Advanced Text book of Geology Descriptive And Industrial
Advanced Text book of Geology Descriptive And Industrial
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In our eReader you can find the full English version of the book. Read Advanced Text book of Geology Descriptive And Industrial Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book Advanced Text book of Geology Descriptive And Industrial
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THE OOLITIC SYSTEM, EMBEACING THE LIAS, THE OOLITE, AND WEALD EN GROUPS.
246. WHATEVER doubt may be entertained as to the epoch of some of the triassic strata, there can be none as to the biological relations of the system we are now about to consider. We have passed the boundary, as it were, of the older rocks, and have fully entered upon the upper or younger secondary formations. Or, speaking palseontologically, we have traced the history of systems whose fossils are all of Palaeozoic types, ...and now proceed to interpret the records of those that are unmistakably Mesozoic. The grand types and patterns are still the same radiate, mol- luscan, articulate, and vertebrate ; but the modifications of these types are new, and the consequent organisation higher and more complex. We now take farewell of the graptolites, cystideaiis, trilobites, and eurypterites of the Silurian seas of the gigantic crustaceans and bone-encased fishes of the old red sandstone of the sigillaria, stigmaria, lepidodendron, and other endogenous forms of the coal period of the cup-in-cup, honeycomb, chain, spider- web, and other corals of the Devonian and mountain limestones of the huge reptile-like fishes that swarmed in the Carboniferous seas, and are introduced to other species and newer forms of vitality.
What to read after Advanced Text book of Geology Descriptive And Industrial?
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To quickly assess the difficulty of the text, read a short excerpt:
THE OOLITIC SYSTEM, EMBEACING THE LIAS, THE OOLITE, AND WEALD EN GROUPS.
246. WHATEVER doubt may be entertained as to the epoch of some of the triassic strata, there can be none as to the biological relations of the system we are now about to consider. We have passed the boundary, as it were, of the older rocks, and have fully entered upon the upper or younger secondary formations. Or, speaking palseontologically, we have traced the history of systems whose fossils are all of Palaeozoic types, ...and now proceed to interpret the records of those that are unmistakably Mesozoic. The grand types and patterns are still the same radiate, mol- luscan, articulate, and vertebrate ; but the modifications of these types are new, and the consequent organisation higher and more complex. We now take farewell of the graptolites, cystideaiis, trilobites, and eurypterites of the Silurian seas of the gigantic crustaceans and bone-encased fishes of the old red sandstone of the sigillaria, stigmaria, lepidodendron, and other endogenous forms of the coal period of the cup-in-cup, honeycomb, chain, spider- web, and other corals of the Devonian and mountain limestones of the huge reptile-like fishes that swarmed in the Carboniferous seas, and are introduced to other species and newer forms of vitality.
What to read after Advanced Text book of Geology Descriptive And Industrial?
You can find similar books in the "Read Also" column, or choose other free books by David Page to read onlineMoreLess
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