The correct answer for this question is option 1: Batholiths.

Batholiths are large bodies of magmatic material that cool and solidify in the deeper depths of the Earth`s crust. They are typically formed through the consolidation of multiple smaller intrusions and can span over hundreds to thousands of square kilometers in area.

Now, let`s take a look at the other options:

Option 2: Lacoliths. Lacoliths are similar to batholiths in that they are also formed from magmatic material. However, lacoliths are smaller in size and are characterized by their mushroom-like shape, with a domed upper surface and a flat lower surface.

Option 3: Lopoliths. Lopoliths are concave-shaped intrusions that are formed when magma accumulates and spreads out horizontally in the Earth`s crust. Unlike batholiths, lopoliths have a bowl-like or saucer-like shape.

Option 4: Phacoliths. Phacoliths are convex-shaped intrusions that bend the surrounding rock layers. They are formed when magma pushes upwards and causes the overlying rocks to fold and warp.

In summary, while options 2, 3, and 4 refer to specific types of magmatic