General History of Connecticut, from Its First Settlement Under George Fenwick to its Latest Period of Amity with Great BritainPeters, Samuel
History
General History of Connecticut, from Its First Settlement Under George Fenwick to its Latest Period of Amity with Great Britain
Peters, Samuel
Connecticut -- History -- Colonial period, ca. 1600-1775; Connecticut -- History -- Revolution, 1775-1783
Connecticut is situated between 41 and 42 degrees of north latitude,
and between 72 and 73 degrees 50 minutes west longitude from London.
Notwithstanding, from this latitude, New-London lies 600 miles nearer
the line than the capital of England, the winter sets in there a month
before it does here, and not only continues longer, but is more
severe. This extraordinary coldness is said by naturalists to arise
from the vast frozen lakes and rivers, and mountains eternally covered
with snow, throughout the northernmost parts of America. The mountains
may have their share in producing this effect; but I am apt to think
the lakes and rivers have a contrary influence. If I ask why lands
bordering on them are three weeks earlier in their productions than
lands ten miles distant, it will readily be imputed to the warmth of
the air, occasioned by the reflection of the sun’s rays from the
water. On the same principle, I argue that the rays of the sun,
multiplied and reflected by ice also, will render the air warmer. But
it may be further said, that the cause is perhaps to be ascribed to
the soil being more sandy and loose near a lake or river, and,
therefore, naturally warmer than that which is remote and not sandy. I
reply, that there are loose, sandy plains, twenty miles off from any
lake or river, three weeks later in their products, and very
perceptibly colder, than lands upon them. It would be to no purpose to
urge that the damps and fogs from unfrozen lakes, rivers, &c. &c.
affect the distant but not the adjacent country; because I apprehend
there are no unfrozen lakes and rivers in the north of America in
winter. Besides, if there were, the mists arising from them would
naturally be intercepted by the first mountains or forests they
approached. But I pretend to little philosophical knowledge in these
matters; I write from experience, and can thence, moreover, assert
that mountains with snow upon them are not so cold as they would be
without it; and that mountains covered with trees are the coldest of
all places, but without trees are not so cold as forests or plains. I
am clearly of opinion, therefore, that not the lakes or rivers, but
the infinite quantity of timber in the immense regions of
North-America, whether upon mountains or not, is the grand cause of
the coldness of the winters in Connecticut. I will add, moreover, in
support of my argument, that beasts, in the coldest weather, are
observed to quit the woods and woody mountains for lakes, rivers, and
cultivated open country; and that Connecticut, having lost most of its
timber, is by no means so intensely cold in winter as it was forty
years ago, and as Susquehanna is at present, a wilderness in the same
latitude. The snow and ice commonly cover the country, without rains,
from Christmas to March; then rains, attended with boisterous winds
from the north and east, melt the snow, which converting brooks into
rivers and rivers into seas, in four or five days the ice is rent from
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