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Natural
Features in Royalston, Massachusetts People often begin researching because they seek the answer to a specific question. As there are a vast number of researchers, there are an equally vast number of questions for which answers may be sought. One person may find an antique table, and so research to learn more about its maker; another may wish to learn about a company for which an ancestor worked; and still others may want to learn more about the people and places referred to in ancestors correspondence or noted in pictures and postcards. I recently received an e-mail inquiry from Tia
Mousseau, who works as a Park Ranger, at Tully Lake, in Royalston. Tia
was interested in learning more about several natural sites in Royalston,
since Tia conducts hikes throughout the summer to many of the local, natural
features. In response, I combed through several Royalston
resources to discover further information about these sites, and Tia
graciously assisted with the identification of the present-day names.
The resources which I consulted are listed below, and the information gleaned
about the various natural features follows. I have chosen to quote
extensively from the historical materials, rather than simply paraphrasing
the information, since I believe the wording of dated materials, may also be
of interest as they stand; for Resources consulted as references for further information about features include the following: Map of Worcester County, Massachusetts, by Henry F. Walling, Sup. of the State Map, Boston : Wm. E. Baker & Co. Publishers, 1857. (hereafter referred to as 1857 Map) Vital Records of Royalston, Massachusetts, To the End of the Year 1849, Worcester : Franklin P. Rice, 1906. (hereafter referred to as Vital Records) The History of the Town of Royalston, Massachusetts,
1762-1917, by Lilley B. Reflections on Royalston, Worcester County, Massachusetts, U.S.A., by Hubert Carlton Bartlett, Fitchburg : The Reflector, 1927. (This book includes a map of the town of Royalston, and is hereafter referred to as Bartlett) Nature's Embellishments in Royalston Royalston, as with many New England towns, has a goodly number of natural land and water features which are matters of considerable interest. Bartlett begins his discussion of Royalston's natural features with a description of geographical feature at the heart of Royalston: "Nature gave the town a 'back-bone' in the form of a ridge of ledgy hills, extending through the middle of the town from its northern limits well down toward its southern extreme, adjoining Athol; her a drop lets Lawrence Brook through from the east to the west side of the ridge, which is continued in Athol as Chestnut Hill. Royalston Common stands on this ridge." There are points on this ridge at the north part of the town from which a large section of the west part of the town can be seen, and many places seem "almost within a stone's throw". However, the only way to reach those places, which seemed to be so near, from that north part of the town, was to go to back to the Common, then by the west road down "Jacobs Hill", making the distance to the nearest places about 3 or 4 miles, and others 5 to 8 miles. This is the reason that Bartlett surmised the Jacobs Hill Road must have been one of the earliest laid out - "...for without it communication between the west part and the Center and other parts of the town must have been extremely difficult..." The topographical features of Royalston, with the ridges and waterways formed, have played key parts in the history of this beautiful New England town. The recognition and admiration of the interplay between the natural features and the daily lives of its residents seems to have been truly appreciated by Royalston's citizens through the years. In contrast to many towns which many name features for famous people of other times and places, Royalston's natural features are, for the most part, named in honor of her own people. Even when a well known and respected 'outsider' came to survey the area for his book, and, while in Royalston, christened one of the town's waterfalls with a name which he thought particularly appropriate, local Royalston citizens appear to have, in large measure, disregarded his chosen name in favor of honoring local residents and the town itself. Below, you will find descriptions of several of
Royalston's natural features and some history of their names. You may
read each by continuing to scroll down this page, or may jump to specific
features by clicking on the following links:
JACOBS HILL is located just northwest from Royalston Center common. Caswell reports that this hill was named for Wightman JACOBS. Wightman JACOBS, son of Nathaniel, became a leader among the Baptists when a young man, and was selected as their pastor being formally ordained and installed in service in 1750, the first minister raised up in Thompson. He remained pastor of that church nearly twenty years. He then relocated to Royalston, in 1769, and was settled as the first pastor of the West Royalston Baptist Church. He served the church as pastor for 16 years. A part of this time his home was in the northerly part of Athol, on Chestnut Hill, and another place that was his abode for some time, was half way up "Jacobs' Hill". Wightman JACOBS died, at the home of his son, Joseph, in Royalston, on 28 March 1801, as a result of a fall. In Reflections on Royalston, Worcester
County, Massachusetts, U.S.A., Bartlett reports the following of
Lawrence Brook: In Reflections on Royalston, Worcester County, Massachusetts, U.S.A., Bartlett includes a map of the Town of Royalston, which shows two ponds situated just west of the Royalston Common. The nearest to the common is identified as Little Pond, and the larger of the two, and furthest west, is shown to be called Long Pond. Caswell writes that Long Pond became known by the name of Tully Pond, and relates 3 possible explanations for the ponds acquiring the newer name of Tully Pond as follows: ...known in the proprietors records only as
Long Pond; its first appearance with the present name of Tully is found
recorded on the town book in 1770, five years later after the town was
incorporated. The source from which this name is derived seems to have
been a subject of much inquiry by antiquarians and writers. Rev. Samuel
Clark in his centennial address delivered at Athol in 1850, gives a tradition
that was commonly accepted for a long time, that the name was derived from an
Indians dog named Tully which in following a deer drove the animal over
the meadows into these waters, and while attempting to seize his prey, was
struck a stunning blow by the fore foot of the deer and held under the water
until poor Tully was drowned.
