MASDIX Tangent Line Mile 3, 1765, Delaware - Maryland
Posted by: Groundspeak Regular Member seventhings
N 38° 30.215 W 075° 41.824
18S E 439219 N 4261921
MASDIX Tangent Line Mile 3, 1765, DE-MD, is a dressed Portland Stone shaft set by Mason and Dixon in 1765 to demarcate the boundary between DE and MD.
Waymark Code: WM3VBR
Location: Delaware, United States
Date Posted: 05/20/2008
Published By:Groundspeak Regular Member GEO*Trailblazer 1
Views: 37

MASDIX Tangent Line Boundary Monument Mile 3, 1765, DE MD, is a 12-inch by 12-inch dressed Portland Stone (oolitic limestone) shaft that projects about 25 inches. It is located along the west side of a dim track road on undeveloped private property about three miles north of the BOUNDARY MON 0 = MD DEL CORNER, PID = HU1800 (marking the southwest corner of Delaware), about 0.5 miles north of Cross Road (Road 507 in DE) and about 0.5 miles east of Norris Twilley Road. The stone is located about 5.9 miles north of Hebron, MD, 4.5 miles northeast of Mardela Springs, MD, about 2.5 miles southeast of Sharptown, MD, and on the Wicomico County, MD – Sussex County, DE boundary line. It is in both the National Geodetic Survey and Geocaching databases as BOUNDARY MONUMENT 3 DE MD, at PID = HU2016: (visit link) and (visit link) .

The stone is an intermediate mile marker (marks a mile point NOT evenly divisible by “5”) with a cut “P” on the east face and a cut “M” on the west face. The stone is in very good condition. The cut letters are intact and sharply-incised, the top is roughly pyramidal, and both the horizontal and vertical fluting are visible on all four sides and the top. The stone is erect and stable. There is a large chip along the south edge of the top, and smaller chips at the southeast and southwest corners of the top. There are four to five two-inch horizontal scratches on each side of the stone.

Mason and Dixon first surveyed this position on or about June 26, 1764, and finalized the position on or about September 27, 1764. The stone was set on or about December 18, 1765, under their direct supervision. The US Coast and Geodetic Survey (USC&GS) monumented the stone in 1962 as BOUNDARY MONUMENT 3 DE MD, PID = HU2016.

To reach from the (US Highway 301 and US Highway 50) bridge over the Chesapeake Bay just east of Annapolis, MD, go easterly on US Highway 301&50 for about 11 miles to where US Highway 50 splits off and heads south. Go south on US Highway 50 for about 54 miles to the intersection with State Highway 54 near Mardela Springs. Turn left and go east on State Highway 54 for about 2.4 miles to the intersection with Norris Twilley Road. Turn left and go northerly on Norris Twilley Road for about 2.3 miles to the intersection with Cross Road. Turn right and go east on Cross Road for about 0.5 miles to the state boundary line. Continue east, now on Road 507, for about 0.10 miles to a gravel drive leading north to an equipment shed. Obtain permission to proceed from the owner at the shed. From the shed, pack north across a corn field for about 625 feet to an east-west drainage ditch. Pack west along the ditch to a board bridge. Cross the bridge and pack north for about 450 feet to the northwest corner of the field. Continue north, now on a dim track road, through the timber for about 450 feet to the stone on the left.

HISTORY OF THE TANGENT LINE
The Tangent Line forms a portion of the boundary line between Delaware and Maryland. It runs from northward for 82 miles from the southwest corner of Delaware to a point of tangency with the Twelve-Mile Circle boundary line centered on the courthouse at New Castle, DE. During the period 1765 – 1768, the Tangent Line was marked with 83 stones. All but nine of the stones survive at or near their original surveyed positions.

In 1750, after 70 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 appointed four commissioners to run the Transpeninsular Line (east-west southern boundary of Delaware) and to determine southwest corner of Delaware at the Middle Point of that line (halfway between the Atlantic Ocean and the Chesapeake Bay). In 1750-1751, the commissioners and surveyors ran and marked the Transpeninsular Line.

In 1760, the Court ratified the Transpeninsular survey and ratified a Final Agreement between the Penns and Calverts. That agreement specified, in part, that 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 boundary line centered on the cupola of the courthouse at New Castle. Colonial surveyors determined the Tangent Point and attempted, unsuccessfully, to run the Tangent Line. In August, 1763, the proprietors of the two colonies engaged Charles Mason and Jeremiah Dixon to complete this line, and to survey all the boundary lines between Maryland and its neighbors to the north and east.

