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Record W823552217

History of Woodstock, Me., with family sketches and an appendix

2009· book· en· W823552217 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueDigitalCommons (California Polytechnic State University) · 2009
Typebook
Languageen
FieldSocial Sciences
TopicCanadian Identity and History
Canadian institutionsnot available
Fundersnot available
KeywordsAppendixHistoryGeology
DOInot available

Abstract

fetched live from OpenAlex

of the Little Androscoggin Eiver.North Alder Eiver Pond discharges its waters into South Pond, the latter lying wholly in Greenwood, and thence through Ptound Pond in the same town and Alder River, to the Great Androscoggin River at Bethel.In the north-east part of the town, Great and Little Concord Ponds empty their waters through the Concord River into the Androscoggin in Rumford.Shagg Pond, situated a short distance south of the last two, discharges its waters easterly through the adjoining town of Sumner.We have no very im- portant streams of water.The outlet of Bryant's Pond soon passes into Greenwood ; t'iiat of the North Alder River Pond is all in that town.There are numerous brooks fed by smaller mountain streams, but in most of them the water is reduced to a mere thread in summer.Most of the streams have their origin in the mountain region, which is situated a little to the north and east of the center of the town, and flow away from them, towfird every point of the compass.This fact accounts for their insignificance for manufacturing purposes ; the con- formation of the land is such that they cannot unite and form larger streams until they get beyond the limits of the town, if indeed they do at all.The mountain region here referred to occupies about nine square miles, or one-fourth of the entire surface of the town.There are in the region ten distinct out- croppings of the rocky foundation of the earth, and most of the entire surface is unfit for cultivation.An interesting Kame or horse-back enters Woodstock from Bethel toward the north-west part of the town, and passing south-easterly to Pinhook, bears westerly to near Bryant's Pond, and then passes into Greenwood a mile or two below.This ridge was known as the " Whale's Back," long before Woodstock had a settler.This' was probably the bed of an arctic river, and the effects of glacial action are apparent in many parts of the town.-Huge boulders are scat- tered here and there, and ridges of rounded cobbles are found in many places.These are all interesting from the standpoint of the scientist, but they make agriculture tedious.tThe physical features of Woodstock are not unlike much of the surrounding territory.The same general characteristics are observed as we go northwardly to Canada, easterly to Katahdin, westerly to the White Hills and beyond, and south- erly for a considerable distance toward the sea coast.The only important difference that exists is found in the fact that those towns through which the larger rivers pass have broader belts of interval, and conseqiiently more and better arable land.This is true of all the Androscoggin towns, and some others through which some of its more important tributaries pass, such as the Ellis, Bear, the Swift, the Little Androscoggin, and some others.In its physical aspect, there is a close similarity in the entire region, embracing Franklin and Milton Plantations, Woodstock, Greenwood and Albany, and portions of the ad- joining towns, while a larger portion of the towns which circle around this territory are made up of better agricultural terri- tory.The soil of Woodstock is strong, but hard to work.In part compensation for this, we have a large area of most excel- lent grazing lands, and our facilities for sheep husbandry could not very well be improved.The rocky formation of Woodstock is generally granite.In some places, as at Bryant's Pond, are deposits of excellent rift, and valuable for building purposes.There is some resemblance between this and the Quincy granite.It is free from the com- pounds of iron and of other metals, and is therefore durable.The constituents of granite, which are mica, quartz and feldspar, are often found in considerable masses by tliemselves, and in many places they unite and form coarse granite or gneiss.Some small deposits of clay are found in the town, and occa- sionally slaty formations, though not of any great extent.Veins of trap rock are not uncommon.Fine specimens of crystallized quartz are found in some localities, and also other interesting minerals of which quartz forms all but the coloring substances.Mr. Nathan A. Perry, of West Paris, formerly a resident of this town, and who has given much attention to its resulted in wresting Canada from the French, that new settlements could be made away from the coast with any degree of safety.After the close of the year 1760, the great wilderness was pierced by settlers in various directions.There