dancers whirling round the room passed close to where Carlos sat. It was a waltz. Catalina was waltzing with the beau Echevarria. At each circle her face was towards Carlos, and then their eyes met. In these transient but oft-recurring glances the eyes of a Spanish maid will speak volumes, and Carlos was reading in those of Catalina a pleasant tale. As she came round the room for the third time, he noticed something held between her fingers, which rested over the shoulder of her partner. It was a sprig with leaves of a dark greenish hue. When passing close to him, the sprig, dexterously detached, fell upon his knees, while he could just bear, uttered in a soft whisper, the word—“Tuya!”
Carlos caught the sprig, which was a branch of “tuya,” or cedar. He well understood its significance; and after pressing it to his lips, he passed it through the button-hole of his embroidered “jaqueta.” As Catalina came round again, the glances exchanged between them were those of mutual and confiding love.
The night wore on—Don Ambrosio at length became sleepy, and carried off his daughter, escorted by Roblado.
Soon after most of the ricos and fashionables left the saloon, but some tireless votaries of Terpsichore still lingered until the rosy Aurora peeped through the “rejas” of the Casa de Cabildo.
Chapter Ten.
The “Llano Estacado,” or “Staked Plain” of the hunters, is one of the most singular formations of the Great American Prairie. It is a table-land, or “steppe,” rising above the regions around it to a height of nearly one thousand feet, and of an oblong or leg-of-mutton form, trending from north to south.
It is four hundred miles in length, and at its widest part between two and three hundred. Its superficial area is about equal to the island of Ireland. Its surface aspect differs considerably from the rest of prairie-land, nor is it of uniform appearance in every part. Its northern division consists of an arid steppe, sometimes treeless, for an extent of fifty miles, and sometimes having a stunted covering of mezquite (acacia), of which there are two distinct species. This steppe is in several places rent by chasms a thousand feet in depth, and walled in on both sides by rugged impassable precipices. Vast masses of shapeless rocks lie along the beds of these great clefts, and pools of water appear at long intervals, while stunted cedars grow among the rocks, or cling from the seams of the cliffs.
Such chasms, called “cañons,” can only be crossed, or even entered, at certain points; and these passes are frequently a score of miles distant from each other.
On the upper plain the surface is often a dead level for a hundred miles, and as firm as a macadamised road. There are spots covered with a turf of grass of the varieties known as gramma, buffalo, and mezquite; and sometimes the traveller encounters a region where shallow ponds of different sizes stud the plain—a few being permanent, and surrounded by sedge. Most of these ponds are more or less brackish, some sulphurous, and others perfectly salt. After heavy rains such aqueous deposits are more numerous, and their waters sweeter; but rain seems to fall by accident over this desolate region, and after long spells of drought the greater number of these ponds disappear altogether.
Towards the southern end of the Llano Estacado the surface exhibits a very singular phenomenon—a belt of sand-hills, nearly twenty miles in breadth and full fifty in length, stretching north and south upon the plain. These hills are of pure white sand, thrown up in ridges, and sometimes in cones, to the height of a hundred feet, and without tree, bush, or shrub, to break their soft outlines, or the uniformity of their colour. But the greatest anomaly of this geological puzzle is, that water-ponds are found in their very midst—even among their highest ridges—and this water not occasional, as from rains, but lying in “lagunas,” with reeds, rushes, and nymphae growing in them, to attest that the water is permanent! The very last place where water might be expected to make a lodgment.
Such formations of drift-sand are common upon the shores of the Mexican Gulf, as well as on European coasts, and there their existence is easily explained; but here, in the very heart of a continent, it cannot be regarded as less than a singular phenomenon.
This sand-belt is passable at one or two points, but horses sink to the knees at every step, and but for the water it would be a perilous experiment to cross it.
Where is the Llano Estacado? Unroll your map of North America. You will perceive a large river called the Canadian rising in the Rocky Mountains, and running, first southerly, and then east, until it becomes part of the Arkansas. As this river bends eastwardly, it brushes the northern end of the Llano Estacado, whose bluffs sometimes approach close to its banks, and at other times are seen far off, resembling a range of mountains—for which they have been frequently mistaken by travellers.
The boundary of the west side of the “Staked Plain” is more definite. Near the head-waters of the Canadian another large river has its source. This the Pecos. Its course, you will observe, is nearly south, but your map is not correct, as for several hundred miles the Pecos runs within a few degrees of east. It afterwards takes a southerly direction, before it reaches its embouchure in the Rio Grande. Now the Pecos washes the whole western base of the Llano Estacado; and it is this very plain, elevated as it is, that turns the Pecos into its southerly course, instead of leaving it to flow eastward, like all the other prairie-streams that head in the Rocky Mountains.
The eastern boundary of the Llano Estacado is not so definitely marked, but a line of some three hundred miles from the Pecos, and cutting the head-waters of the Wichita, the Louisiana Bed, the Brazos, and Colorado, will give some idea of its outline. These rivers, and their numerous tributaries, all head in the eastern “ceja” (brow) of the Staked Plain, which is cut and channelled by their streams into tracts of the most rugged and fantastic forms.
At the south the Llano Estacado tapers to a point, declining into the mezquite plains and valleys of numerous small streams that debouch into the Lower Rio Grande.
This singular tract is without one fixed dweller; even the Indian never makes abode upon it beyond the few hours necessary to rest from his journey, and there are parts where he—inured as he is to hunger and thirst—dare not venture to cross it. So perilous is the “Jornada,” or crossing of the Llano Estacado, that throughout all its length of four hundred miles there are only two places where travellers can effect it in safety! The danger springs from the want of water, for there are spots of grass in abundance; but even on the well-known routes there are, at certain seasons, stretches of sixty and eighty miles where not a drop of water is to be procured!
In earlier times one of these routes was known as the “Spanish Trail,” from Santa Fé to San Antonio de Bexar, of Texas; and lest travellers should lose their way, several points were marked with “palos,” or stakes. Hence the name it has received.
The Llano Estacado is now rarely travelled, except by the ciboleros, or Mexican buffalo-hunters, and “Comancheros,” or Indian traders. Parties of these cross it from the settlements of New Mexico, for the purpose of hunting the buffalo, and trafficking with the Indian tribes that roam over the plains to the east. Neither the hunt nor the traffic is of any great importance, but it satisfies a singular race of men, whom chance or inclination has led to the adopting it as a means of subsistence.
These men are to the Mexican frontier pretty much what the hunter and backwoodsman are upon the borders of the Anglo-American settlements. They are, however, in many respects different from the latter—in arms and equipments, modes of hunting, and otherwise. The outfit of a cibolero, who is usually also a coureur de bois, is very simple. For hunting, he is mounted on a tolerable—sometimes a fine—horse and armed with a bow and arrows, a hunting-knife, and a long lance. Of fire-arms
