The Geology and Extinct Volcanos of Central FranceJ. Murray, 1858 - 258 psl. |
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xi psl.
... conglomerates , which these geologists persist in asserting not to have produced the mountain or its parasitic cones , which our eyes see them at work upon , but to have filled some supposed pre - existing hollow , afterwards raised by ...
... conglomerates , which these geologists persist in asserting not to have produced the mountain or its parasitic cones , which our eyes see them at work upon , but to have filled some supposed pre - existing hollow , afterwards raised by ...
xv psl.
... 1. The Volcanic Mountain - Its general Outline - Conglomerates . - § 2. Structure - Central Peaks — Trachytic Plateaux and Basalt . § 3. Recent Eruptions . Clinkstone Page 1 6 30 37 40 114 CHAPTER VII . REGION III . - CANTAL § 1.
... 1. The Volcanic Mountain - Its general Outline - Conglomerates . - § 2. Structure - Central Peaks — Trachytic Plateaux and Basalt . § 3. Recent Eruptions . Clinkstone Page 1 6 30 37 40 114 CHAPTER VII . REGION III . - CANTAL § 1.
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... conglomerate , associated with red , blue , and white marls and sandstones ; 2ndly , green and white foliated marls ; 3rdly , limestone or travertin , often oolitic . 66 1. The sandstones and conglomerates forming the first or lowest of ...
... conglomerate , associated with red , blue , and white marls and sandstones ; 2ndly , green and white foliated marls ; 3rdly , limestone or travertin , often oolitic . 66 1. The sandstones and conglomerates forming the first or lowest of ...
18 psl.
... conglomerate composed of fragmentary basalt and scoriæ , cemented by calcareous spar , and finally to a compact basalt . Such examples are found in the Puys de Crouel and de la Poix ( remarkable for its abundant bitumen ) , at ...
... conglomerate composed of fragmentary basalt and scoriæ , cemented by calcareous spar , and finally to a compact basalt . Such examples are found in the Puys de Crouel and de la Poix ( remarkable for its abundant bitumen ) , at ...
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... conglomerate consisting of fragments of basalt and scoria , without pumice or any trachytic matter , united either ... conglomerates . C 2 The Puys de la Piquette and de Marmont , which CHAP . II . 19 CALCAREOUS PEPERINO .
... conglomerate consisting of fragments of basalt and scoria , without pumice or any trachytic matter , united either ... conglomerates . C 2 The Puys de la Piquette and de Marmont , which CHAP . II . 19 CALCAREOUS PEPERINO .
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Pagrindiniai terminai ir frazės
Allier ancient appears Ardèche augite Auvergne basin bed of basalt breccia calcareous calcareous peperino Cantal cellular Central France chain of puys channel character Clermont clinkstone colour columnar compact conglomerate considerable contains covered crater Crown 8vo current of lava deposits distance district domite dyke east Edition elevation eruption evidently excavation Fcap feet felspar fissures flowed formed fragments freshwater formation geologists Gergovia gneiss granitic platform Graveneire Haute Loire heights hill Illustrations lacustrine lake lava lava-current Le Puy Limagne limestone marls mass matter Mezen miles Mont Dore Monts Dôme mountain neighbouring numerous observed occupied olivine Pariou peperino plain Plate plateau points Pomel Pont Portrait Post 8vo prisms probably Puy de Dôme recent remarkable ridge rise river rock sandstone scoriæ side Sioule slope strata stream of lava substance summit surface tertiary thick tion trachyte tuff valley vent Vivarais volcanic cones Vols Woodcuts
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206 psl. - ... 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...