Serra sentence example

serra
  • Monchiquite (Ria do Ouro, Serra de Tingua).
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  • Ranges of these chapadas form the boundary lines with three states - the Serras dos Irmaos and Vermelha with Piauhy, the Serra do Araripe with Ceara., and the Serra dos Cariris Velhos with Parahyba.
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  • The general elevation of the plateau is estimated to be about 2700 ft., and the highest elevation was reported in 1892 to be the Serra dos Pyreneos (5250 ft.).
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  • The capital of the state is GoYAz, or Villa-Boa de Goyaz, a mining town on the Rio Vermelho, a tributary of the Araguaya rising on the northern slopes of the Serra de Santa Rita.
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  • Most of the wooded district south of the Mantiqueira belongs to the states of Sao Paulo and Rio de Janeiro, but east of the Espinhago it belongs to Minas Geraes and extends eastward to the Serra das Aymores, on the frontier of Espirito Santo.
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  • The tributaries of the Rio Doce cover the slopes of the Serra do Espinhago for a distance north and south of about 200 m.
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  • On the western frontier a northern extension of the great central chain of Goyaz forms the water-parting between the drainage basins of the Sao Francisco and Tocantins, and is known at different points as the Serra do Paranan, Serra de Sao Domingos and Serra das Divisoes.
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  • South-east of this chain, between the headwaters of the Parana and Sao Francisco, are the Serra da Canastra and Serra da Matta da Corde, an irregular chain of moderate elevation running north and south.
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  • The highest elevations in the state, so far as known, are Itatiaya (8898 ft.) in the Serra da Mantiqueira, and Caraga (6414 ft.), near Ouro Preto, in the Serra do Espinhago.
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  • The latter rises on the western slopes of the Serra da Matta da Corde, and one of its northern tributaries has its source in a "knot" of the Serra dos Pyreneos, from which streams flow eastward to the Sao Francisco and northward to the Tocantins.
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  • Its source is in the Serra da Canastra, and its general course across the state is north by east, during which it receives the Paracatu, Urucuia, Pardo and Carinhanha from the west and the Verde Grande and das Velhas from the east.
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  • The city is built upon the lower slope of the Serra do Ouro Preto, a spur of the Espinhago, deeply cut by ravines and divided into a number of irregular hills, up which the narrow, crooked streets are built and upon which groups of low, old-fashioned houses form each a separate nucleus.
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  • The Mau5, railway was opened to the foot of the serra (Raiz da Serra) in 1854, and the macadamized road up the serra to the town in 1856.
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  • The most northerly point, the Serra Roraima on the Venezuela and British Guiana frontier (5° 10' N.), is 56 m.
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  • On the 9th of December 1905 protocols were signed at Caracas accepting the line between Cucuhy and the Serra Cupuy located in 1880, and referring the remainder, which had been located by a Brazilian commission in 1882 and 1884, to a mixed commission for verification.
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  • Running north-east and south-east to enclose the sources of the Rio Paru, it unites with the French Guiana line at 2° 10' N., 55° W., and thence runs easterly along the water-parting of the Serra Tumuc-Humac to the source of the Oyapok, which river is the divisional line to the Atlantic coast.
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  • The first consists of an almost continuous range crossing the northern end of Rio Grande do Sul and following the coast northward to the vicinity of Cape Frio, and thence northward in broken ranges to the vicinity of Cape St Roque, and a second parallel range running from eastern Sao Paulo northeast and north to the eastern margin of the Sao Francisco basin in northern Bahia, where that river turns eastward to the Atlantic. The first of these is generally known as the Serra do Mar, or Coast Range, though it is locally known under many names.
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  • Its culminating point is in the Organ Mountains (Serra dos Orgaos), near Rio de Janeiro, which reaches an elevation of 7323 ft.
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  • The inland range, which is separated from the Coast Range in the vicinity of Rio de Janeiro by the valley of the Parahyba do Sul river, is known as the Serra da Mantiqueira, and from the point where it turns northward to form the eastern rim of the Sao Francisco basin, as the Serra do Espinhaco.
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  • North of Cape Frio the Coast Range is much broken and less elevated, while the Serra do Espinhaco takes a more inland course and is separated from the coast by great gently-sloping, semi-barren terraces.
