Answer :
Let's fill in the temperature values for the given depths in the table.
1. Crust: At a depth of 1 kilometer, the temperature is [tex]\( 25^{\circ} C \)[/tex]. This value is already provided as an example in the table.
2. Mantle: At a depth of 1,000 kilometers, the temperature is approximately [tex]\( 1500^{\circ} C \)[/tex].
3. Outer Core: At a depth of 4,000 kilometers, the temperature is approximately [tex]\( 4000^{\circ} C \)[/tex].
4. Inner Core: At a depth of 6,000 kilometers, the temperature is approximately [tex]\( 5300^{\circ} C \)[/tex].
Now, let's complete the table with these temperatures:
[tex]\[ \begin{tabular}{|c|c|c|} \hline \text{Zone} & \text{Depth (Kilometers)} & \text{Temperature } ( ^{\circ} \text{C}) \\ \hline \text{Crust} & 1 \text{ km} & 25 ^{\circ} \text{C} \\ \hline \text{Mantle} & 1,000 \text{ km} & 1500 ^{\circ} \text{C} \\ \hline \text{Outer Core} & 4,000 \text{ km} & 4000 ^{\circ} \text{C} \\ \hline \text{Inner Core} & 6,000 \text{ km} & 5300 ^{\circ} \text{C} \\ \hline \end{tabular} \][/tex]
Thus, the specified temperatures for each depth in the different compositional zones of Earth's interior are filled in the table accordingly.
1. Crust: At a depth of 1 kilometer, the temperature is [tex]\( 25^{\circ} C \)[/tex]. This value is already provided as an example in the table.
2. Mantle: At a depth of 1,000 kilometers, the temperature is approximately [tex]\( 1500^{\circ} C \)[/tex].
3. Outer Core: At a depth of 4,000 kilometers, the temperature is approximately [tex]\( 4000^{\circ} C \)[/tex].
4. Inner Core: At a depth of 6,000 kilometers, the temperature is approximately [tex]\( 5300^{\circ} C \)[/tex].
Now, let's complete the table with these temperatures:
[tex]\[ \begin{tabular}{|c|c|c|} \hline \text{Zone} & \text{Depth (Kilometers)} & \text{Temperature } ( ^{\circ} \text{C}) \\ \hline \text{Crust} & 1 \text{ km} & 25 ^{\circ} \text{C} \\ \hline \text{Mantle} & 1,000 \text{ km} & 1500 ^{\circ} \text{C} \\ \hline \text{Outer Core} & 4,000 \text{ km} & 4000 ^{\circ} \text{C} \\ \hline \text{Inner Core} & 6,000 \text{ km} & 5300 ^{\circ} \text{C} \\ \hline \end{tabular} \][/tex]
Thus, the specified temperatures for each depth in the different compositional zones of Earth's interior are filled in the table accordingly.