USCTE PRISM Stone, 1849, Delaware-Maryland
Posted by: Groundspeak Regular Member seventhings
N 39° 40.224 W 075° 47.316
18S E 432362 N 4391473
USCTE PRISM Stone, 1849, DE-MD, is a dressed granite stone that once marked the location of the DE-MD-PA tri-state boundary intersection point.
Waymark Code: WMMY8
Location: Delaware, United States
Date Posted: 08/21/2006
Published By:Groundspeak Premium Member stvanme
Views: 48

USCTE PRISM Stone, 1849, Delaware-Maryland, is a US Corps of Topographical Engineers (USCTE) dressed granite stone set by Lt Col J. D. Graham in 1849 that once marked the location of the DE-MD-PA tri-state boundary intersection point. This granite stone replaced a roughly dressed gneiss stone that Mason and Dixon set in 1766 to demarcate the intersection of the “North Line” and “Arc Line” segments of the boundary line that ran northerly from the southwest corner of Delaware to the eastern end of the “West Line” (the southern boundary of Pennsylvania). Due to a boundary adjustment in the 1920’s, today it marks the Delaware-Maryland boundary. It is in both the NGS and Geocaching databases as station MD DEL BDRY INTERSEC STONE 2, PID = JU3846: (visit link) and (visit link) .

The stone is a three-sided granite shaft. It is about 12 inches on a side and projects about 42 inches. The north face is inscribed with the letter “P”, the names of the commissioners who oversaw Graham’s survey, and the date “1849”. The west face is inscribed with the letter “M”, and the southeast face with the letter “D”. The stone is very weathered (though the inscribed characters are readily discernable) and all the horizontal and vertical edges are badly chipped. The stone is located 69 feet southeast (155 degrees true) of the modern triangulation station PRISM, PID = JU3855. It is in a split-rail and wood pole enclosure in a wooded area in the northwest section of the Stine-Haskell Labs facility of DuPont. This is a secure facility: it is not open to the public and gaining authorized access is difficult. For this reason, I decline to include any additional environmental references.

Lying within the Prism Stone’s enclosure is a roughly dressed, dark gray gneiss stone of the type, shape and size used by Mason and Dixon to demarcate the “Arc Line” in 1766. According to Roger Nathan’s 1984 recovery (reported in the Delaware Geological Survey’s datasheet for this station), the old stone is, in fact, the original Mason-Dixon stone that stood on this spot. Mason and Dixon surveyed this position on or about June 5, 1765, and set the original stone here on or about June 18, 1765.

To reach the Stine-Haskell Labs from Exit 109 off Interstate Highway 95 south of Newark, DE, go northeast on MD State Highway 279 for about 1.15 miles to the MD-DE boundary line. Continue northeast, now on DE State Highway 2, for about 0.8 miles to the Stine-Haskell main gate on the left. Travel beyond the main gate is possible only under escort from armed security personnel. They know where the Prism Stone is located.

HISTORY OF THE ARC LINE
The Arc Line forms a small portion of the boundary line between Delaware and Maryland. It is a 1.47-mile segment of the Twelve Mile Circle boundary line centered on the courthouse at New Castle, DE. It extends north and south from the western-most point of the Circle, and is marked with nine surviving historical stones that are described below.

In 1760, after 80 years of dispute and failed negotiations between the proprietors of Delaware and Pennsylvania (the Penn Family) and the proprietors of Maryland (the Calvert Family), the Court of Chancery ratified a Final Agreement between the parties regarding the boundaries of those three colonies. Among the Court’s determinations were (paraphrased):

a. The Twelve Mile Circle forming the northern boundary line of Delaware with Pennsylvania was to be centered on the cupola of the New Castle courthouse and measured horizontally as a radius,
b. The southwest corner of Delaware was to be the “Middle Point” of a line to be run from Cape Henlopen on the Atlantic coast (the modern Fenwick Island) across the Delmarva Peninsula,
c. The western boundary of Delaware was to be a line (the “Tangent Line”) run northerly from the Middle Point to a point tangent (the “Tangent Point”) with the Twelve Mile Circle,
d. The Tangent Line was to be run due north (the “North Line”) from the Tangent Point until it intersected a line of constant latitude (the “West Line”) fifteen miles south of the most southerly point in Philadelphia,
e. If any portion of the Twelve Mile Circle extended west beyond the North Line, the area within the Circle would remain Delaware territory (it did, and the portion of the colony’s boundary that the extending Circle formed would later be known as the “Arc Line”), and,

Prior to its 1760 ruling, the Court had appointed local surveyors to run the Trans- peninsular Line and, then, to run the Tangent Line northerly to the Twelve-Mile Circle boundary line. In 1750-1751, the surveyors ran and marked the Transpeninsular Line. In 1761, the surveyors began to run the Tangent Line but, after about two years’ work, the task proved to be beyond their technical abilities. In August, 1763, the proprietors of the two colonies engaged Charles Mason and Jeremiah Dixon to complete this line, and to survey and mark all the boundary lines between Maryland and the Penns’ two colonies.