was a general movement all along the line, the lands on the larger rivers being those first selected.Fryeburg, on the Saco, was settled in 1762 by emigrants from Concord, N. H., this being the first settle- ment made within the limits of Oxford county.Settlers also came there from Andover and from other points, and Fryeburg soon became a rallying point for new settlements farther back.Bethel was settled, or a settlement was begun there, in 1773, and Waterford in 1775.Brunswick was also a rallying pomt fof settlers farther up the Androscoggin, and New Gloucester and Gray for the central parts of this County.But the break- ing out of the Eevolutionary war called all the able-bodied men of New Sngland into the army, and the farther settlement of the interior of Maine was postponed.Towards the close of the war settling movements were again resumed, though not pushed with much vigor.Paris was settled from Plymouth and Worcester Counties, in Massachusetts, in 1779, Eumford in 1780, and Buckfield in 1777, by people from New Gloucester.It was after the war closed, that a great rush was made for eastern lands by those who had been in the service.They were generally poor, government money, in which they had been paid, having become worthless, and they turned to the unsettled wilderness as the only place where they could hope to make homes for themselves and their families.There was a great rush of new settlers to the towns before named, and other set- tlements were begun.Sumner was settled in 1783, Norway in 1786 and Peru in 1793.These towns are circled around the territory which now comprises Woodstock, Greenwood, Albany, Milton Plantation and Franklin Plantation, which was still left unsettled.Its rough surface was not inviting to the set- tler, and its situation away from any considerable water course kept settlers away from it."To all to whom these presents shall come : Greeting : " Whereas, the Legislature of the Commonwealth of Massachusetts, in General Court assembled, by a resolve passecj^n the 27th day of February, A. D. 1707, granted to the Trustees of Dummer Academy, and to their successors, half a township of laud ^ix miles square for the use of said Academy, to be laid out or assigned by the committee for the sale of eastern lands, in some of the unappropriated lands in the District of Maine, belonging to said Commonwealth, excepting all lands within six miles of Penobscot River, with the reservations and conditions which have been usually made in sim- ilar cases; and whereas, Loturop Lewis, Surveyor, in pursuance of instruc- tions to him given by the committee for the sale of eastern lands, did in the month of November, 1799, return to the said committee a plan of the tract of land hereinafter described for the purpose aforesaid : Now, therefore, know ye that we, the undersigned, whose seals are hereunto affixed, being a major part of the committee for the sale of eastern lands, in conformity to the resolve aforesaid, do by these presents convey and confirm to the Trustees of Dummer Academy, and to their successors, a certain tract of land in the County of Cumberland, being part of township number three and bounded as follows: Beginning at the northwesterly corner of Paris and thence running easterly and bounded by said Paris, three miles and eight rods to a stake ; then turning and running north thirty degrees west, six miles to a rock maple tree marked ; then turning and running south sixty-eight and one-half degrees, three miles and eight rods to township number four (now Greenwood) ; then turning and running south thirty degrees east by township number four, to the first bound, containing eleven thousand, five hundred and twenty acres ; conditioned, however, that the said grantees shall lay out and convey to each settler who settled on said tract before the first day of January, 178-1, one hundred acres of land, to be so laid out as best to include his improvements, and be least injurious to the adjoining land; that they shall settle on said land ten families in six years, including those now settled thereon, and that they shall lay out three lots of one hundred and sixty acres each, for the following uses, viz : one lot for the use of the ministry, one for the first settled minister, his heirs and assigns, and one lot for the use of schools in the said ti'act.To have and to hold, &c." In testimony whereof, we have hereunto set our hands and seals the 5th day of March, a. d. 1800.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Science and technology studies
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Other · Consensus signal: Other
Teacher disagreement score0.339
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0030.000
Science and technology studies0.0000.003
Scholarly communication0.0000.001
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.015
GPT teacher head0.201
Teacher spread0.186 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it