Mason and Dixon arrived in America in November of 1763. They started work on the Tangent Line in June, 1764, and, after running the line north and south a total of three times, completed the survey and temporary marking in November, 1764. In June, 1765, they marked the Tangent Point (the intersection of the Tangent Line and the Arc Line boundary segment) with a dark gray, gneiss stone that bore the abbreviated armorial crests of the Penns and Calverts. In December, 1765, Mason and Dixon placed the first 50 of 83 Portland Stone markers along the Tangent Line at one-mile intervals from Mile 1 through Mile 50, working from south to north. They placed 32 more stones in October – November, 1766, marking Mile 51 through 82. The stone at Mile 82 was a crown stone and it was placed a few yards south of the 1765 stone that marked the Tangent Point. In November, 1768, (about two months after Mason and Dixon departed America), the joint boundary commission set a stone at the Middle Point, the south end of the Tangent Line and the intersection with the Transpeninsular Line. The stone is a 14-inch by 14-inch Portland Stone shaft that projects about 36 inches, and is a “double crown stone” - the armorial crest of the Penn Family is cut into the north and east faces of the stone, and the crest of the Calvert Family is cut into the south and west faces. Though not set by Mason and Dixon, the Middle Point stone is generally described as a “Mason-Dixon stone”.

Mason and Dixon were assisted by three colonial surveyors: Joel Bailey, Jonathan Cope and William Darby. They also engaged the services of a small army of axmen, teamsters and other laborers.

The Tangent Line runs from the double crown stone at the Middle Point (see PID = HU1800) northward (3 degrees 36” 6’ west of north) about 82 miles to the Tangent Point. As determined by Mason and Dixon, the Tangent Point was a few yards north of Mile 82. In 1849, a survey (the “Graham Survey”) by the US Corps of Topographical Engineers (USCTE) adjusted the Tangent Point and marked it with a granite stone at PID = JU3840. Today, the original 1765 Mason-Dixon stone abuts the 1849 granite marker; the 1766 Mile 82 marker that originally stood a few yards to the south has been lost.

Along the line, the five-mile intervals are marked with stones that have the Penn and Calvert armorial crests carved on their east and west faces, respectively. The intermediate mile markers have a cut “M” on the west face and a cut “P” on the east. The stones are high-grade oolitic limestone – greater than 95 percent calcium carbonate – and were quarried near the Isle of Portland (a peninsula) on the south coast of England. The dense limestone is generically known as “Portland Stone”. The intermediate mileposts are generally 12-inches by 12-inches and about 40 inches in length, and few stones project more than 24 inches. The crown stones are about a foot longer. The vertical faces of the stones are fluted (with very shallow flutes of about 0.5 inches), with a two-inch band of horizontal fluting at the corners (with shallow flutes of about 0.4 inches). The tops originally were pyramidal and fluted. Due to weathering and damage, the tops of most stones are flat or slightly rounded. The cut letters are about five inches in height and are surrounded by an eight-inch flattened oval. Many of the stones have chiseled X’s in their tops. Most of the stones have PIDs, and about one dozen are accessible to the public. According to the Delaware Geological Survey, 76 of the original 82 (apparently not counting the Mile 82 marker near the Tangent Point) Mason-Dixon stones survive. By my count 74 of the 83 stones survive (counting the Mile 82 marker) at or near their original surveyed positions. The nine non-surviving or relocated stones are:

1. Mile 5 – missing
2. Mile 7 – missing (may be in the Naticoke River)
3. Mile 10 – moved to the Mile 79 position in 1976, moved to the Delaware Geological Survey building in 1991
4. Mile 11 – moved to a point near the Mile 42 position in 1976
5. Mile 30 – missing
6. Mile 42 – missing (may be in Mudd Mill Pond), replaced with Mile 11 stone in 1976.
7. Mile 61 – missing
8. Mile 64 – missing
9. Mile 82 – missing

I strongly suspect that the Mile 82 marker, a crown stone, now resides in the Historical Society of Delaware in Wilmington. Mason and Dixon probably placed a crown stone at this location (not a mile point divisible by 5) because it represented the north end of the Tangent Line and south end of the Arc Line.

During boundary re-surveys in 1961-62 by the US Coast & Geodetic Survey (USC&GS) and in 1975-1977 by its successor, the National Geodetic Survey (NGS), five Mason-Dixon stones were repositioned to the original (but re-calculated) boundary line. The five were the markers at Miles 34, 45, 63, 73 and 75. Also, fifteen stones were found to be “missing”; of these, eleven were restored. A few of the surviving markers (two or three) have been moved short distances along the line to distance them from roads, plowing operations and other hazards.

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)

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

Wikipedia article: “Mason-Dixon line” 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: Shenck, 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: Mason-Dixon Stone

Explain Non-Public access:
The stone is located on undeveloped private property.


Historical significance:
See above


County: Wicomico County, MD, and Sussex County, DE

USGS Quad: Sharptown (MD - DE)

NGS PID: HU2016

Other Coordinates: N 38° 30.215 W 075° 41.824

Other Coordinates details:
Adjusted horizontal coordinates for PID = HU2016.


Approximate date of monument: 12/18/1765

Monumentation Type (if other): Not listed

Monument Category (if other): Not listed

Accessible to general public: 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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