An Examination of Dr. Burnet's Theory of the Earth: With Some Remarks on Mr. Whiston's New Theory of the Earth. Also an Examination of the Reflections on the Theory of the Earth; and a Defence of the Remarks on Mr. Whiston's New Theory |
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Pagina 97
Having thus determined the proportion of the centrifugal force at the Aquator to
the force of gravity , it will be easy from thence to shew their proportions in any
parallel , for it is compounded of the proportion of i to 289 , and of the co - fine of
the ...
Having thus determined the proportion of the centrifugal force at the Aquator to
the force of gravity , it will be easy from thence to shew their proportions in any
parallel , for it is compounded of the proportion of i to 289 , and of the co - fine of
the ...
Pagina 104
을 - = pr - inr which equation expresses the nature of the curve that is made by
the section of the earth with a plane through its poles , and by this , the proportion
of the axis of the earth to the diameter of the æquator may be easily determined ...
을 - = pr - inr which equation expresses the nature of the curve that is made by
the section of the earth with a plane through its poles , and by this , the proportion
of the axis of the earth to the diameter of the æquator may be easily determined ...
Pagina 169
The whole problem then is plainly reduced to this ; Having two Cylinders or
Columns of the same intensive gravity , but of different heights that swim in any
Fluid , to find what proportion the parts or heights immerged bear to one another .
The whole problem then is plainly reduced to this ; Having two Cylinders or
Columns of the same intensive gravity , but of different heights that swim in any
Fluid , to find what proportion the parts or heights immerged bear to one another .
Pagina 237
... would not be the ten millionerh part of what is upon the present Sea ; and the
vapours raised from the Abyss , would be less than those which are raised from
the Sea very near in the same proportion , tion . Has not the Theorist now
mended ...
... would not be the ten millionerh part of what is upon the present Sea ; and the
vapours raised from the Abyss , would be less than those which are raised from
the Sea very near in the same proportion , tion . Has not the Theorist now
mended ...
Pagina 328
... and that time , and had troubled himself a little further to calculate the
proportion of the quantity of heat that was in the Primitive Earth upon his
Hypothesis , to that which is in our present Earth , he would have found the
mistake was not on my ...
... and that time , and had troubled himself a little further to calculate the
proportion of the quantity of heat that was in the Primitive Earth upon his
Hypothesis , to that which is in our present Earth , he would have found the
mistake was not on my ...
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An Examination of Dr. Burnet's Theory of the Earth: With Some Remarks on Mr ... John Keill Volledige weergave - 1734 |
An Examination of Dr. Burnet's Theory of the Earth: With Some Remarks on Mr ... John Keill Volledige weergave - 1734 |
An Examination of Dr. Burnet's Theory of the Earth: With Some Remarks on Mr ... John Keill,John Maupertuis Geen voorbeeld beschikbaar - 2013 |
Veelvoorkomende woorden en zinsdelen
Abyſs according Æquator againſt allow alſo anſwer appear argument attraction Author Axis becauſe believe Bodies caſe cauſes Center centrifugal force Chaos Circle Comet conſequently conſider continually Cruſt Defender Deluge demonſtrated deſcend Diameter diſtance drawn Earth eaſily effect endeavour equal Equator evident Examination face fall fame Figure firſt fluid follow give given gravity greater greateſt half heat Hypotheſis imagine impoſſible Land Laws leaſt leſs matter means miles moſt motion Mountains move muſt nature neceſſary never Obſervations Ocean Philoſophers plain Planets Poles poſition preſent Primitive principles produce Properties proportion prove quantity raiſed reaſon riſe Rivers round ſaid ſame ſays ſee ſeems ſelf ſhould ſince ſolid ſome ſpace Stars ſtill ſuch ſufficient ſuppoſe ſurface tells thence Theoriſt Theory theſe thing thoſe thought thro tion true turn uſe vapours weight whole whoſe World
Populaire passages
Pagina 232 - And the waters prevailed exceedingly upon the earth ; and all the high hills, that were under the whole heaven, were covered.
Pagina 233 - God made a wind to pass over the earth, and the waters assuaged ; the fountains also of the deep and the windows of heaven were stopped, and the rain from heaven was restrained ; and the waters returned from off the earth continually : and after the end of the hundred and fifty days the waters were abated.
Pagina 232 - And the flood was forty days upon the earth; and the waters increased, and bare up the ark, and it was lift up above the earth.
Pagina 232 - In the six hundredth year of Noah's life, in the second month, the seventeenth day of the month, the same day were all the fountains of the great deep broken up, and the windows of heaven were opened. And the rain was upon the earth forty days and forty nights.
Pagina 29 - ... which being once filled, all the overplus of water that comes thither runs over by the lowest place, and breaking out by the sides of the hills forms single springs...
Pagina 15 - Heaven and the earth ; and the earth was without form, and void, and darknefs was upon the face of the deep ; and the fpirit of God moved upon the face of the waters.
Pagina 28 - The trees of the Lord are full of sap; the cedars of Lebanon, which he hath planted; Where the birds make their nests: as for the stork, the fir trees are her house. The high hills are a refuge for the wild goats; and the rocks for the conies.
Pagina 29 - Valleys between the Ridges of the Hills, and coming to unite, form little Rivulets or Brooks : many of thefe again meeting in one common Valley, and gaining the plain Ground, being grown...
Bibliografische gegevens
| Titel | An Examination of Dr. Burnet's Theory of the Earth: With Some Remarks on Mr. Whiston's New Theory of the Earth. Also an Examination of the Reflections on the Theory of the Earth; and a Defence of the Remarks on Mr. Whiston's New Theory |
| Auteur | John Keill |
| Editie | 2 |
| Uitgever | H. Clements, 1734 |
| Oorspronkelijk uit | de University of Michigan |
| Gedigitaliseerd | 14 april 2006 |
| Lengte | 414 pagina's |
| Citatie exporteren | BiBTeX EndNote RefMan |