In karst terrain and limestone caverns, open lava tubes, or large rock fractures, the rate of groundwater movement resembles that of streams and rivers on the surface.
(the rate of groundwater movement; resembles; that of streams and rivers on the surface; L:In karst terrain and limestone caverns, open lava tubes, or large rock fractures)
the rate of groundwater movement
resembles
that of streams and rivers on the surface L:In karst terrain and limestone caverns, open lava tubes, or large rock fractures