TY - JOUR
T1 - Bar sedimentology of the Squamish River, British Columbia
T2 - definition and application of morphostratigraphic units
AU - Brierley, G. J.
PY - 1991
Y1 - 1991
N2 - In a 20 km river reach in which channel platform changes progressively downstream from braided to meandering, there is a corresponding down-valley change in bar type from mid-channel compound bars to bank-attached compound bars to point bars. Four fluvial morphostratigraphic units, defined in terms of their surface morphology and sedimentary characteristics, are differentiated: bar platform, chute channel, ridge, and remnant floodplain. -from Author
AB - In a 20 km river reach in which channel platform changes progressively downstream from braided to meandering, there is a corresponding down-valley change in bar type from mid-channel compound bars to bank-attached compound bars to point bars. Four fluvial morphostratigraphic units, defined in terms of their surface morphology and sedimentary characteristics, are differentiated: bar platform, chute channel, ridge, and remnant floodplain. -from Author
UR - http://www.scopus.com/inward/record.url?scp=0026077245&partnerID=8YFLogxK
U2 - 10.1306/D42676D6-2B26-11D7-8648000102C1865D
DO - 10.1306/D42676D6-2B26-11D7-8648000102C1865D
M3 - Article
AN - SCOPUS:0026077245
VL - 61
SP - 211
EP - 225
JO - Journal of Sedimentary Petrology
JF - Journal of Sedimentary Petrology
SN - 0022-4472
IS - 2
ER -