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Allier appears basalt base basin beds belonging breccia calcareous called Cantal central channel character colour compact composed cone considerable consist contains continuous covered crater crystals deep deposits described direction distance district Dordogne east Edition elevation entirely eruption evidently excavation existing extensive extremity feet felspar flowed formation formed fragments France frequently freshwater granite heights hill Illustrations immediately Italy lake lava Limagne limestone Loire lower mass matter miles Mont Dore Monts D˘me mountain nature nearly numerous observed occasionally occupied occur origin perhaps period plain Plate plateau platform points portions position Post 8vo present primary principal probably range recent regular remains remarkable rest rise river rock scoriŠ seems seen separated side similar slope sometimes species strata stream substance summit surface thick tion trachyte upper valley vast vent volcanic Vols whole
Page 1 - The Life and Death of John of Barneveld, Advocate of Holland : with a View of the Primary Causes and Movements of "The Thirty Years
Page 7 - TF) on the Constitution and Practice of Courts-Martial; with a Summary of the Law of Evidence, and some Notice of the Criminal Law of England with reference to the Trial of Civil Offences. Sixth Edition. 8vo. STANLEY'S (DEAN) Sinai and Palestine. Map. 8vo. 14s. . Bible in the Holy Land ; Extracted from the above Work. By a Lady. Wsodcuts. Fcap. Svo. 2╗. 6d. St. Paul's Epistles to the Corinthians. With Dissertations and Notes. 8vo. 18ź.
Page 258 - BISSET'S (ANDREW) History of the Commonwealth of England, from the Death of Charles I. to the Expulsion of the Long Parliament by Cromwell.
Page 206 - ... been completed. There was first a period when the spacious lakes, of which we still may trace the boundaries, lay at the foot of mountains of moderate elevation, unbroken by the bold peaks and precipices of Mont d'Or, and unadorned by the picturesque outline of the Puy de Dome, or of the volcanic cones and craters now covering the granitic platform. During this earlier scene of repose, deltas were slowly formed ; beds of marl and sand several hundred feet thick deposited; siliceous and calcareous...