Principles of Geology: Being an Attempt to Explain the Former Changes of the Earth's Surface, by Reference to Causes Now in Operation, Volym 1J. Murray, 1830 - 511 sidor |
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afterwards alluvial ancient animals Apennines appear basalt beds Calabria calcareous carbonic acid carboniferous causes century changes channel cliffs climate coast cone considerable continued convulsions crater deep delta deluge deposits depth distance district earth earthquakes elevation eruption estuary Etna fissures flood flowed formation formed former fossil geological geologist globe gradually granite heat height Herculaneum hills hundred feet igneous igneous rocks inhabitants Ischia island isles Journ lakes land lapilli latitudes lava limestone marine mass matter Mediterranean miles mineral modern Monte Nuovo mountains mouth nature observations ocean origin period phenomena plain plants Pompeii present produced Puzzuoli quantity regions rise river rocks sand scoriæ sediment shells shock shores Sicily side Solfatara species springs Strabo strata stream submarine subterranean movements supposed surface temperature theory thousand feet thrown tides tion torrents trachyte tract travertin tuff valleys vapour vegetable Vesuvius violent volcanic whole