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  • The eastern range of this central system, which crosses western Minas Geraes from the so-called Serra das Vertentes to the valley of the Paracatu, a western tributary of the Sao Francisco, is called the Serra da Canastra and Serra da Matta da Corde.
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  • Its culminating point is toward its southern extremity in the Serra da Canastra, 4206 ft.
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  • There remains only the elevated valley of the Parahyba do Sul, lying between the so-called Serra das Vertentes of southern Minas Geraes and the Serra do Mar, and extending from the Serra da Bocaina, near the city of Sao Paulo, eastward to Cape Frio and the coastal plain north of that point.
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  • It is traversed by two mountain chains, the Serra da Mantiqueira and Serra do Mar, and the broad, fertile valley of the Parahyba do Sul which lies between them, and which slopes gently toward the east from a general elevation exceeding 2000 ft.
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  • Their character is also determined by the distance of the Serra do Mar from the coast, the more southern rivers having short precipitous courses.
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  • North of the Sao Francisco the watershed projecting from the plateau eastward toward Cape St Roque, known as the Serra da Borborema in Parahyba and Rio Grande do Norte where its direction becomes north-east, leaves a triangular section of the easterly slope in which the river courses are short and much broken by rapids.
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  • South of Cape Frio there are no large rivers along the coast because of the proximity of the Serra do Mar - the coastal plain being very narrow and in places disappearing altogether.
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  • The largest of these and the only one of commercial value is the Ribeira de Iguape, which has its source on the tablelands of Parana and after receiving several affluents west of the Serra do Mar breaks through a depression in that range and discharges into the Atlantic"some miles below Santos on the southern boundary of the state of Sao Paulo.
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  • Those of the Paraguay drain the south-western part of Matto Grosso, and the tributaries of the Parana cover the western slopes of the Serra do Mar from Rio Grande do Sul north to the south-west part of Minas Geraes, and include the south-east part of Matto Grosso and the south part of Goyaz within their drainage basin.
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  • In the Parahyba valley, which extends across the state of Rio de Janeiro, the mean temperature is somewhat higher than it is in Sao Paulo and Minas Geraes, and the nights are warmer, but the higher valleys of the Serra do Mar enjoy a delightfully temperate climate.
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  • The surrounding region, lying on the eastern slopes of one of the lateral ranges of the Serra do Espinhaco, is rough and barren, but.
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  • The principal exception is the Zatas or Sorraia, which, rising in the Serra d'Ossa, flows westwards across the plateau of Alemtejo, and joins the Mar de Pedro.
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  • A presidio (Spanish military post) was established here in 1782, and a Franciscan mission, by Junipero Serra, about four years later.
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  • The western border of the state is traversed by low ranges of mountains forming a northward continuation of the Serra do Mar.
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  • The longest and most prominent of these ranges, which are for the most part the eastern escarpments of the great Brazilian plateau, is the Serra dos Aymores, which extends along fully two-thirds of the western frontier.
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  • East of the Sao Francisco it may be divided into three distinct regions: a rough limestone plateau rising gradually to the culminating ridges of the Serra da Chapada; a gneissose plateau showing extensive exposures of bare rock dipping slightly toward the coast; and a narrower plateau covered with a compact sandy soil descending to the coastal plain.
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  • The water supply is derived from three sources: the small streams flowing down the mountain sides which serve small localities; the old Carioca aqueduct, dating from colonial times, which collects a considerable supply from the small streams of the Serra da Carioca and brings it into the city through a covered conduit which once crossed the gap between Santa Thereza and Santo Antonio hills on two ranges of stone arches (now used as a viaduct by the Santa Thereza Tramway Company); and the modern Rio do Ouro waterworks, which brings in an abundant supply from the Serra do Tinqua, N.W.
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  • There is daily communication with Petropolis by a branch line of the Leopoldina system, and also by a steamer to the head of the bay and thence by rail up the serra.
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  • The diamond here occurs in river gravels and sands associated with the same minerals as in Minas Geraes; since 1844 the richest mines have been worked in the Serra de Cincora, where the mountains are intersected by the river Paraguassu and its tributaries; it is said that there were as many as 20,000 miners working here in 1845, and it was estimated that 54,000 carats were produced in Bahia in 1858.
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  • The earlier workings were in the Serra de Chapada to the N.W.
