...line, with few interruptions, bounding long parallel ridges of nearly Khe same height, declining eently towards the side where the stratification dips from the horizon, and more precipitous on the ojiposite .side where the «dge of the stratum breaks out to the day. Of the primitive rocks Granite...

...on the north west side, sloping gradually towards the primitive, which ranges along its south east boundary. The outline of the mountains of this formation,...precipitous on the opposite side, where the edge of the strata comes to the surface. This formation is composed of a small-grained transition limestone, of...

...deviation in some places from this general rule ; the dip being, for a short distance, to the south-east. The outline of the mountains of this formation is almost a straight line, with few interruptions, bound, ing long parallel ridges of nearly the same height, declining gently towards the side where...

...dipping generally to the north-west, at an angle in most places under 45° from the horizon." — " The outline of the mountains of this formation, is...grained transition limestone of all the shades of color from a white to a dark blue, and in some places intimately mixed with a stratum of grey wacke...

...direction, dipping generally to the northwest, at an angle in most places under 45" from the horizon.""" The outline of the mountains of this formation, is...dips from the horizon, and more precipitous on the oposite side, where the edge of the stratum breaks out to the day." " This formation is composed of...

...on the north west side, sloping gradually towards the primitive, which ranges along its south east boundary. The outline of the mountains of this formation,...precipitous on the opposite side, where the edge of the strata comes to the surface. This formation is composed of a small-grained transition limestone, of...