One of the undoubted geological truths is that sedimentary layers can be more or less complete modifications through the action of fire rocks that were initially classified as "transitional" because they were distinctive in their features how would posredstvom link between rocks of fiery origin, lying under them, and the sedimentary layers lying on top of them, are now time nothing like sedimentary layers, transformed as part of your and in appearance from the intense heat of adjacent molten substances, that's why these rocks are called "metamorphic". The latest studies have also shown that these metamorphic rocks are not all the same ancient thought of before. In addition to primary and secondary layers, modified by the action of fire, there are modified such the same way the layers of tertiary origin, and they occur often a distance of some quarter of a mile from points of contact with neighboring granite. This process, needless to say, fossils exterminated. "In other cases, says sir Charles Lyell, dark limestones containing abundant shells and corals become white statuary marble, and hard clay, containing vegetable and other the remains were transformed into slate, known as slate resin slate or hornblende; from organic bodies have not disappeared." Next is almost an indisputable truth that all kinds of mining rocks of plutonic origin are in essence the product of sedimentary strata underwent complete melting. We have several examples of what granite and gneiss, chemical composition of which is identical, passed one another; so, in Vallorcine, near Mont Blanc, where both breeds come in contact with one another, it is noticed that "each of them is known modifications of their mineral characteristics. Granite, still staying nanakorn, begins to stir with green particles; with the other hand, talkaway gneiss takes grantourismo device keeping your naslano".
1 comment:
One of the undoubted geological truths is that
sedimentary layers can be more or less complete modifications
through the action of fire rocks that were initially classified as
"transitional" because they were distinctive in their features
how would posredstvom link between rocks of fiery origin, lying
under them, and the sedimentary layers lying on top of them, are now
time nothing like sedimentary layers, transformed as part of
your and in appearance from the intense heat of adjacent molten
substances, that's why these rocks are called "metamorphic". The latest
studies have also shown that these metamorphic rocks are not all
the same ancient thought of before. In addition to primary and secondary
layers, modified by the action of fire, there are modified such
the same way the layers of tertiary origin, and they occur often
a distance of some quarter of a mile from points of contact with neighboring
granite. This process, needless to say, fossils
exterminated. "In other cases, says sir Charles Lyell, dark
limestones containing abundant shells and corals become white
statuary marble, and hard clay, containing vegetable and other
the remains were transformed into slate, known as slate resin
slate or hornblende; from organic bodies have not disappeared."
Next is almost an indisputable truth that all kinds of mining
rocks of plutonic origin are in essence the product of sedimentary strata
underwent complete melting. We have several examples of what
granite and gneiss, chemical composition of which is identical, passed
one another; so, in Vallorcine, near Mont Blanc, where both breeds come in
contact with one another, it is noticed that "each of them is
known modifications of their mineral characteristics. Granite, still
staying nanakorn, begins to stir with green particles; with
the other hand, talkaway gneiss takes grantourismo device
keeping your naslano".
Post a Comment