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  • Among more general works are Brequigny, Histoire des revolutions de Genes 'usqu'en 1748; Serra, La Storia dell' antica Liguria e di Genova (Turin, 1834) Varesi, Storia della repubblica di Genova sino al 1814 (Genoa, 18 351839); Canale, Storia dei Genovesi (Genoa, 1844-1854), Nuova istoria della repubblica di Genova (Florence, 1858), and Storia della rep. di Genova dall' anno 1528 al 1550 (Genoa, 1874); Blumenthal, Zur Verfassungsand Verwaltungsgeschichte Genua's im 12ten Jahrhundert (Kalbe an der Saalc, 1872); Mallison, Studies from Genoese History (London, 1875).
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  • The leader in this movement was a really remarkable man, Miguel Jose Serra (known as Junipero Serra, 1713-1784), a friar of very great ability, purest piety, and tireless zeal.
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  • The boundary line with Piauhy follows one of these ranges, the Serra de Ibiapaba, which unites with another range on the southern boundary of the state, known as the Serra do Araripe.
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  • Its principal affluent is the Rio das Mortes, which rises in the Serra de Sao Jeronymo, near Cuyaba, Matto Grosso, and is utilized by boatmen going to Para.
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  • The bleak and desolate heights of the Serra da Estrella and the ranges of the northern frontier are almost alpine in character, although they nowhere reach the limit of perpetual snow.
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  • The following ranges belong to the Transmontane system, which is the southern extension of the mountains of Galicia: Peneda (4728 ft.), forming the watershed between the river Lima and the lower Minho; the Serra do Gerez (4817 ft.), which rises like a gigantic wall between the Lima and the Homem, and sends off a spur known as the Amarella, Oural and Nora, south-westward between the Homem and the Cavado; La Raya Seca, a continuation of Gerez, which culminates in Larouco (4390 ft.) and contains the sources of the Cavado; Cabreira (4196 ft.), which contains the sources of the river Ave and separates the basin of the Tamega from that of the Cavado; Marao (4642 ft.), Villarelho (3547 ft.) and Padrella (3763 ft.), forming together a large massif between the rivers Tamega, Tua and Douro; and Nogueira (4331 ft.) and Bornes (3944 ft.), which divide the valley of the Tua from that of the Sabor.
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  • North of the Mondego it includes Montemuro (4534 ft.), separating the Douro from the upper waters of its left-hand tributary the Paiva; Gralheira (3681 ft.) between the Paiva and the Vouga; the Serra do Caramullo (35 11 ft.), between the Vouga and the Dao; and the Serra da Lapa (3215 ft.), which gives rise to the Paiva, Tavora, Vouga and ado.
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  • South of these ranges, but nominally included in the same system, is the Serra da Estrella, the loftiest ridge in Portugal (6532 ft.).
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  • The Estrella Mountains, which enclose the headwaters of the Mondego in a deep ravine, stretch from north-east to south-west and are continued in the same direction by the Serra de Lousa (3944 ft.).
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  • The greater part of the Serra da Estrella constitutes the watershed between the Mondego and Zezere.
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  • Lesser ranges, which are included in the Beirene system and vary in height from 2000 to 4000 ft., are the Mesas, between the rivers Coa and Zezere; the Guardunha and Moradal, separating the Zezere from the Ponsul and Ocreza, tributaries of the Tagus; the Serra do Aire, and various ridges which stretch south-westward as far as the mountains of Cintra (q.v.).
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  • The Serra da Arrabida (1637 ft.) rises between Cape Espichel and Setubal.
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  • Sao Mamede (3363 ft.), with the parallel and lower Serra de Portalegre, extends along part of the frontier of northern Alemtejo.
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  • The Serra Grandola and Monte Cereal, two low ranges stretching from north to south, skirt the coast of southern Estremadura.
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  • Between the Minho and Douro the chief rivers are the Lima (Spanish Limia or Antela), which also rises in Galicia, and reaches the sea at Vianna do Castello; the Cavado, which receives the Homem on the right, and forms the port of Espozende in its estuary; and the Ave, which rises in the Serra da Cabreira and issues at the port of Villa do Conde.
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  • Between the Douro and Tagus the Vouga rises in the Serra da Lapa and reaches the sea through the lagoon of Aveiro; the Mondego flows north-east through a long ravine in the Serra da Estrella, and then bends back so as to flow west-south-west.