In 1764, Mason and Dixon accepted the colonial surveyors’ determinations of the Middle Point and the Tangent Point and ran the Tangent Line. In June, 1765, Mason and Dixon ran a line due north from the Tangent Point and established both the Arc Line and the North Line segments of the Delaware-Maryland boundary line. That month, they also marked the Arc Line with five unmarked dark gray gneiss stones (one at the Tangent Point and four in the “periphery” of the Circle. In November, 1766, they added a standard limestone intermediate mile stone that served to mark the 83rd mile north of the southwest corner of Delaware.

In 1849, Lt. Col. J. D. Graham, US Corps of Topographical Engineers (USCTE), re-surveyed the Arc Line and the North Line. The USCTE survey set new stones at the north and south ends of the Arc Line, and an additional stone on the line about 0.7 miles north of the Tangent Point.

According to my calculations, the Arc Line is 1.467 miles long with a chord of 1.466 miles. At its widest, the sliver of land between the Arc Line and an imaginary line run due north from the Tangent Point is 118.3 feet. The area gained by Delaware from the specification that created the Arc Line is 14.01 acres.

The Arc Line was marked with nine historical stones, all of which survive:

1. The “Tangent Stone”, a granite 1849 US Corps of Topographical Engineers (USCTE) survey stone with PID = JU3840 (BOUNDARY MON 82 TANGENT STONE).

2. Abutting the Tangent Stone is roughly-dressed gneiss stone set by Mason and Dixon in June, 1765. This stone does not have a PID.

3. About 0.4 miles north of the Tangent Stone, a stone with PID = JU4144, (BOUNDARY ARC STONE 1 DE MD RESET) originally set by Mason and Dixon in June, 1765. This stone lies in a chamber below the southwest-bound lanes of MD State Highway 279 / DE State Highway 2 (Elkton Road). The DGS describes the stone as an unmarked, obelisk-shaped piece of granite.

4. About 0.7 miles north of the Tangent Stone, a roughly-dressed gneiss stone with PID = JU3851 (BOUNDARY ARC STONE 2 DE MD) set by Mason and Dixon in June, 1765. It is a 7 x 12 x 20-inch, unmarked gneiss stone of the same type as the stone that abuts the Tangent Stone.

5. About 0.7 miles north of the Tangent Stone (and about 41 feet north of ARC STONE 2), a granite 1849 USCTE granite stone with PID = JU3852 (BOUNDARY ARC STONE 3 DE-MD).

6. About 1.0 miles north of the Tangent Stone, a dressed stone with PID = JU3850 (BOUNDARY ARC STONE 4, BOUNDARY MONUMENT 83). It is an intermediate mile marker set by Mason and Dixon in November, 1766. It is a 12-inch by 12-inch Portland Stone shaft that projects about 15 inches, and has a cut “M” on the west face and a cut “P” on the east face.

7. About 1.1 miles north of the Tangent Stone, an unmarked stone with PID = JU3849 (BOUNDARY ARC STONE 5 DE MD) set by Mason and Dixon in June, 1765.

8. About 1.4 miles north of the Tangent Stone, a stone with PID = JU3846 (MD SEL BDRY INTERSEC STONE 2). It is an 1849 USCTE stone, and is known locally as the “Prism Stone”. It is a three-sided granite shaft that projects about 24 inches. It has a cut “D” on the southeast face, a cut “M” on the west face, and a cut “P” on the north face.

9. At the Prism Stone, a roughly-dressed stone with no PID, but identified by the Delaware Geological Survey as the stone that Mason and Dixon set on this spot in June, 1765. It is an 8 x 12 x 44 dark gray gneiss stone, and is lying on its side in a wood cradle a few feet from the Prism Stone. It is of the same shape and material as Arc Stone 2.

According to the 1994 boundary agreement between Delaware and Maryland, the surviving Mason-Dixon and Graham Survey stones continue to mark this portion of the two states’ common boundary line.

