irritable and jealous, Battle of would not work cordially with Wellesley; Venegas - Talavera, counter-ordered it is said by the Spanish junta - did July 27, 28, not go to Arganda, and Wilson, though he advanced 1809.
28); the old forces of Venegas and Cuesta (50,000), now united under Areizaga, were decisively routed by King Joseph at Ocana (Nov.19); and Gerona after a gallant defence, had surrendered to Augereau (Dec. 10).
Figueras surrendered to Cuesta before the end of May; and peace was formally signed at Paris on the 30th of May.
overlooking the inner lowland in a well-defined slope dissected by many inland-flowing streams, and descending from its broad crest very gently seaward, thus giving ri~e to what has been called a belted coastal plain, in which the relief is arranged longitudinally and the upland member, with its very unsymmetrical slopes, has sometimes been called a cuesta.
This is a ferm of relief frequently occurring elsewhere, as in the Niagara cuesta of the Great Lake district of the northern United States and in the Cotswold and Chiltern hills of England, typical examples of the cuesta class.
There is good reason for believing that at least along the southern border of New England a narrow coastal plain was for a time added to the continental border; and that, as in the New Jersey section the plain was here stripped from a significant breadth of inland overlap and worn down so as to form an inner lowland enclosed by a longitudinal upland or cuesta; and that when this stage was reached a submergence, of the kind which has produced the many embayments of the New England coast, drowned the outer part of thy plain and the inner lowland, leaving only the higher parts of the cuesta as islands.
Heavy terminal moraines and outwashed fluviatile plains have been laid on the cuesta remnants, increasing their height as much as 100 ft.
The chief upland belt or cuesta is formed by the firm Niagara limestone, which takes its name from the gorge and falls cut through the upland by the Niagara river.
As in all such forms, the Niagara cuesta has a relatively strong slope or infacing escarpment on the side towards the oldland, and a long gentle slope on the other side.
The cuesta would be straight from east and west if the slant of the strata were uniformly to the south; but the strata are somewhat warped, and hence the course of the cuesta is strongly convex to the north in the middle, gently convex to the south at either end.
The cuesta begins where its determining limcstone begins, in west-central New York; there it separates the lowlands that contain the basins of lakes Ontario and Erie; thence it curves to the north-west through the province of Ontario to the belt of islands that divide1 Georgian Bay from Lake Huron; then westward throtigh the land-arm between lakes Superior and Michigan, and south-westward into the narrow points that divide Green Bay from Lake Michigan, and at last westward to fade away again with the thinning out of the limestone; it is hardly traceable across the Mississippi river.
The arrangement of the Great Lakes is thus seen to he closely synipathetic with the course of the lowlands worn on the two belts of weaker strata on either side of the Niagara cuesta; Ontario, Georgian Bay and Green Bay occupy depressions in the lowland on the inner side of the cuesta; Erie, Huron and Michigan lie in depressions in the lowland on the outer side.
The occurrence of the lake basins in the lowland belts on either side of the Niagara cuesta is an abnormal feature, not to be explained by ordinary erosion, which can produce only valleys.
The most significant stage in this series of changes occurred when the glacio-marginal lake wateis were lowered so that the long cuesta of Niagara limestone was laid bare in western New York; the previously confluent waters were then divided into two lakes; the higher one, Erie, supplying the outfiowing Niagara river, which poured its waters down the escarpment of the cuesta to the lower lake, Ontario, whose outlet for a time ran down the Mohawk Valley to the Hudson: thus Niagara falls began.
The lowland is enclosed by an upland or cuesta, known as Chunnenugga Ridge, sustained by partly consolidated sandy strata; the upland, however, is not continuous, and hence should be described as a maturely dissected cuesta.
In the embayment of the coastal plain some low cuesta-like belts of hills with associated strips of lowlands suggest the features of a beltedcoastal plain; the hillybeltordissected cuesta determined by the Grand Gulf formation in western Mississippi is the most distinct.
in area, enclosed by bluffs one or two hundred feet high in the northern part, generally decreasing to the southward, but with local increase of height associated with a decrease in flood plain breadth on the eastern side where the Grand Gulf cuesta is traversed.
An inland extension from the coastal plain in north-central Texas leads to a large cuesta known as Grand Prairie (not structurally included in the coastal plain), upheld at altitudes of 1200 or 1300 ft.
to a mile) is dissected by many branching consequent streams; in its southernpart, as it ap~iroaches the Colorado river the cuesta is dissected into a belt of discontinuous hills.
The western cross timbers follow a sandy belt along the inner base of the ragged escarpment of Grand Prairie; the eastern cross timbers follow another sandy belt in the lowland between the eastern~ slope of Grand Prairie and the pale western escarpment of the next eastward and lower Black Prairie cuesta.
This cuesta is supported at an altitude of 700 ft.
Then comes the East Texas timber belt, broad in the north-east, narrowing to a point before reaching the Rio Grande, a low and thoroughly dissected cuesta of sandy Eocene strata; and this is followed by the Coast Prairie, a very young plain, with a seaward slope of less than 2 ft.
Near the Colorado river the dissected cuesta of the Grand Prairie passes southward, by a change to a more nearly horizontal structure, into the dissected Edwards plateau (to be referred to again as part of the Great Plains), which terminates in a maturely dissected fault scarp, 300 or 400 ft.
high, overlooking the central denuded area of that state; and there, between the Brazos and Colorado rivers, occurs a series of isolated outliers capped by a limestone which underlies both the Llano on the west and the Grand Prairies cuesta on the east.
He had the support of a Spanish army under General Cuesta; but his movements were delayed by the neglect of the Spanish government, and Soult was able to collect a large force for the purpose of falling upon the English line of communication.
13,000 Pie de Cuesta (Santander).
The eastern elevation is a ridge or cuesta formed by an outcropping hard layer of the ancient coastal plain; and it separates the Wisconsin river basin from the Fox River Valley and the streams flowing into Lake Michigan.
a rocky limestone ridge or cuesta some 30 m.
Westward from the Lower Tennessee river the surface of the East Gulf Coastal Plain rises rapidly to the summit of a broken cuesta or ridge and then descends gently and terminates abruptly in a bluff overlooking the Mississippi Flood Plain.
cuesta el libro azul?
The famous and stunningly beautiful Hearst Castle is part of the Hearst San Simeon State Historical Monument and is also known as La Cuesta Encantada, The Enchanted Hill, and America's Castle.
The word usage examples above have been gathered from various sources to reflect current and historial usage. They do not represent the opinions of YourDictionary.com.