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Details for Benchmark: AA6882

N 41° 08.515 W 081° 20.260 (NAD 83)

Altitude: 1119

Coordinates may not be exact. Altitude is GPS OBS and location is ADJUSTED. (more info)

Location:
In PORTAGE county, OH View Original Datasheet
Designation:
FR-04-01
Marker Type:
survey disk
Setting:
set into the top of a round concrete monument
Stability:
May hold, but of type commonly subject to surface motion.

Reference Points

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A new road, East Campus Drive, has been built here. Measurements fell under the pavement.

Documented History (by the NGS)

01/01/1993 by OH3880 (MONUMENTED)
DESCRIBED BY CITY OF KENT OHIO 1993 (DT) THE STATION MARK IS ON THE SOUTH SIDE OF SUMMIT STREET ABOUT 0.1 MI WEST OF THE INTERSECTION OF LOOP ROAD IN THE SOUTHEAST PART OF THE CITY OF KENT, OHIO. TO REACH THE STATION FROM THE JUNCTION OF SOUTH WATER STREET (STATE ROUTE 43) AND HAYMAKER PARKWAY (STATE ROUTE 59) NEAR KENT CITY HALL, TRAVEL SOUTH ALONG SOUTH WATER STREET ABOUT 0.1 MI TO THE INTERSECTION OF SUMMIT STREET. TURN LEFT ON TO SUMMIT AND TRAVEL EAST ABOUT 0.3 MI TO THE INTERSECTION OF LINCOLN STREET. BEAR RIGHT AND CONTINUE SOUTHEAST ALONG SUMMIT ABOUT 0.9 MI AND THE STATION ON THE RIGHT. THE STATION MARK IS A STANDARD CITY OF KENT BRONZE DISK STAMPED FR-04-01 SET IN A CONCRETE MASS ABOUT 2 INCHES BELOW THE SURFACE WITH RE-BAR FOR MAGNETIC DETECTION. THE STATION IS OPPOSITE MUSSLEMAN HALL ACROSS THE STREET ON THE CAMPUS OF KENT STATE UNIVERSITY. A MONUMENT BOX ASSEMBLY IN THE CENTERLINE OF SUMMIT STREET IS ABOUT 51.0 FT NORTHEAST OF THE STATION MARK. A FIRE HYDRANT LOCATED ON THE SOUTH SIDE OF THE STREET IS ABOUT 63.3 FT WEST OF THE STATION. THE STATION MARK IS ABOUT 21.9 FT SOUTH OF THE PAVEMENT CENTERLINE OF SUMMIT STREET. STATION MARK FR-14-01 ABOUT 0.3 MI TO THE NORTHWEST ON THE SOUTH SIDE OF SUMMIT STREET MAY BE USED FOR AN AZIMUTH MARK.

Control Text

  • The horizontal coordinates were established by GPS observations and adjusted by the National Geodetic Survey in April 1998.
  • The orthometric height was determined by GPS observations and a high-resolution geoid model.
  • The Laplace correction was computed from DEFLEC99 derived deflections.
  • The geoid height was determined by GEOID99.

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