Step 1: Approach Statement (I) by asking whether any natural aquifer material is ever perfectly uniform in every direction. Sand, gravel, clay layers, and fractured rock all form through processes like sedimentation and weathering that naturally produce layering and directional differences in how easily water moves through them. A truly isotropic and homogeneous aquifer would need the material to be identical everywhere and in every direction, which almost never happens in nature, so calling such aquifers rare is a fair and standard observation.
Step 2: Approach Statement (II) by picturing an actual pumping test in the field. Engineers cannot read the aquifer properties directly, so they pump one well steadily and watch how the water table drops in nearby wells set up beforehand at different distances, some very close and some further out, over the course of the test. That is precisely the setup Statement (II) is describing, so it lines up with real field procedure.
Step 3: Neither statement runs into a contradiction with standard groundwater theory or practice, so both stand as valid together.\[\boxed{\text{Both Statement (I) and Statement (II) are correct}}\]