The module begins with how the aquifer structure
was developed historically as a result of the intrusion of a finger of
the Purcell Lobe of the Cordilleran Ice Sheet during the
ice age. The effects of the Great Spokane Floods from ancient
glacial Lake Missoula are also mentioned for their role in the aquifer
formation. It discusses the formation of an unconfined aquifer
as opposed to a confined type. The origin of the water supply
(chiefly from the Clark Fork River drainage through Lake Pend
Oreille; from the Coeur d'Alene River and St. Joe River drainages
through Lake Coeur d'Alene; from various smaller local lakes: Spirit
Lake, Twin Lakes, Newman Lake, Hauser Lake, Liberty Lake, and
Hayden Lake; seepage from the Spokane
River; and, of course, local precipitation) and its
history
is covered next. The final discussion is on man's use of and effects
upon the aquifer. Idaho water use is discussed from a historical
perspective, and is compared to the changing population patterns of today
and tomorrow. Use is examined from domestic, agricultural, and commercial/industrial
viewpoints. Also examined are the levels of governmental control
over water protection.
There are text, review questions, vocabulary studies and numerous activities for each chapter. There is a second section of activities related to water and its use and conservation. These activities have been chosen for their adaptability in other curricular areas, so the student can be immersed in the topic in most of his classes simultaneously (with faculty cooperation).
A complete list of references is provided for further searches and a greater depth of knowledge. Potential users are encouraged to seek further information from the module builder!
KEY TERMS: unconfined aquifer, domestic water pollution, agricultural pollution, industrial pollution, water conservation, groundwater
Module prepared by Greg Cossette gcossett@sd273.k12.id.us or greg_id@hotmail.com