Extending her role as teacher and mother she became an ethnic spokesperson as she confronted the power of the Yankee Protestant men of the Public School Association. She worked to replace year-old textbooks, to protect the claims of local Boston women for career opportunities in the school system, and to propose a degree-granting teachers college. It took over six months to remove the molasses from the cobblestone streets, theaters, businesses, automobiles, and homes. Boston Harbor ran brown until summer.
Eventually, the term came to refer to all Ozark Plateau drainage into the Arkansas and Missouri Rivers. An alternative origin for the name "Ozark" relates the French term aux arcs.
In the later 17th and early 18th centuries, French cartographers mapped the Arkansas and Mississippi Rivers. The large, top most arc or bend in this part of the Arkansas River was referred to as the aux arcs—the top or most northern arc in the whole of the lower Arkansas.
Travelers arriving by boat would disembark at this top bend of the river to explore the Ozarks; the town of Ozark, Arkansas is located on the north bank at this location.
Other possible derivations include aux arcs meaning "[land] of the arches,"  in reference to the dozens of natural bridges formed by erosion and collapsed caves in the Ozark region.
It is even suggested aux arcs is an abbreviation of aux arcs-en-ciel, French for "toward the rainbows," which are a common sight in the mountainous regions.
After the Louisiana Purchase inAmerican travelers in the region referred to various features of the upland areas using the term Ozark, such as Ozark Mountains and Ozark forests.
By the early 20th century, the Ozarks had become a generic and widely used term. Karst features such as springs losing streamssinkholes and caves are common in the limestones of the Springfield Plateau and abundant in the dolostone bedrock of the Salem Plateau and Boston Mountains.
Kept open by periodic fires that limit growth of grasses and forbs in shallow soil, glades are home to collared lizards, tarantulas, scorpions, cacti and other species more typical of the desert southwest.
The Ouachita Mountains to the south rise a few hundred feet higher, but are not geographically associated with the Ozarks. Summits can reach elevations of just over 2, feet m with valleys to 1, feet m deep m to m.
Turner Ward Knob is the highest named peak. Located in western Newton County, Arkansasits elevation is 2, feet m. Nearby, five unnamed peaks have elevations at or slightly above 2, feet m. Drainage is primarily to the White River, with the exception of the Illinois Riveralthough there also is considerable drainage from the south slopes of the Boston Mountains to the Arkansas River.
Although the Springfield formation's surface is primarily Mississippian limestone and chertthe Salem Plateau is older Ordovician dolostones, limestones, and sandstones.
The formations are separated by steep escarpments that dramatically interrupt the rolling hills. Although much of the Springfield Plateau has been denuded of the surface layers of the Boston Mountains, large remnants of these younger layers are present throughout the southern end of the formation, possibly suggesting a peneplain process.
The igneous and volcanic rocks of the Saint Francois Mountains are the exposed remains of a Proterozoic mountain range hundreds of millions of years old. The remaining hills are the exposed portion of an extensive terrane the Spavinaw terrane in part of granitic and rhyolitic rocks dating from to mya that stretches from Ohio to western Oklahoma.
Reef complexes occur in the sedimentary layers surrounding this ancient island. These flanking reefs were points of concentration for later ore -bearing fluids which formed the rich lead - zinc ores that have been and continue to be mined in the area. The igneous and volcanic rocks extend at depth under the relatively thin veneer of Paleozoic sedimentary rocks and form the basal crust of the entire region.
A major unconformity in the region attests that the Ozarks were above sea level for several hundred million years from the time of the volcanism in the Precambrian until the mid- Cambrian with an erosionally produced relief of up to feet.
Coral reefs formed around the granite and rhyolite islands in this Cambrian sea. This carbonate formation, the Bonneterre now mostly dolomiteis exposed around the St. Withdrawal of the seas resulted in another unconformity during the latest Cambrian and early Ordovician periods.
Hydrothermal mineralizing fluids formed the rich lead ore deposits of the Lead Belt during this time. The sandstone of the Roubidoux forms prominent bluffs along the streams eroding into the southern part of the Salem Plateau.
The Roubidoux and Gunter sandstones serve as significant aquifers when present in the subsurface.History "Rock & Roll Band" is the song that Paul Ahern played for Charlie McKenzie to interest him in the yet unnamed band that was to become Boston.
Shortly after, Ahern and McKenzie signed on as the band's managers. The History Of Rock Essay INTRODUCTION Rock and Roll started after the year with its roots being in Blues, Gospel, and Jazz. This influenced vocal music, which was popular with the African American population/5(1).
Professor Golove History of Rock 04/03/13 Boston is an American rock band hailing from, as their name implies, Boston, Massachusetts. They attained their most noteworthy successes during the .
Buffalo Lookout, the highest point in the Ozarks, is located in the Boston Mountains. Geologically, the area is a broad dome with the exposed core in the St. Francois Mountains. The Ozarks cover nearly 47, square miles (, km 2), making it the most extensive highland region between the Appalachians and Rockies.
Learn history of rock and roll with free interactive flashcards. Choose from different sets of history of rock and roll flashcards on Quizlet. Short Essay. On December 16, , American patriots dressed as Mohawk Indians boarded the vessels of the East Indian Company docked in the Boston harbor and dumped all the tea that was on the three ships into the ocean.