Step 1: Concept of Pratt's Model.
According to Pratt's hypothesis of isostasy, all crustal columns have the same thickness, but different densities to achieve balance at the compensation depth.
\[
\text{Condition: } \rho \cdot t = \text{constant for equilibrium.}
\]
Here,
\[
t = 30 \, \text{km (crustal thickness)}
\]
\[
\rho_c = 2700 \, \text{kg/m}^3 \quad \text{(continental crust density)}
\]
\[
h = 1.5 \, \text{km (lake depth)}
\]
\[
\rho_w = 1000 \, \text{kg/m}^3
\]
Step 2: Mass column for reference crust (without lake).
For the normal continental crust of thickness $t$,
\[
M_c = \rho_c \cdot t = 2700 \times 30 = 81000 \, \text{kg/m}^2
\]
(This is the reference column mass per unit area.)
Step 3: Mass column for lake region (with reduced density $\rho_1$).
In the lake region, total column mass =
\[
M_l = \rho_1 \cdot (t - h) + \rho_w \cdot h
\]
Here,
\[
t - h = 30 - 1.5 = 28.5 \, \text{km}
\]
So,
\[
M_l = \rho_1 \cdot 28.5 + 1000 \cdot 1.5
\]
Step 4: Apply isostatic balance condition.
For equilibrium at compensation depth:
\[
M_l = M_c
\]
\[
\rho_1 \cdot 28.5 + 1500 = 81000
\]
\[
\rho_1 \cdot 28.5 = 79500
\]
\[
\rho_1 = \frac{79500}{28.5}
\]
Step 5: Final computation.
\[
\rho_1 = 2789.47 \, \text{kg/m}^3
\]
Wait—check again. The lake replaces crustal material, so correction is needed. The effective condition should be:
\[
\rho_c \cdot t = \rho_1 \cdot t - (\rho_1 - \rho_w)h
\]
\[
81000 = \rho_1 \cdot 30 - (\rho_1 - 1000)(1.5)
\]
\[
81000 = 30\rho_1 - 1.5\rho_1 + 1500
\]
\[
81000 - 1500 = 28.5 \rho_1
\]
\[
79500 = 28.5 \rho_1
\]
\[
\rho_1 = \frac{79500}{28.5} = 2789.47 \, \text{kg/m}^3
\]
Final Answer:
\[
\boxed{2789.47 \, \text{kg/m}^3}
\]
A color model is shown in the figure with color codes: Yellow (Y), Magenta (M), Cyan (Cy), Red (R), Blue (Bl), Green (G), and Black (K). Which one of the following options displays the color codes that are consistent with the color model?