36F. Regions with shallow limestone or dolomite deposits can be particularly susceptible to groundwater contamination because water may move rapidly through dissolved caverns or sinkholes.
(Regions with shallow limestone or dolomite deposits; can be; particularly susceptible to groundwater contamination; because water may move rapidly through dissolved caverns or sinkholes) (water; may move rapidly; through dissolved caverns or sinkholes)
Regions with shallow limestone or dolomite deposits water
can be may move rapidly
particularly susceptible to groundwater contamination because water may move rapidly through dissolved caverns or sinkholes
through dissolved caverns or sinkholes