Question: What is the only major mountain range located between the Appalachian Mountains and the mountains higher than those which contain parts of the state other than Florida which received error coins?

<P0-S0> Most of the state has a humid subtropical climate, with the exception of some of the higher elevations in the Appalachians, which are classified as having a mountain temperate climate or a humid continental climate due to cooler temperatures. <P0-S1> The Gulf of Mexico is the dominant factor in the climate of Tennessee, with winds from the south being responsible for most of the state's annual precipitation. <P0-S2> Generally, the state has hot summers and mild to cool winters with generous precipitation throughout the year, with highest average monthly precipitation generally in the winter and spring months, between December and April. <P0-S3> The driest months, on average, are August to October. <P0-S4> On average the state receives 50 inches (130 cm) of precipitation annually. <P0-S5> Snowfall ranges from 5 inches (13 cm) in West Tennessee to over 16 inches (41 cm) in the higher mountains in East Tennessee. <SEP> <P1-S0> Early releases of the Washington coin included error coins shipped primarily from the Philadelphia mint to Florida and Tennessee banks. <P1-S1> Highly sought after by collectors, and trading for as much as $850 each within a week of discovery, the error coins were identified by the absence of the edge impressions "E PLURIBUS UNUM IN GOD WE TRUST 2007 P". <P1-S2> The mint of origin is generally accepted to be mostly Philadelphia, although identifying the source mint is impossible without opening a mint pack also containing marked units. <P1-S3> Edge lettering is minted in both orientations with respect to "heads", some amateur collectors were initially duped into buying "upside down lettering error" coins. <P1-S4> Some cynics also erroneously point out that the Federal Reserve makes more profit from dollar bills than dollar coins because they wear out in a few years, whereas coins are more permanent. <P1-S5> The fallacy of this argument arises because new notes printed to replace worn out notes, which have been withdrawn from circulation, bring in no net revenue to the government to offset the costs of printing new notes and destroying the old ones. <P1-S6> As most vending machines are incapable of making change in banknotes, they commonly accept only $1 bills, though a few will give change in dollar coins. <SEP> <P2-S0> oklahoma has four primary mountain ranges: the ouachita mountains, the arbuckle mountains, the wichita mountains, and the ozark mountains. <P2-S1> contained within the u.s. interior highlands region, the ozark and ouachita mountains mark the only major mountainous region between the rocky mountains and the appalachians. <P2-S2> a portion of the flint hills stretches into north-central oklahoma, and near the state's eastern border, cavanal hill is regarded by the oklahoma tourism & recreation department as the world's tallest hill; at 1,999 feet (609 m), it fails their definition of a mountain by one foot. <SEP> <P3-S0> the great plains come to an abrupt end at the rocky mountains. <P3-S1> the rocky mountains form a large portion of the western u.s., entering from canada and stretching nearly to mexico. <P3-S2> the rocky mountain region is the highest region of the united states by average elevation. <P3-S3> the rocky mountains generally contain fairly mild slopes and wider peaks compared to some of the other great mountain ranges, with a few exceptions (such as the teton mountains in wyoming and the sawatch range in colorado). <P3-S4> the highest peaks of the rockies are found in colorado, the tallest peak being mount elbert at 14,440 ft (4,400 m). <P3-S5> the rocky mountains contain some of the most spectacular, and well known scenery in the world. <P3-S6> in addition, instead of being one generally continuous and solid mountain range, it is broken up into a number of smaller, intermittent mountain ranges, forming a large series of basins and valleys. <SEP> <P4-S0> The Appalachian Mountains (French: les Appalaches), often called the Appalachians, are a system of mountains in eastern North America. <P4-S1> The Appalachians first formed roughly 480 million years ago during the Ordovician Period. <P4-S2> They once reached elevations similar to those of the Alps and the Rocky Mountains before experiencing natural erosion. <P4-S3> The Appalachian chain is a barrier to east - west travel, as it forms a series of alternating ridgelines and valleys oriented in opposition to most highways and railroads running east - west. <SEP> <P5-S0> The Great Plains lie west of the Mississippi River and east of the Rocky Mountains. <P5-S1> A large portion of the country's agricultural products are grown in the Great Plains. <P5-S2> Before their general conversion to farmland, the Great Plains were noted for their extensive grasslands, from tallgrass prairie in the eastern plains to shortgrass steppe in the western High Plains. <P5-S3> Elevation rises gradually from less than a few hundred feet near the Mississippi River to more than a mile high in the High Plains. <P5-S4> The generally low relief of the plains is broken in several places, most notably in the Ozark and Ouachita Mountains, which form the U.S. <P5-S5> Interior Highlands, the only major mountainous region between the Rocky Mountains and the Appalachian Mountains.