Where Are Vernal Pools
Found?
California's vernal pools occur on
a variety of landscape formations, most often on alluvial formations
deposited by ancient waterways and seas. The greatest extent of
this type of landscape formation is in our Central Valley, in
areas where alluvial surfaces were exposed after the retreat of
the inland sea during the Pleistocene era. Similar alluvial landscape
formations occur in inland valleys of the inner Coast Ranges,
and along coastal terraces of Southern California, where geologic
forces have lifted the original alluvial landscape surfaces above
sea level.
A second type of landscape formation
with vernal pools are ancient volcanic mudflows, where rapid weathering
of volcanic materials have formed dense clay soils and bedrock
restricting layers near the soil surface. Volcanic landscape formations
are found in northeast California and in the northern end of the
Sacramento Valley.
Why Are Vernal Pools Regulated
and Who Regulates Them?
Federal, state, and local laws and
policies regulate certain activities in wetlands, including vernal
pools, and may prohibit activities that could harm or harass threatened
or endangered wildlife species or migratory waterfowl. In addition,
the California Environmental Quality Act, a state law, requires
public agencies to consider the effects of proposed actions on
biological resources. Environmental laws and policies that pertain
to vernal pools in California include:
These environmental laws and policies require agencies
and landowners to consider the effects of a proposed action on
the environment; determine if a less damaging alternative is available;
obtain and comply with necessary wetland permits; and comply with
endangered species laws (for vernal pools that support endangered
species). Compensatory mitigation may be required by local Planning
Departments or regulatory permitting agencies to help ensure that
the project does not result in a loss of wetland functions.






