Details for Benchmark: HU0270
N 38° 20.033 W 075° 05.800 (NAD 83)
Altitude: 13.86
Coordinates may not be exact. Altitude is ADJUSTED and location is SCALED. (more info)
- Location:
- In WORCESTER county, MD View Original Datasheet
- Designation:
- G 104
- Marker Type:
- bench mark disk
- Setting:
- abutments and piers of large bridges
- Stability:
- Probably hold position/elevation well.
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Documented History (by the NGS)
01/01/1962 by CGS (MONUMENTED) |
DESCRIBED BY COAST AND GEODETIC SURVEY 1962
AT OCEAN CITY. SET IN A DRILL HOLE IN THE NORTHEAST CONCRETE ABUTMENT AT THE NORTHWEST END OF U.S. HIGHWAY 50 BRIDGE OVER SINEPUXENT BAY. 9 FEET NORTHEAST OF THE NORTHEAST CURB OF HIGHWAY 50 AND 1 FOOT ABOVE THE LEVEL OF THE HIGHWAY. |
01/01/1984 by NGS (GOOD) |
RECOVERY NOTE BY NATIONAL GEODETIC SURVEY 1984
RECOVERED IN GOOD CONDITION. |
01/01/1988 by USPSQD (GOOD) |
RECOVERY NOTE BY US POWER SQUADRON 1988 (RBD)
RECOVERED IN GOOD CONDITION. |
05/14/1991 by MDSHA (GOOD) |
RECOVERY NOTE BY MARYLAND DOT HIGHWAY ADMINISTRATION 1991
THE MARK IS LOCATED ABOUT 6.65 MI (10.70 KM) EAST OF BERLIN, 0.53 MI (0.85 KM) WEST OF OCEAN CITY AND ON ROAD RIGHT-OF-WAY. TO REACH FROM THE INTERSECTION OF U.S. 50 AND 113, GO EAST ON U.S. HIGHWAY 50 FOR 6.6 MI (10.6 KM) TO THE ASSAWOMAN BAY BRIDGE AND THE MARK ON THE LEFT. IT IS 32.0 FT (9.8 M) NORTH OF THE CENTER LINE OF U.S. HIGHWAY 50, 9.8 FT (3.0 M) NORTHWEST OF THE WEST END OF A CHAIN LINK FENCE, 2.7 FT (0.8 M) NORTHEAST OF A LIGHT POLE, AND SET IN A DRILL HOLE IN THE WEST ABUTMENT OF THE BRIDGE. |
Control Text
- The horizontal coordinates were scaled from a topographic map and have an estimated accuracy of +/- 6 seconds.
- The orthometric height was determined by differential leveling and adjusted by the National Geodetic Survey in June 1991.
- The geoid height was determined by GEOID99.
- The dynamic height is computed by dividing the NAVD 88 geopotential number by the normal gravity value computed on the Geodetic Reference System of 1980 (GRS 80) ellipsoid at 45 degrees latitude (g = 980.6199 gals.).
- The modeled gravity was interpolated from observed gravity values.