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GEOG 3000 - Lecture Notes

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All of the lecture notes from GEOG 3000 - Geomorphology, taught at the University of Guelph. All hand-written notes.

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  • December 19, 2022
  • 57
  • 2022/2023
  • Class notes
  • Jackie cockburn
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GEOG 3000

,NOTES

, Geomorph Refresher
GEOMORPHIC PRINCIPLES
Balance / landforms and
equilibrium between Processes may be linked such tha
_
-




processes may initiate the action of another
Perceived Can
equilibrium is created by the interaction view over various time interva
-





of force and resistance framework used will have an effe
that
Changes in
driving force and/or resistance may can be made about processes an
-




stress the system beyond the defined limits of

stability >
-
thresholds and complex responses


DIVERSITY OF FORM
Ephemeral usually dry except immediately after Channel substrate
- -
-




rainfall '


Bedrock -
> alluvial
.

Perennial -
flows year round-
'

Southern Ontario -
> semi -

alluvial




DRAINAGE NETWORK PATTERNS grow upslope +



into continuous stream
integrate

Dendritic trellis parallel radial
rectangular
-




, , , ,




DRAINAGE DENSITY
Glock 11931 ) proposed 5 / see picture)
stages



continued channel
erosion -7 losses
focuses
21st century work on
geological variability first-order
'

of
streams

through time and space

lithology
↳ Tectonic activity , ,
structure

, Factors in Fluvial Systems
WHAT FACTORS INFLUENCE RIVER SYSTEMS ?
Climate / weather
Vegetation human anim
-




non
-
+ -




Interactions with humans
Topography
-
'




Geology
.




PROCESS + FORM
sediment
Example of connectivity in a riv
-




yield


)

longitudinal water mov
-




< to downstream
↳ lateral -
channel < >
flo
↳ Vertical
groundwater
- <

branches ,
]
logs ,
etc .




all connected to
one another

c)


FACTORS THAT INFLUENCE SHAPE
Balance of and forces Variation of
driving resisting discharge
- .




Erosion of channel boundary Channel slope ( called gradie
.
-




deposition of sediment 95% of
Reworking and is used to overc
-




energy
'








Depends on channel type 1 bedrock us alluvial) .
resistance
5% of is used for
energy geom
-
~




DRAINAGE NETWORK PATTERNS
Parallel trellis and patterns Radial commonly found vo
rectangular is on
-


are
-




, ,



due to structural
geography
DRAINAGE DENSITY
Space for time studies 21st century work focuses
^


on
.
- -





subspace for time variability
↳ Look at 1000 Channels ↳
through space and tim
over one year Tectonic activity ,
litholog
instead of 1 Channel over 1000 years

FLOW AND SEDIMENT SUPPLY
Form
adjusts in response to fluctuations in
-

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