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Congressional Giants
The Congress of the United States operates in the shadow of the American presidency, which can make the legislative branch appear less important than the executive in our constitutional system of government. And yet Congress is a co-equal branch of government, deriving its powers from Article I of the United States Constitution. Love it or hate it, the institution is a source of incredible power. It behooves all Americans to learn more about Congress. Although a single slender volume cannot provide information on all there is to know about Congress, it can begin the journey. In Congressional Giants, political scientist J. Michael Martinez explores the careers and achievements of 14 influential leaders of Congress—men who either held formal positions within the chambers of Congress, such as speaker of the House of Representatives or Senate majority leader, or who served on important committees--to determine how they shaped the course of American history.
Congressional Record
The Congressional Record is the official record of the proceedings and debates of the United States Congress. It is published daily when Congress is in session. The Congressional Record began publication in 1873. Debates for sessions prior to 1873 are recorded in The Debates and Proceedings in the Congress of the United States (1789-1824), the Register of Debates in Congress (1824-1837), and the Congressional Globe (1833-1873)
Geology, Geochemistry, and Mineral Resource Assessment of the Southern Nantahala Wilderness and Adjacent Roadless Areas, Rabun and Towns Counties, Georgia, and Clay and Macon Counties, North Carolina
The Southern Nantahala Wilderness and the Buzzard Knob and Southern Nantahala Roadless Areas are near one another and near the North Carolina-Georgia State line in Rabun and Towns Counties, Ga., and Clay and Macon Counties, N.C. The areas collectively span a region of polydeformed and metamorphosed rocks assigned to three major thrust sheets, from east to west the Tallulah Falls, Helen, and Richard Russell thrust sheets. Outcrop patterns and minor structures in the older sillimanite- grade Richard Russell rocks in the western part of the study area outline an earlier phase of isoclinal folding not apparent in the outcrop pattern of younger kyanite- and staurolite-grade Coweeta Group rocks im...
