dabton.] NEW JERSEY. 103 
The following wells have reached the horizon at the depths indicated: 
Locality. 
Asbury Park 
Ocean Grove 
Atlantic Highlands 
Fellowship 
Freehold 
Freehold, 1| miles north 
Glassboro 
Hartford 
Matawan 
Port Monmouth ( ?) 
Red Bank 
Kumsou Neck 
Maple Shade 
Seabright, 3 wells 
Seabright, Hotel Normandy . 
Monmouth Beach 
SeaGirt 
Point Pleasant 
Mantoloking 
Woodbury 
Woodbury, 2 miles south 
3 miles southwest of Marlton 
Marlton 
Sewell 
Wenonah waterworks 
Depth. 
Feet. 
448-1, 083 
1,134 
108-112 
131 
322 
210 
511 
161-167 
100 
100 
230 
210 
64-97 
258 
190 ? 
380 
694 
800 
922 
80 
120 
316? 
200 
342-351 
196 
Remarks. 
500 gallons per minute. 
Fair supply. 
Not very satisfactory 
Do. 
Do. 
Too much fine sand. 
Do. 
Hows. 
Large. 
60 gallons per minute. 
Considerable. 
120 gallons per minute. 
Flows. 
Satisfactory supply. 
Not utilized? 
Satisfactory supply. 
Fair supply. 
Satisfactory. 
Do. 
Water to —28 feet. 
Small amount. 
Satisfactory. 
No water at these horizons was reported in wells at WoodstowD, 
Marlton, Mount Holly, Columbus, and Holmdel. 
The region from Matawan to Asbury Park, and probably to Mount 
Pleasant, appears to be underlain by a continuous stratum of the 
upper water-bearing horizon containing a good supply of water, with 
the possible exception of the Holmdel area. In the Asbury Park 
region and southward there are also several lower horizons. 
In the region east and southeast of Camden the upper horizon was 
found to yield some water, notably at Woodbury, and possibly in the 
well 3 miles southwest of Marlton; but basal Matawan and deeper 
beds furnish a more satisfactory supply. In the Hartford well there 
was plenty of water at this horizon, but it was mixed with much fine 
sand. The Kedbank and Seabright wells are the greatest producers 
from the upper horizon, and the Asbury Park and Ocean Grove wells 
obtain large supplies from lower horizons. The areas known to be 
underlain by these waters and that of the basal Matawan horizon are 
represented by one pattern on the map, PI. II, and some of the rela- 
tions are shown in the cross sections in PI. III. 
UPPER CRETACEOUS HORIZONS. 
These are mainly in the Lower Marl and Kedbank formations. A 
well at Harrisonville and another at Gibbsboro draws from a bed of 
sand in the Rancocas formation. 
