TP Line Mile 5, 1751, DE-MD, is a 12-inch by six-inch dressed dark gray gneiss stone that projects 29 inches and marks the five mile point along the Transpeninsular Line, the east-west line that forms Delaware’s southern boundary with Maryland. It is located about ten feet south of the southwest corner of an old, wire fence that encloses an overgrown pasture. The stone is located about 8.5 miles northwest of Ocean City, MD, about 5.1 miles east of Selbyville, DE, about 4.9 miles west of the Atlantic Ocean shoreline at the town of Fenwick Island, DE, and on the Wicomico County, MD, - Sussex County, DE, boundary line. The stone is in both the Geocaching and National Geodetic Survey databases at PID = HU1546, BOUNDARY MON EW 5 DE MD: (
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According to the Delaware Geological Survey (
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The stone is located on private undeveloped land (formerly a pasture for goats), about 300 feet southwest of the centerline of Muskrattown Road, and about 250 feet southwest of the residence located in the southern angle of the intersection of Muskrattown Road and West Line Road, and about ten feet south of the southwest corner of the old pasture.
To reach from the intersection of the Ocean City Expressway (State Highway 90) and the Coastal Highway (State Highway 528) in Ocean City, MD, go north on the Coastal Highway for about 4.7 miles to the MD-DE boundary line. Continue north for about 0.07 miles to the village of Williamsville and the intersction with West Line Road. Turn left and go southwest on West Line Road for about 0.6 miles to the intersection with Muskrattown Road. Turn left and go southeast on Muskrattown Road for about 50 yards to the gravel driveway on the right, just southeast of the first residence on the southwest side of the road. After obtaining permission to continue (either at the residence or at the mobile home directly across the street), pack southwest from the gravel driveway for about 250 feet to the southwest corner of the old pasture and the stone.
HISTORY OF THE TRANSPENINSULAR LINE
The Transpeninsular Line (TP Line) constitutes a portion of the boundary line between Delaware and Maryland. It runs almost due west from the Atlantic Ocean at Fenwick Island across the Delmarva Peninsula. It ends at the mid-point of the peninsula, about 35 miles west of its origin. The line was marked with seven historical stones. Six of the seven survive.
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 ruled that the southwest corner of Delaware was to be the “Middle Point” of a line running due west from Cape Henlopen on the Atlantic coast across the Delmarva Peninsula. The “Cape Henlopen” actually identified on the charts used by the Court was located at Fenwick Island, about 24 miles south of the modern Cape Henlopen.
The Court appointed four commissioners, John Watson and William Parsons of Pennsylvania and John Emory and Thomas Jones of Maryland, to run the TP Line. Most of the actual surveying work was done by Nicholas Sculls of Pennsylvania. In 1750-1751, the commissioners ran the TP Line and marked it with five gray gneiss stones – one near the initial point and one every five miles (except for the Mile 15 point) to the 25-mile point. The surveyors did not set a stone at the Mile 15 point because the point was located in the Pocomoke River. Also, they did not fix the middle point of the line because the contending parties could not agree on whether the width of the peninsula should be measured all the way to the eastern shore of the Chesapeake Bay or only to the eastern reach of the Bay’s tidal waters, about four miles east of the shoreline.
In 1760, the Court ratified a “Final Agreement” between the contending parties. That agreement specified, in part, that the Middle Point would be determined with respect to the width of the peninsula measured all the way to the eastern shore of the Chesapeake Bay. The Court also accepted the survey as run in 1750 – 1751. Upon this acceptance,
the commissioners set stones at Miles 30 and 35 (Middle Point).
With the Court of Chancery’s ratification of the TP Line in 1760, colonial surveyors John Riggs, Thomas Garrett, John Lukens and Archibald McClean ran a twelve-mile radius from the New Castle courthouse and established the “Tangent Point”, where a line run a few degrees west of north from the Middle Point would intersect the Twelve-Mile Circle boundary line. In 1761, the surveyors began to run the Tangent Line (western boundary of Delaware) 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 survey and mark all the boundary lines between Pennsylvania and Maryland.
In November, 1763, Mason and Dixon arrived in Philadelphia. Mason and Dixon accepted without change the determination of the Middle Point as established in 1751 and ratified in 1760. In June, 1764, Mason and Dixon started their survey of the Tangent Line northward from the Middle Point.
The stones marking Miles 0, 5, 10, 20 and 35 miles survive at or near their original locations. The stone at Mile 25 was moved to avoid road construction and now is co-located with the Mile 35 stone near the Middle Point. The Mile 30 stone disappeared in the 1970’s. Both the Mile 25 and Mile 35 stones are situated in a wrought-iron enclosure along with a double crown stone set in November, 1768. The double crown stone was set by the commissioners who oversaw Mason and Dixon’s 1763 – 1767 surveys of the remaining boundary lines between Maryland and the Penn Family’s two colonies.
The TP Line stones are dark gray gneiss (specifically, perhaps, a type known as “amphibolite gneiss”). They are about 12 inches across at the bottom, about six inches thick, and the tops are rounded. The stones originally bore the armorial crests of the Penn and Calvert families on their north and south faces, respectively. The crests on the stone at Miles 0 and 5 are still readily discernable, but all the remaining stones have weathered to the point that the crests are not recognizable.
The stone at Mile 0 was originally set 2,224 feet (139 perches) west of the shoreline at the Atlantic Ocean. The nominal distances for the stones at Miles 5 through 35 originate at the shoreline (and not the initial stone). The stone at Mile 35 (as originally measured) was a few hundred feet less than 35 miles from the shoreline (because the peninsula was originally measured as 69.93 miles wide). Using the National Geodetic Survey’s INVERSE calculator, the distance between the stone at Mile 0 and the stone at Mile 35 is 34.6474 miles. Adding 2,224 feet to that measure places the Middle Point 35.0686 miles from the Atlantic shoreline today. Measured from point to point along the line (because it curves north of the parallel), the line is 35.088 miles long.
The agreements between the Penn and Calvert families, as well as the Court of Chancery’s rulings, specified that the TP Line was to run due west. However, the line bends a bit to the north, and the Middle Point is about 3,215 feet (0.609 miles) north of a parallel of latitude originating at Mile 0.
According to the 1994 boundary agreement between Delaware and Maryland, the surviving 1751 stones that have not been moved from their original positions 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)
Bedini, Silvio A., “The Scull Dynasty of Pennsylvania Surveyors”, Professional Surveyor Magazine, May, 2001, Volume 21 Number 5.
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 (
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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 (
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Shenck, William S., “Delaware’s State Boundaries” (Delaware Geological Survey, undated) at (
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Wikipedia article: “Transpeninsular Line” at (
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Miscellaneous National Geodetic Survey datasheets and state historical signs
Also, the “State Boundaries” section of the Delaware Geological Survey (DGS) website at (
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