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:
\[
\boxed{2789.47 \, \text{kg/m}^3}
\]