MASDIX Tangent Line Boundary Monument Mile 17, 1765, DE MD, is an 11.5-inch by 11.5-inch Portland Stone (oolitic limestone) shaft that projects 30 inches. It is located on private property, in a cultivated field along the north side of MD State Highway 318 and DE State Highway 18. It is about 7.3 miles northwest of Seaford, DE, about 6.3 miles west-southwest of Bridgeville, DE, about 3.3 miles east-northeast of Federalsburg, MD, and on the Caroline County, MD, – Sussex County, DE, boundary line. It is 17 miles north of the southwest corner of Delaware at BM 0 = MD-DE CORNER, PID = HU1800. The boundary stone is in both the National Geodetic Survey and Geocaching databases as BOUNDARY MON 14 DEL MD at PID = HU2042 (USC&GS, 1962): (
visit link) and (
visit link) .
The stone is an intermediary boundary mile marker (does not mark a mile point divisible by 5), and is in fair to good condition as compared to the other surviving Mason Dixon stones. It has an M cut into the west face and a P cut into the east face. The stone is unique in that the “P” cut into the east face appears to have been cut over an “M”. Apparently, the stone cutter inscribed “M” on both faces then, realizing his mistake, over-laid the “M” on the east face with a “P”. The top is roughly pyramidal, and has a clearly etched cross. The fluting, both vertical and horizontal, is discernable on all four sides and on the top. Though weathered, the fluting is in much better shape on the west face than on the east face. The east face and southeast corner are badly chipped, and there are minor chips on the other vertical corners. In October, 2004, the stone leaned five to seven degrees to the north, but photos taken (by “hart612”) in March, 2005, reveal that the stone stood upright at that time. The stone lies about 325 feet north of MD State Highway (DE State Highway 18), in a cultivated field that straddles the state boundary line. It may not be visible from the highway when crops are in the field. The best approach to the stone is due north along the state boundary line from the north shoulder of the highway when the field is not under active cultivation.
Mason and Dixon first surveyed this position on or about July 9, 1764, and finalized the position on or about September 29, 1764. The stone was set on or about December 21, 1765, under their direct supervision.
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, and US Highway 301 continues northeast. Follow the signs for US Highway 50 and go southeast and south on US Highway 50 for about 7.0 miles to the intersection with MD State Highway 404 leading east. Turn left and go easterly on MD State Highway for about 15.7 miles to the intersection where MD State Highway joins MD State Highway 404 from the north. Continue east and south on MD State Highway 404 & 313 around the east side of Denton, MD, for about 6.1 miles to the intersection where MD State Highway 313 leads south and MD State Highway 404 leads southeast. Turn right and go south on MD State Highway 313 for about 10.0 miles to the intersection where MD State Highway 318 joins from the west, on the northwest edge of Federalsburg, MD. Follow MD State Highway 318 south and east around Federalsburg and towards Bridgeville, DE, for about 5.3 miles to the state line, and the field and 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)
Schenck, 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: 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.