References:
Mason, Charles and Jeremiah Dixon, “The Journal of Charles Mason and Jeremiah Dixon”, transcribed by A. Hughlett Mason (American Philosophical Society, 1969);

Bayliff, William H., “The Maryland-Pennsylvania and Maryland-Delaware Boundaries”, (Maryland Board of Natural Resources, Bulletin 4 Second Edition, 1959);

Cummings, Hubertis M., “The Mason and Dixon Line, Story for a Bicentenary, 1763-1963”, (Commonwealth of Pennsylvania, Department of Internal Affairs, 1962);

Danson, Edwin “Drawing the Line: How Mason and Dixon Surveyed the Most Famous Border in America” (John Wiley & Sons, 2001);

Mackenzie, John “A brief history of the Mason-Dixon survey line” (University of Delaware, 2002 (?)) at (visit link) ;

Meade, Buford K., “Report on Surveys of Delaware – Maryland Boundaries”, (U.S. Department of Commerce, National Oceanic and Atmospheric Administration, 1982);

Nathan, Roger E., “East of the Mason-Dixon Line”, (Delaware Heritage Press, 2000);

Robinson, Morgan, “Evolution of the Mason-Dixon Line” (The Journal of American History, 1909) at (visit link) ;

Schenck, William S., “Delaware’s State Boundaries” (Delaware Geological Survey, undated) at (visit link) ;

Wikipedia articles:
“Mason-Dixon line” at (visit link) ,
“The Wedge (border)” at (visit link) ,
“Transpeninsular Line” at (visit link) ,
“The Twelve Mile Circle” at (visit link) ;

Miscellaneous National Geodetic Survey datasheets and state historical signs.

Also, the “State Boundaries” section of the Delaware Geological Survey (DGS) website at (visit link) has several valuable references: Schenck, William S., “Delaware’s State Boundaries” (undated); copies of the current state boundary agreements with Maryland, Pennsylvania and New Jersey; and a database of the state’s boundary markers accessible through a “clickable” map of the state. The database comprises an inventory of all the Delaware boundary markers (modern and historic), and includes Roger Nathan’s field observations from his 1982 – 1985 inventory of the markers.
Monumentation Type: Dressed stone

Monument Category: State boundary marker

Accessible to general public: no

Explain Non-Public access:
Not accessible to the public.


Historical significance:
In 1765, Charles Mason and Jeremiah Dixon set a stone on or very near this spot to mark the intersection of the “Arc Line” and the “North Line”, two of the three segments of boundary line that ran northerly from the southwest corner of Delaware to the eastern end of the southern boundary of Pennsylvania. Since the northern boundary of Delaware was defined, in part, by a twelve-mile arc centered on the courthouse in Newcastle, the Mason-Dixon survey created a “wedge” of disputed territory. Both Pennsylvania and Delaware claimed the territory formed by the fact that the “North Line” ran due north from this point and the Newcastle Circle ran northeast. The resulting “Wedge” of territory was an inverted right triangle about 3.57 miles north-south, about 0.79 miles east-west, and comprising about 1.068 square miles. Most maps depicted this territory as belonging to Pennsylvania, but Delaware provided most legal and administrative services. In 1849, a joint boundary commission charged Lt Col Graham of the US Topographical Engineers (incorporated into the US Army Corps of Engineers in 1863) with re-surveying the “North Line” and “Arc Line”. He set the Prism Stone at the intersection of the two lines (in the same location as that marked by Mason and Dixon) and labeled the spot as being the tri-state boundary. Delaware refused to accept this outcome. In 1889, Delaware and Pennsylvania agreed that the “Wedge” should belong to Delaware. In 1892, a joint boundary commissioned engaged the US Coast and Geodetic Survey (USCGS) to re-survey the northern boundary of Delaware. The USCGS extended Mason and Dixon’s southern boundary of Pennsylvania east for about 0.79 miles until it intersected the Newcastle Circle. This eliminated the “Wedge”, and, in the 1920’s, the US Congress validated the 1892 survey. This act officially eliminated the “Wedge”, and reduced the Prism Stone from its status as a tri-state boundary point to merely marking the boundary between MD and PA. The 1994 boundary agreement between Delaware and Maryland reaffirms the stone’s status.


County: Cecil County, MD and New Castle County, DE

USGS Quad: Newark West (DE)

NGS PID: JU3846

Other Coordinates: N 39° 40.224 W 075° 47.316

Other Coordinates details:
Adjusted horizontal coordinates for PID = JU3846.


Approximate date of monument: 07/01/1849

Monumentation Type (if other): Not listed

Monument Category (if other): Not listed

Monument Website: Not listed

Visit Instructions:
1. A closeup photo of the monument is required.
______
2. A 'distant' photo including the monument in the view is highly recommended. Include the compass direction you faced when you took the picture.
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