Pizarro having arrived at Pachacamac, and being desirous of building a city near the sea coast, he sent some of his officers to search for a convenient harbour either to the north or to the south. They first visited the harbour of Chilca, which, though a good one, and near Pachacamac, was still defective; the coast was a sandy desert, and the poor indians who lived upon it for the purpose of fishing were often forced to abandon their houses, because their wells of brackish water became dry. The commissioners were obliged to look out for another situation, and having arrived at Callao they found that its bay was very capacious, with the river Rimac entering it on the north. They afterwards explored the delightful surrounding valley, and reported their success to Pizarro, who immediately came from Pachacamac, and approving of the situation, laid the foundation of Lima, on the south side of the river, about two leagues from the sea. On the 8th day of January, 1534, he removed to it those Spaniards whom he had left for the purpose of building a town at Jauja. Lima is called by the Spaniards La Ciudad de los Reyes, from being founded on the day on which the Roman Church celebrates the epiphany, or the feast of the worshipping of the kings or magi of the east. Its arms are a shield with three crowns, Or, on an azure field, and the star of the east; for supporters the letters J. C. Jane and Charles, with the motto—Hoc signum vere Regum est. These arms and the title of royal city were granted to Lima by the Emperor Charles V. in 1537. Pizarro built a palace for himself, about two hundred yards from the river, on the contrary side of the great square, or plasa mayor, to that where the palace of the Viceroy now stands; and the remains of it may yet be found in the Callejon de Petateros, mat maker's alley. He was murdered here on the 26th of June, 1541.
According to several Spanish authorities Lima is situated in 12° 2´ 51´´ south latitude, and in 70° 50´ 51´´ longitude west of Cadiz. To the northward and eastward of the city hills begin to rise, which ultimately compose a part of the great chain of the Andes; or rather they are parts of the high mountains which run north and south about twenty leagues to the eastward of Lima. These mountains gradually descend to the sea coast, producing between each row beautiful and fertile valleys, of which the Rimac is one. The chain opening at the back of Lima forms the valley Lurigancho, which closes on its suburbs. That of the greatest height, bordering on the city, is called San Cristobal, and the other Amancaes; the former is 1302 feet above the level of the sea, and the latter 2652. The mountains slope towards the west, and when seen from the bridge appear to have reached the level about three miles from that station, which extremity, viewed from the same place, is the point where the sun disappears at the time of the winter solstice. To the south west is the island called San Lorenzo; more to the south lies Morro Solar, about eight miles distant, where large hills of sand are observed, which, stretching to the eastward and gently rising, form with the Amancaes a crescent, enclosing the picturesque valley Rimac, through which the river of that name majestically flows, producing in its course or wherever its influence can be obtained all the beauties of Flora and the gifts of Ceres.
The site of Lima gradually inclines to the westward, the great square, plasa mayor, being 480 feet above the level of the sea. Thus all the streets in this direction, with many of those intersecting them at right angles, have small streams of water running along them, which contribute very much to the cleanliness and salubrity of the city and its inhabitants. The water which runs through the streets, as well as that which feeds the fountains and the canals for the irrigation of gardens, orchards and plantations, which fill the whole valley, is drawn from the river Rimac. This river has its origin in the province of Huarochiri, and receives in its course several small streams, which descend the mountains, and are produced by the melting of the snow on the tops of the Andes, as well as by the rains which fall in the interior, at which time the river swells very much, and covers the whole of its bed, which at other times is in many places almost dry. The water in Lima is said to be crude, holding in solution a considerable quantity of selenite, besides being impregnated with abundance of fixed air; hence, indigestions and other affections of the stomach are attributed to it; but Dr. Unanue very justly asks, "may not these diseases be derived from Cupid and Ceres?" The water is certainly far from being pure; for the artaxea, which supplies the city fountains, and the pugios, which supply the suburbs, called San Lazaro, are stagnant pools; both are often full of aquatic plants, which decay and rot in them; they moreover contain water that has been employed in the irrigation of the plantations and farms at the back of the city, and not unfrequently animals have been drowned in them.
The climate of Lima is extremely agreeable; the heat which would naturally be expected in so low a latitude is seldom felt, and those who have been accustomed to the scorching sun and suffocating heat of Bahia, on the opposite side of the Continent, or to those of Carthagena, in the same latitude, are astonished at the mild and almost equable climate of Lima. The following thermometrical observations, made in the years 1805 and 1810, will evince the truth of what has been asserted:—
THERMOMETRICAL OBSERVATIONS,
MADE AT NOON IN THE SHADE OF AN OPEN ROOM AT LIMA.
| 1805 | 1810 | ||||||
| ___ | /\ | ___ | ___ | /\ | ___ | ||
| / | \ | / | \ | ||||
| Max. | Min. | Max. | Min. | ||||
| January | 77 | 74¾ | 76 | 73¾ | |||
| February | 79½ | 76 | 77 | 74¾ | |||
| March | 78½ | 74¾ | 77 | 74¾ | |||
| April | 74¾ | 72 | 74¾ | 71¼ | |||
| May | 73¾ | 67 | 71¼ | 67 | |||
| June | 65¾ | 65 | 66 | 64 | |||
| July | 65 | 63 | 64¾ | 61 | |||
| August | 63½ | 62¾ | 63¾ | 61 | |||
| September | 65 | 63½ | 64¾ | 64 | |||
| October | 65¾ | 63½ | 65¾ | 63½ | |||
| November | 69½ | 65¾ | 69½ | 65½ | |||
| December | 73¾ | 69½ | 71½ | 70 | |||
| —— | —— | —— | —— | ||||
| Mean height du-} | |||||||
| ring the Year.} | 79½ | 62¾ | 77 | 61 | |||
| ==== | ==== | ==== | ==== | ||||
The coolness of the climate is occasioned by the wind and a peculiar state of the atmosphere. The wind generally blows from different points of the compass between the south west and the south east. When from the former direction, it crosses in its course a great portion of the Pacific Ocean, and when it comes from the eastward it has not to pass over sandy deserts or scorching plains, but to traverse first the immense tract of woodland countries lying between the Brazils and Peru, and afterwards the frozen tops of the Cordillera, at a distance of twenty leagues from Lima; so that, in both cases, it is equally cool and refreshing. A northerly wind is very seldom felt in Lima; but when it blows, as if by accident, from that quarter, the heat is rather oppressive. On the 6th of March, 1811, the wind being from the north, I made the following observations with a Farenheit's thermometer, at one o'clock, p. m.
| In the shade in an open room | 80° |
| In the air, five yards from the sun's rays | 87° |
| In the sun | 106° |
| Water in the shade from sunrise | 74° |
| Water in a well 20 yards below the surface of the earth | 70° |
| Sea water at Callao at 4 p. m. | 64° |
| Heat of the body, perspiring | 96° |
| ———————after cooling in the shade | 94° |
The heat of the sun in summer is mitigated by a canopy of clouds, which constantly hang over Lima, and although not perceptible from the city, yet when seen from an elevated situation in the mountains, they appear somewhat like the smoke floating in the atmosphere of large towns where coal is burnt; but as this material is not used in Lima, the cause and effect must be different.