geology and geomorphology of the prairies Flashcards
geology
study of the earth over geologic time which includes interior, exterior, minerals, rock formation processes, and past present and future changes
geologic time scale (biggest to smallest)
- eons: we are in the phanerozoic
- era: we are on the cenozoic era
- period: we are in the quaternary period
- epoch: we are on the holocene epoch
geomorphology
the scientific study of the morphology of the surface of the earth and the processes operating on it in the present, past and future
morphologists are concerned with
- the shape composition and topological characteristics of landforms
- formation, occurance, and nature of the processes responsible for creating landforms
what are the two highest % of minerals in the earths crust
oxygen (47%)
silicon (28%)
sedimentary rock process
- rock fragments are created by chemical processes and weathering
- mass wasting (move downslope)
- transported slowly down rivers or streams
- deposition usually occurs in a body of water
- lithification - sediments are compacted together to form a new rock
three classes of sedimentary rock
- clastic
- chemical
- organic
what is a clastic sedimentary rock
contains mineral fragments derived from any of the three major rock groups ex. shale
chemical rock? how
formed from thick deposits of mineral compounds that accumulate ex. limestone which forms from calcium carbonate
what is an organic rock
consists of carbon based materials that accumulate in thick deposits at the surface and then get buried by other sediments
three major geologic developments
- formation of the shield
- formation of mountains from sediments that accumulated in basins
- deposition of sediments in shallow parts of the intervening area
who is bruce
a mosasour from around the cretaceous period, was the largest in the world for this time period and was over 13 meters in length
three key elements that make up a physiographic region
- extends over a large area
- landforms have been shaped by a common set of geomorphic processes
- common geologic structure and history
first prairie level - the Manitoba plain
surfaces modified from glaciers with some low plateaus and consist mainly of limestone and dolomite
second prairie level - Saskatchewan plain
dominated by the effects of glaciation, slightly elevated areas corresponds to low domes in the cretaceous rock below