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He took up his position between the towns of Pandosia and Heraclea, on the River Siris. The Romans, who were encamped on the other side of the river, were the first to begin the battle. They crossed the river, and were immediately attacked by the cavalry of Pyrrhus, who led them to the charge in person, and distinguished himself as usual by the most daring acts of valor. The Romans, however, bravely sustained the attack; and Pyrrhus, finding that his cavalry could not decide the day, ordered his infantry to advance. The battle was still contested most furiously: seven times did both armies advance and retreat; and it was not till Pyrrhus brought forward his elephants, which bore down every thing before them, that the Romans took to flight, leaving their camp to the conqueror (B.C. 280).

The Jicarillas, or, as they are commonly called, "Jicarilla Apaches," occupy a reservation of nearly four hundred and fifty square miles of mountainous country in northern New Mexico. Linguistically the Jicarillas are of the same stock as the Apache of Arizona; but here the relationship ceases, for the two peoples have virtually no knowledge one of the other; each, according to their respective genesis myths, had their origin in the general region in which they live to-day, while the dialect, mythology, legends, and medicine rites of the Jicarillas more closely resemble those of the Navaho than any of the Apache groups. The designation "Jicarilla Apaches" is an inheritance from the early Spaniards, who were wont to designate as Apache any warlike tribe which had not been brought under subjection. Such were the Apaches de Nabaju (Navaho), the Apaches del Perrillo, the Apaches Gilenos, Apaches Tejuas, Apaches Vaqueros, Apaches Faraones, Apaches Llaneros, Apaches Lipanes, and a host of others, of whom the Spanish missionaries and colonists had little or no knowledge except that derived, alas, from predatory raids on the peaceable Indians among whom they were established. The name "Apache," therefore, was applied in the Rio Grande country of New Mexico in much the same way as the term "Yavapai" was given in the Rio Colorado region of Arizona, and, naturally enough, it still survives.

Owing to many natural causes the river may, after a while, cease to flow, leaving enlarged portions of its channel behind as a succession of chambers in a cave. But water would still come trickling in from the tops and sides, and be continuously dripping to the floor, where it speedily evaporates. When such is the case it leaves behind it the limestone it held in solution. So, in process of time, if the deposition is undisturbed, there will be formed over the floor of the cave a more or less continuous layer of limestone matter known as stalagmite. The same formations on the top and sides of the cave are called stalactites. In places where the drip is continuous the stalactite gradually assumes the shape of an immense icicle; while the stalagmite on the floor of the cave, underneath the drip, rises in a columnar mass to meet the descending stalactite. A union of these is not uncommon, and, we have pillars and columns presenting the strange, fantastic appearance on which tourists delight to dwell in their notes of travel.

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