History of Piscataquis County, Maine
From
A Gazetteer of the
State of Maine
By Geo. J. Varney
Published by B. B. Russell, 57 Cornhill,
Boston 1886
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Piscataquis County Towns - Brownville - Dover - Elliotsville - Foxcroft - Garland - Greenville - Guilford - Howard - Kingsbury - Medford - Milo - Monson - Orneville - Parkman - Sangerville - Sebec - Shirley - Williamsburg |
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Piscataquis County is the central region of Maine.
Penobscot County bounds it on the east and south, Somerset on the west and south, and Aroostook on the north and
east. On the western boundary lies Moosehead Lake, and opposite, on the eastern side, are Peinadumcook and Millinoket
lakes. This county also constitutes a large part of the most elevated region of Maine, lying, on an average upwards
of 1200 feet above the sea. Midway of its eastern border rises Katahdin to a height of 5,385 feet above sea level.
Several others rise many hundreds of feet above the surrounding region, and to thousands of feet above the sea.
The greatest height of land appears to be about midway between Moosehead Lake on the west and Pemadumcook on the
east, Chesuncook on the north and Sebec Lake on the south, and again in the region of Mount Katahdin and north-west
thereof. From these tracts the streams flow off in all directions; and between them runs the west branch of the
Penobscot. There is not known to me any other tract of equal extent with this in the world having so many lakes
and ponds. On Pleasant River, in the eastern township of the Bowdoin College grant, and some 20 miles above the
Katahdin Iron Mines, is a marvellous glen, through which the little river makes its wild course,—now leaping down
stupendous cataracts, and anon shooting between towering walls, forming a passage which is the dread of lumbermen,
and quite enrapturing to visitors. In Elliotsville, a township adjoining Greenville on the south-west, is a natural
curiosity which has yet received little attention. It is a fall on a stream called the Little Wilson, of 80 feet
perpendicular. Clapboard bolts have sometimes been driven over this fall, but many of them would be split and quartered
from end to end. The whole of this county is on the north side of the 45th parallel of north latitude. Frosts come
early, the winters are long and snows deep; yet even in the northern part wheat and the other farm products, excepting
corn, ripen abundant crops. When first entered by settlers. this territory was included in Hancock and Kennebec
counties, but when (in 1809) Somerset County was incorporated, the western portion, amounting to three tiers of
townships, was embraced in this new county. In 1816, Penobscot County was incorporated, and all but the three western
tiers of townships above mentioned were included in that county. In 1838, Piscataquis County was incorporated,
taking four tiers of townships from Penobscot, and three from Somerset county,—the most western tier being included
in the Bingham purchase. It then extended in full width to Canada, but in 1844 its northern portion, embracing
about 60 townships, was annexed to Aroostook County. In its present extent it contains more than 100 full townships,
with an area of 3,780 square miles. The townships are generally 6 miles square, lying in regular ranges; the latter
was numbered from the north line of the Waldo patent (now constituting a part of the north line of Waldo County)
the southern tier in Piscataqius County being the sixth range in this enumeration. In its length north and, south,
it includes 16 townships, and in its width, 7. Nearly two-thirds of these townships arc now covered with forests,
and wholly unoccupied, except by the lumber men in their annual pursuit of logs. |
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