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  • The Serra de Monchique is petrographically of great interest.
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  • The rainfall is heaviest in the north and on the Serra da Estrella; it is least in Algarve.
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  • The meteorological station on the Serra da Estrella, with a mean annual temperature of 44.7° F., is the coldest spot in Portugal in which systematic observations are taken.
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  • Wolves are found in the wilder parts of the Serra da Estrella, and wild boars are preserved in some districts.
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  • The Serra da Estrella has a rich alpine flora, and the lagoon of Aveiro contains a great number of aquatic plants.
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  • In all, rather more than 45% of the country is uncultivated, chiefly in Alemtejo, Traz-os-Montes and the Serra da Estrella.
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  • Wellesley, who had now become Viscount Wellington, opposed his march south wards, and won a victory at Bussaco on the 27th of September; but Massena subsequently turned the position of the allied army on the Serra de Bussaco, and caused Wellington to fall back upon the fortified lines which he had already constructed at Torres Vedras.
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  • Correa da Serra (I i vols., Lisbon, 1790-1804); Quadro elementar das relac es politicas e diplomatical de Portugal, ed.
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  • Their names were among others Alexandre de Gusmao, the Cavalheiro de Oliveira, Ribeiro Sanches, Correa da Serra, Brotero and Nascimento.
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  • On the Serra Orlando, a mountain not far off, are the extensive remains of an unknown city, the finest in eastern Sicily, but rapidly suffering destruction from the spread of cultivation and unauthorized excavations.
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  • It rises in the mountainous district known as the Pyreneos; but its more ambitious western affluent, the Araguay, has its extreme southern headwaters on the slopes of the Serra Cayapo, and flows a distance of 1080 m.
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  • The Serra do Mar rises not far from the coast and leaves only a narrow coast zone, and the plateau above is much broken with irregular ranges of mountains.
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  • The Serra da Estrella, in Portugal, is usually regarded as a fourth section in the CarpetanoVetonica chain.
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  • Moreover, the significance for Serra of having the work permanently affixed was known to all concerned.
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  • Thereafter, always present in good numbers on the Serra, regular along the river and often heard around the lodge clearings.
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  • Serra is often unfairly maligned for his work on GE, I think.
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  • And any other serra piranha for that matter, must be small.
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  • Half board. q Night 4: Santo de Serra.
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  • The largest of the coastal rivers are the Goyanna, which is formed by the confluence of the Tracunhaem and Capibaribe-mirim, and drains a rich agricultural region in the north-east part of the state; the Capibaribe, which has its source in the Serra de Jacarara and flows eastward to the Atlantic at Recife with a course of nearly 300 m.; the Ipojuca, which rises in the Serra de Aldeia Velha and reaches the coast south of Recife; the Serinhaen and the Una.
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  • The most northerly point, the Serra Roraima on the Venezuela and British Guiana frontier (5° 10' N.), is 56 m.
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  • Running north-east and south-east to enclose the sources of the Rio Paru, it unites with the French Guiana line at 2° 10' N., 55° W., and thence runs easterly along the water-parting of the Serra Tumuc-Humac to the source of the Oyapok, which river is the divisional line to the Atlantic coast.
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  • The names, areas, and populations of the states, together with the names and populations of their capitals, are as follows: Communications.-Railway construction in Brazil dates from 1852, when work was initiated on the Maua railway running from the head of the bay of Rio de Janeiro to the foot of the Serra where Petropolis is situated.
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  • Regular river navigation begins only at Abrantes, a few miles below which the Tagus is greatly widened by receiving on its right bank the impetuous Zezere from the Serra da Estrella.
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  • The Roman antiquities here preserved belong to other places - Luna, Libarna, &c. The Adorno, Giorgio Doria (both containing small but choice picture-galleries), Parodi and Serra and other palaces in this street are worthy of mention.
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  • The meteorological station on the Serra da Estrella, with a mean annual temperature of 44.7° F., is the coldest spot in Portugal in which systematic observations are taken.
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  • Santa Barbara County has a history of winemaking and winegrape growing stretching back more than 200 years to before California was a state (Father Junipero Serra brought grapevine cuttings from Mexico in 1782 to be planted).
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