A |
Largely bedrock outcrops with lowlands near Bakersfield stadium (1&2). Minimal hazards loss. |
B |
Inwood lowlands. 20-60 ft bedrock depth (3), which according to (5) could be either C or D class soils. This area has considerable amounts of fill and sediment, so it was designated as a softer class D type. (1). This area contains bedrock of South East sloping gradient, so it could have been considered as a transition C-soil. With a higher resolution depth to bedrock map overlayed on the census tract, instead of just bedrock contour data a different judgement could have been applied [1,2,3]. |
C |
Major outcrops in this area. All pertinent
facilities and population located predominately on bedrock. [1,2]. |
D |
Located between 155 to 158 st, there is an indentation in the bedrock sloping towards the Hudson River [1,2,3]. There are B soil areas down to 145 st. - 148 st. Area is almost entirely made up of Manhattan Schist. Substantial bedrock info combined with MTA Boreholes and generalized by sources [1,2,3]. |
E |
City College highlands.
Predominately rocky soils with outcroppings [1,2] |
F |
Bronx
portion of Manhattan. High lying hills with most facilities located in
low lying areas. Previously East River channel, so mostly built on fill.
This justifies a D class soil definition. [1&2]. |
G |
Inwood
lowlands. 20-60 ft bedrock depth [3], which according to [5] could be
either C or D class soils. This area has considerable amounts of fill
and sediment, so it was designated as a softer class D type. [11 |
H |
Inwood
lowlands. 20-60 ft bedrock depth [3], which according to [5] could be
either C or D class soils. This area has considerable amounts of fill
and sediment, so it was designated as a softer class D type [1]. This
tract also contains a considerable amount of filled swamp land [2]. |
I |
Inwood
Marble and Elevating Manhattan Schist with flat lying bedrock plateau,
140-200 ft. [1,2]. |
J |
Harlem
Lowlands. Deep silty soils [1 2]. |
Figure 3a: Site classes for Manhattan by census tracts
|