An analysis of the downfall of the plains indians in the 1800s

History[ edit ] The nomadic tribes historically survived on hunting and gathering, and the American Bison or buffalo was one primary resource for items which people used for everyday life, including food, cups, decorations, crafting tools, knives, and clothing. The tribes followed the seasonal grazing and migration of the bison. The Plains Indians lived in teepees because they were easily disassembled and allowed the nomadic life of following game. While searching for a reputedly wealthy land called Quivira inCoronado came across the Querechos in the Texas panhandle.

An analysis of the downfall of the plains indians in the 1800s

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Central Texas section — central Texas. It extends northward from the Mexican boundary far into Canada. The semi-arid climate excludes tree growth and opens far-reaching views.

They are of diverse structure and of various stages of erosional development. They are occasionally interrupted by buttes and escarpments. They are frequently broken by valleys. Yet on the whole, a broadly extended surface of moderate relief so often prevails that the name, Great Plains, for the region as a whole is well-deserved.

The eastern boundary of the plains is more climatic than topographic. The line of 20 in. If a boundary must be drawn where nature presents only a gradual transition, this rainfall line may be taken to divide the drier plains from the moister prairies.

The plains may be described in northern, intermediate, central and southern sections, in relation to certain peculiar features. The strata here are Cretaceous or early Tertiarylying nearly horizontal.

The surface is shown to be a plain of degradation by a gradual ascent here and there to the crest of a ragged escarpment, the escarpment-remnant of a resistant stratum.

All these reliefs are more plentiful towards the mountains in central Montana. The peneplain is no longer in the cycle of erosion that witnessed its production. It appears to have suffered a regional uplift or increase in elevation, for the upper Missouri River and its branches no longer flow on the surface of the plain, but in well graded, maturely opened valleys, several hundred feet below the general level.

This peculiar feature is explained as the result of displacement of the river from a better graded preglacial valley by the Pleistocene ice sheet. Here, the ice sheet overspread the plains from the moderately elevated Canadian highlands far on the north-east, instead of from the much higher mountains near by on the west.

The Black Hillschiefly in western South Dakotaare the largest group. The weaker uppermost strata have been eroded down to the level of the plains where their upturned edges are evenly truncated.

The next following harder strata have been sufficiently eroded to disclose the core of underlying igneous and metamorphic crystalline rocks in about half of the domed area. Known as the Badlandsit is a minutely dissected form with a relief of a few hundred feet.

This is due to several causes: That is, this section was once smoothly covered with a gently sloping plain of gravel and sand that had been spread far forward on a broad denuded area as a piedmont deposit by the rivers which issued from the mountains.

Since then, it has been more or less dissected by the erosion of valleys. The central section of the plains thus presents a marked contrast to the northern section. While the northern section owes its smoothness to the removal of local gravels and sands from a formerly uneven surface by the action of degrading rivers and their inflowing tributaries, the southern section owes its smoothness to the deposition of imported gravels and sands upon a previously uneven surface by the action of aggrading rivers and their outgoing distributaries.

The two sections are also alike in that residual eminences still here and there surmount the peneplain of the northern section, while the fluviatile plain of the central section completely buried the pre-existent relief. Exception to this statement must be made in the southwest, close to the mountains in southern Colorado, where some lava-capped mesas Mesa de MayaRaton Mesa stand several thousand feet above the general plain level, and thus testify to the widespread erosion of this region before it was aggraded.

Like the central section, it is for the most part a dissected fluviatile plain. However, the lower lands which surround it on all sides place it in so strong relief that it stands up as a table-land, known from the time of Mexican occupation as the Llano Estacado.

It is of very irregular outline, narrowing to the south. Like the High Plains farther north, it is extraordinarily smooth. The Llano is separated from the plains on the north by the mature consequent valley of the Canadian Riverand from the mountains on the west by the broad and probably mature valley of the Pecos River.

There, between the Brazos and Colorado rivers, occurs a series of isolated outliers capped by a limestone which underlies both the Llano Uplift on the west and the Grand Prairies escarpment on the east.

The southern and narrow part of the table-land, called the Edwards Plateauis more dissected than the rest, and falls off to the south in a frayed-out fault scarp.

This scarp overlooks the coastal plain of the Rio Grande embayment. The central denuded area, east of the Llano, resembles the east-central section of the plains in exposing older rocks.

Between these two similar areas, in the space limited by the Canadian and Red Rivers, rise the subdued forms of the Wichita Mountains in Oklahomathe westernmost member of the Ouachita system. However, during the Late Cretaceous to the Paleocene 65—55 million years agothe seaway had begun to recede, leaving behind thick marine deposits and a relatively flat terrain which the seaway had once occupied.

During the Cenozoic era, specifically about 25 million years ago during the Miocene and Pliocene epochs, the continental climate became favorable to the evolution of grasslands. Existing forest biomes declined and grasslands became much more widespread.

An analysis of the downfall of the plains indians in the 1800s

The grasslands provided a new niche for mammals, including many ungulates and gliresthat switched from browsing diets to grazing diets. Traditionally, the spread of grasslands and the development of grazers have been strongly linked.The Plains Indians found by Coronado had not yet obtained horses; it was the introduction of the horse that revolutionized Plains culture.

When horses were obtained, the Plains tribes rapidly integrated them into their daily lives. Evidence from the Agate Basin site in eastern Wyoming, for example, indicates that humans lived in the Plains at least as early as B.C.

Radiocarbon dating of material from the Lewisville site near Dallas, Texas, suggests Indians and their precursors may have been in the Plains for at least 38, years.

Native Americans of the Great Plains began annu- mate in the Great Plains began in the early s and were made at forts established by the US Army (e.g., Lawson ; Grice ). Th e majority of the obser- Great Plains Research 25 (Fall )– Figure 1.

Native American paints a winter count on a buff alo skin (National. At the time of Spanish decline and Mexican independence, traders from the United States began to venture onto the Plains and establish contacts with Santa Fe and the Indian groups between the United States and New Mexico.

An analysis of the downfall of the plains indians in the 1800s

Plains Indians, Interior Plains Indians or Indigenous people of the Great Plains and Canadian Prairies are the Native American tribes and First Nation band governments who have traditionally lived on the greater Interior Plains (i.e.

the Great Plains and the Canadian Prairies) in North America. Their historic nomadic culture and development of.

The Cattle Kingdom really started to bust when disaster struck in and Much of the prairie grass that was depended on by the the ranchers for feed had been eaten by the huge cattle herds on the Plains.

Plains Indians - Wikipedia