Memoirs of the Connecticut Academy of Arts & SciencesArchon Books, 1810 - 42 páginas |
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Página 18
... reason to think the climate has suffered any considerable alte ration . Dr. Williams mentions the year 401 , when the Eux- ine was covered with ice for 20 days , as an evidence that the climate was formerly colder than at present ; and ...
... reason to think the climate has suffered any considerable alte ration . Dr. Williams mentions the year 401 , when the Eux- ine was covered with ice for 20 days , as an evidence that the climate was formerly colder than at present ; and ...
Página 20
... reason to suppose the least melioration of that climate within 2000 years . The next series of facts to prove a great mitigation of the cold in winter , consists of what authors have record- ed of ancient Gaul and Germany . Diodorus ...
... reason to suppose the least melioration of that climate within 2000 years . The next series of facts to prove a great mitigation of the cold in winter , consists of what authors have record- ed of ancient Gaul and Germany . Diodorus ...
Página 28
... reason- ing which has principally supported the hypothesis of a modern diminution of cold in winter . Authors have mentioned and described the severe winters ; while or- dinary seasons have passed unnoticed ; and this is the source of a ...
... reason- ing which has principally supported the hypothesis of a modern diminution of cold in winter . Authors have mentioned and described the severe winters ; while or- dinary seasons have passed unnoticed ; and this is the source of a ...
Página 30
... reason why Greece and Italy are more tem- perate than other countries under the same parellels of latitude . Let us now attend to the evidence of a mitigation of the cold of American winters . The first proof adduced by Dr. Williams ...
... reason why Greece and Italy are more tem- perate than other countries under the same parellels of latitude . Let us now attend to the evidence of a mitigation of the cold of American winters . The first proof adduced by Dr. Williams ...
Página 42
... reason to suppose that the inclination of the earth's axis to the plane of its orbit has ever been varied ; but strong evidence to the contra- ry . If this inclination has always been the same , it fol- lows that the quantity of the ...
... reason to suppose that the inclination of the earth's axis to the plane of its orbit has ever been varied ; but strong evidence to the contra- ry . If this inclination has always been the same , it fol- lows that the quantity of the ...
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Abyſs acid ancient appears arches atmosphere auroral light body cause Celtic Chronic Debility circle circumference climate cold comet Connecticut considerable costiveness covered with ice Cronus Danube debility degree deity diameter diarrhea digestion disease dyspeptic earth effect ELIZUR WRIGHT equal evidence fact feet fermentation fever figure fire fluid formed frequently frost gastric liquor Gaul Greek heat Hebrew Hence Hesiod instances intestines iron Italy JEREMIAH DAY Judea language Latin latitude less manner mass mentioned meteor meteoric stones Midian mild miles modern months moon morbid motion mountains nature observed occasion orbit origin Ovid perihelion perpendiculars persons probably produced prove pyrites quantity remarkable rivers Romans root says severe signifies snow spring stomach Strabo supposed surface temperature theſe Thrace tion usually vapor viscus weather whin stone whole wind winter word Yale College
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Página 68 - From a careful comparison of these facts," he says, " it appears that the weather, in modern winters, is more inconstant, than when the earth was covered with wood, at the first settlement of Europeans in the country ; that the warm weather of autumn extends further into the winter months, and the cold weather of winter and spring encroaches upon the summer ; that the wind being more variable, snow is less permanent, and perhaps the same remark may be applicable to the ice of the rivers. These effects...
Página 42 - evidence of things not seen," in the fulness of Divine grace ; and was profound on this, the greatest concern of human life, while unable even to comprehend how the " inclination of the earth's axis to the plane of its orbit" could be the cause of the change of the seasons.
Página 40 - A change in our climate, however, is taking place very sensibly. Both heats and colds are become much more moderate within the memory even of the middle-aged. Snows are less frequent and less deep. They do not often lie, below the mountains, more than one, two, or three days, and very rarely a week. They are remembered to have been formerly frequent, deep, and of long continuance. The elderly inform me, the earth used to be covered with snow...
Página 202 - Justice; the first to whom mortals raised temples ; represented as holding a sword in one hand, and a pair of scales in the other.
Página 37 - The frost was so great and continual this winter, that all the bay was frozen over, so much and so long, as the like, by the Indians...
Página 172 - ... thirty on the other (some allowance being made for the resistance of the air and the motion of the earth), the body will revolve in an ellipsis, returning in regular periods. Now, the velocity of the meteors, which have been observed, has generally been estimated to be rather more than three hundred miles in a minute. In some instances it is perhaps too great to suffer the body ever to return ; but in most cases, it is calculated to be such as would be necessary in describing the lower part of...
Página 142 - The attention of Judge Wheeler was first drawn by a Sudden flash of light, which illuminated every object. Looking up he discovered in the north a globe of fire, just then passing behind the cloud, which obscured, though it did not entirely hide the meteor. In this situation its appearance was distinct, and well defined, like that of the sun seen through a mist. It rose from the north, and proceeded in a direction nearly perpendicular to the horizon...
Página 149 - All the stones, when first found, were friable, being easily broken between the fingers ; this was especially the case, where they had been buried in the moist earth ; but by exposure to the air, they gradually hardened. This stone was all in fragments, none of which exceeded the size of a man's fist, and was rapidly dispersed by numerous visitors, who carried it away at pleasure. Indeed we found it difficult to obtain a sufficient supply of specimens of the various stones, an object, which was at...