The lithostatic pressure (P) can be calculated using the formula:
\[ P = \rho \cdot g \cdot h \]
Where:
Substituting the given values into the formula:
\[ P = 2800 \, \text{kg/m}^3 \times 9.8 \, \text{m/s}^2 \times 36,500 \, \text{m} = 1.0 \times 10^9 \, \text{Pa} \]
To convert from Pascals to Gigapascals (GPa), divide by \( 10^9 \):
\[ P = 1.0 \, \text{GPa} \]
The lithostatic pressure is: 1 GPa.
In the isochemical phase diagram shown below, the curved arrow represents the P-T path. The variance at peak metamorphism is _.
The units A to H marked on the figure represent different rock formations. Select the option that describes the chronological sequence from old to young.
Consider two intersecting, north-easterly striking and south-easterly dipping dikes Y1 and Y2, which are exposed on an east-west trending vertical wall of a granite (X) quarry as shown below.
The angle that the dikes make with the horizontal on the quarry wall is