ISBN: 1130834913

[EAN: 9781130834918], Neubuch, [PU: RareBooksClub.com], ROYAL PHYSICAL SOCIETY OF EDINBURGH,SUBJECTS, This item is printed on demand. Paperback. 180 pages. Dimensions: 9.7in. x 7.4in. x 0… Plus…

[EAN: 9781130834918], Neubuch, [PU: RareBooksClub.com], ROYAL PHYSICAL SOCIETY OF EDINBURGH,SUBJECTS, This item is printed on demand. Paperback. 180 pages. Dimensions: 9.7in. x 7.4in. x 0.4in.This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1885 Excerpt: . . . southern side of the dislocation. The upheaval may have gone on locally and irregularly at first, but seems not to have been great enough to raise the Palaeozoic rocks above sea-level till the end of the Senonian period, when the whole sea floor was laid bare, and all further deposition arrested. 1 Sec von Groddeck, Erzlagerstattenlehre, pp. 265, 266. There appears to be no evidence of post-cretaceous submergence in this district, and it is difficult to determine the date at which the upheaval ceased. The most important representative of the Tertiary deposits is the Oligocene Brown Coal which occurs in depressions at various places on and around the Harz. A bed of workable brown coal, 50 feet in thickness, occupies a bay-like hollow in the core rocks immediately adjoining the line of fault at Wienrode between Thale and Blankenburg. The coal appears to cross the line of dislocation, and rest on the upturned edges of the Zechstein and Red Bunter sandstone in a way which seems clearly to show that the upward movement had entirely ceased before the agencies of denudation had hollowed out the depression subsequently filled up by the vegetable deposit. 10. Recapitulation. The area now occupied by the Harz Mountains was, during the Palaeozoic period, a portion of the great sea in which the yilurian, Devonian, and Lower Carboniferous rocks of Central Europe were deposited. The alternating greywackes, sandstones, shales, and limestones, with their accompanying fossils, indicate changes in the depth and condition of the water, but form throughout a perfectly conformable series. Volcanic action was vigorous in the Devonian period, when diabases and tuffs were emitted at various parts of the area. Towards the close of the Lower Carboniferous period the sea. . . This item ships from La Vergne,TN.<

2012, ISBN: 1130834913

[EAN: 9781130834918], Neubuch, [PU: Rarebooksclub.com, United States], Language: English Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing … Plus…

[EAN: 9781130834918], Neubuch, [PU: Rarebooksclub.com, United States], Language: English Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1885 Excerpt: . southern side of the dislocation. The upheaval may have gone on locally and irregularly at first, but seems not to have been great enough to raise the Palaeozoic rocks above sea-level till the end of the Senonian period, when the whole sea floor was laid bare, and all further deposition arrested. 1 Sec von Groddeck, Erzlagerstattenlehre, pp. 265, 266. There appears to be no evidence of post-cretaceous submergence in this district, and it is difficult to determine the date at which the upheaval ceased. The most important representative of the Tertiary deposits is the Oligocene Brown Coal which occurs in depressions at various places on and around the Harz. A bed of workable brown coal, 50 feet in thickness, occupies a bay-like hollow in the core rocks immediately adjoining the line of fault at Wienrode between Thale and Blankenburg. The coal appears to cross the line of dislocation, and rest on the upturned edges of the Zechstein and Red Bunter sandstone in a way which seems clearly to show that the upward movement had entirely ceased before the agencies of denudation had hollowed out the depression subsequently filled up by the vegetable deposit. 10. Recapitulation. The area now occupied by the Harz Mountains was, during the Palaeozoic period, a portion of the great sea in which the yilurian, Devonian, and Lower Carboniferous rocks of Central Europe were deposited. The alternating greywackes, sandstones, shales, and limestones, with their accompanying fossils, indicate changes in the depth and condition of the water, but form throughout a perfectly conformable series. Volcanic action was vigorous in the Devonian period, when diabases and tuffs were emitted at various parts of the area. Towards the close of the Lower Carboniferous period the sea.<

2012, ISBN: 1130834913

[EAN: 9781130834918], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****. This historic book may have numerous typos and missing text. Purchasers … Plus…

[EAN: 9781130834918], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****. This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1885 Excerpt: . southern side of the dislocation. The upheaval may have gone on locally and irregularly at first, but seems not to have been great enough to raise the Palaeozoic rocks above sea-level till the end of the Senonian period, when the whole sea floor was laid bare, and all further deposition arrested. 1 Sec von Groddeck, Erzlagerstattenlehre, pp. 265, 266. There appears to be no evidence of post-cretaceous submergence in this district, and it is difficult to determine the date at which the upheaval ceased. The most important representative of the Tertiary deposits is the Oligocene Brown Coal which occurs in depressions at various places on and around the Harz. A bed of workable brown coal, 50 feet in thickness, occupies a bay-like hollow in the core rocks immediately adjoining the line of fault at Wienrode between Thale and Blankenburg. The coal appears to cross the line of dislocation, and rest on the upturned edges of the Zechstein and Red Bunter sandstone in a way which seems clearly to show that the upward movement had entirely ceased before the agencies of denudation had hollowed out the depression subsequently filled up by the vegetable deposit. 10. Recapitulation. The area now occupied by the Harz Mountains was, during the Palaeozoic period, a portion of the great sea in which the yilurian, Devonian, and Lower Carboniferous rocks of Central Europe were deposited. The alternating greywackes, sandstones, shales, and limestones, with their accompanying fossils, indicate changes in the depth and condition of the water, but form throughout a perfectly conformable series. Volcanic action was vigorous in the Devonian period, when diabases and tuffs were emitted at various parts of the area. Towards the close of the Lower Carboniferous period the sea.<

2012, ISBN: 1130834913

[EAN: 9781130834918], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing text. Purchasers c… Plus…

[EAN: 9781130834918], Neubuch, [PU: Rarebooksclub.com, United States], Brand New Book ***** Print on Demand *****.This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1885 Excerpt: . southern side of the dislocation. The upheaval may have gone on locally and irregularly at first, but seems not to have been great enough to raise the Palaeozoic rocks above sea-level till the end of the Senonian period, when the whole sea floor was laid bare, and all further deposition arrested. 1 Sec von Groddeck, Erzlagerstattenlehre, pp. 265, 266. There appears to be no evidence of post-cretaceous submergence in this district, and it is difficult to determine the date at which the upheaval ceased. The most important representative of the Tertiary deposits is the Oligocene Brown Coal which occurs in depressions at various places on and around the Harz. A bed of workable brown coal, 50 feet in thickness, occupies a bay-like hollow in the core rocks immediately adjoining the line of fault at Wienrode between Thale and Blankenburg. The coal appears to cross the line of dislocation, and rest on the upturned edges of the Zechstein and Red Bunter sandstone in a way which seems clearly to show that the upward movement had entirely ceased before the agencies of denudation had hollowed out the depression subsequently filled up by the vegetable deposit. 10. Recapitulation. The area now occupied by the Harz Mountains was, during the Palaeozoic period, a portion of the great sea in which the yilurian, Devonian, and Lower Carboniferous rocks of Central Europe were deposited. The alternating greywackes, sandstones, shales, and limestones, with their accompanying fossils, indicate changes in the depth and condition of the water, but form throughout a perfectly conformable series. Volcanic action was vigorous in the Devonian period, when diabases and tuffs were emitted at various parts of the area. Towards the close of the Lower Carboniferous period the sea.<