Caswell reports there are at least 3 waterfalls connected with deep gorges in
SPIRIT FALLS (This falls appears to have had no name in the early resources; presently known as Spirit Falls): Known presently by the name of Spirit Falls, this
name apparently did not come into use until after ca. 1927, since it is
described, but remains unnamed, in early Royalston resources. This
waterfall, per Caswells description, appears to be located about 1 mile
west of the Royalston Common at Royalston Center, emptying into Long Pond,
also known as Tully Pond. Caswell describes it thus: ...About
a mile west of the meeting house and center of the town, is a deep valley
running north and south, nearly across the town. Near the meeting house
is a pond [Little Pond] which empties itself into this valley by plunging
rapidly down a steep declivity which must be eight hundred or a thousand feet
high. It then empties into another large pond [Long Pond / aka Tully
Pond], or rather a Bartlett writes further of the pond called Little Pond as follows: This Little Pond, near the meeting-house, on the Common, excites the curiosity of to its source of supply, as no brooks empty into it and the water-shed draining into it is limited in territory. It seems probable that some natural breaking-up of the crust left this cavity, and that it is filled mainly by water seeping through the fissures in the ledges of the higher ridge at the north. It seems reasonable to suppose that the water secured through the artesian wells driven around the Common in recent years [ca. before 1927], may come from substantially the same sources as that which fills Little Pond; that pond may be something like a natural artesian well. Bartlett reports that Prof. Edward Hitchcock, of
Amherst College, had visited Bartlett writes further of the recreational use
of Little Pond in yesteryear: Along in some of the years between
1850 and 1860 a row-boat of fair proportions was in commission on Little
Pond. It might have been built and launched at an earlier time, by the
fellows at the furniture shop; but in the years mentioned it was captained
and manned by boys from the FRYE, WHEELER, PIERCE, and BULLOCK families, and
probably others, who gallantly took high-school girls and others on limited
trips. The boat was of a flat-bottom, raft-like construction, which
would not easily upset; and so long as it did not
Apparently, this falls did not yet have a known name
at the time of Prof. Hitchcocks visit. By 1870, however, it had
become known as Forbes Falls, no doubt due to its location
on Calvin FORBES land. Royalstons Vital Records report a Calvin
FORBES was born, on 29 December 1783, in Royalston, to a James and Abigail
FORBES. James and Abigail also had several other children born in
Royalston during the 1780s and 1790s, including James (born 10 Oct 1788) and
John (born 4 Jan 1801). The Royalston Vital Records also report the
marriage intentions of a Calvin FORBES, on 27 April 1807, to Polly BUFFUM, of
Richmond, in addition to the births of children to Calvin and Polly as
follows: Nelson (born 17 Oct 1807), Silas (born 8 May 1809), Willard
(born 15 May Forbes Falls, also known in yesteryear as "The Royal Cascade", is referred to presently by the name of "Royalston Falls"; retaining a portion of one of the original names. DOANE FALLS (also known as The Republican
Cascade): Bartlett includes a quote from Prof. Hitchcock,
concerning this falls as well. Hitchcock wrote of Doane Falls, ca.
1838, as follows: Its width, indeed, must be as much as 25 feet,
and its depth considerable. In a short distance here the water
descends, at several successive leaps, as much as 200 feet, between high
walls of gneiss and granite. Toward the upper part of the descent,
several mills are erected, but a small part only of the water power is
employed. Below the mills the stream passes into the woods; and toward
the lowest part of the descent, we get a single view of two falls of about 25
feet each. There is more of beauty and less of wildness at this spot
than at The Royal Cascade. This stream also has been, and
still more extensively can be, applied to useful purposes. Perhaps,
therefore, considering the character of our political institutions, and our
well known reputation for utilitarian tendencies, this, rather in contrast to
The Royal Cascade, may be denominated The Republican
Cascade. But if I can induce persons of taste and leisure to
visit it, I care but little for the name. This falls came to be called by the name of Doane
Falls in honor of Amos Doane, who owned the land around the falls, and
built a large mill nearby. Caswell writes the following of the DOANE
Family: The 1857 map reports an A. DOANE residence near
the location where |
Copyright 2001-2013, by Ann
McRoden Mensch.
Ann McRoden Mensch
is a professional historical genealogist, researching on-site and with the vast
resources of the Allen County Public Library, in Fort Wayne, Indiana. For
professional research assistance, see her web page at <http://sites.google.com/site/annmcrodenmensch/>.
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