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 78
Also an Examination of the Reflections on the Theory of the Earth; and a Defence
of the Remarks on Mr. Whiston's New Theory John Keill. every one that wanted
water must go as far as the equator to fetch it . No says the Theo rist there was no
...
Also an Examination of the Reflections on the Theory of the Earth; and a Defence
of the Remarks on Mr. Whiston's New Theory John Keill. every one that wanted
water must go as far as the equator to fetch it . No says the Theo rist there was no
...
Pagina 209
One argument I brought was , . . that by the present position of the Earths Axis ,
we receiv ' d more of the Suns heat , than if it had mov ' d always in the Equator ;
and if our heat at present is not too great for us , ( as without doubt it is not ) it was
...
One argument I brought was , . . that by the present position of the Earths Axis ,
we receiv ' d more of the Suns heat , than if it had mov ' d always in the Equator ;
and if our heat at present is not too great for us , ( as without doubt it is not ) it was
...
Pagina 273
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 John Keill. « teen miles deeper at the
Equator than ...
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 John Keill. « teen miles deeper at the
Equator than ...
Pagina 275
That the Sea ought to be seventeen miles deeper at the Equator than at the Poles
; he would have done well to have offered us some of his abstruse reasons why it
ought to be fo , for a common Reader , that is not used to his profound way of ...
That the Sea ought to be seventeen miles deeper at the Equator than at the Poles
; he would have done well to have offered us some of his abstruse reasons why it
ought to be fo , for a common Reader , that is not used to his profound way of ...
Pagina 276
to the Poles , it were a paradox to say , that the water will not descend from the
Equator to the Poles ; but it would be a greater to suppose , that Rivers would rise
from thence to the Equator . Well , if this be a paradox , I hope he will thank me if I
...
to the Poles , it were a paradox to say , that the water will not descend from the
Equator to the Poles ; but it would be a greater to suppose , that Rivers would rise
from thence to the Equator . Well , if this be a paradox , I hope he will thank me if I
...
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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 |