Click on a tag to filter your results:
geochemistryphysical sciences
slumping
ground ice
permafrost thaw
surface water
water chemistry
rock chemistry
snowmelt
runoff process
waterflow monitoring
catchment drainage
ice formation
groundwater discharge
over-wintering areas
2 record(s) found for principal investigator "CLARK, Ian" (multi-year projects are grouped):
Not seeing the results you want? Tryadvanced search.
Chronology of thaw flow and geochemistry of associated massive ground ice. Fort McPherson, Northwest Territories.
Principal Investigator: CLARK, Ian D.
Licensed Year(s): 2011 2010
Summary: The main goal of this project is to determine the distribution, nature and origin of thaw flows and the associated massive ground ice bodies in Fort McPherson region, Northwest Territories. This study will use sedimentological analyses and radiocarbon datation to determine the nature and age of sediment in which massive ice is included. Radardsat 2 image from the summer 2009 will be used to eva...
Licensed Year(s): 2011 2010
Summary: The main goal of this project is to determine the distribution, nature and origin of thaw flows and the associated massive ground ice bodies in Fort McPherson region, Northwest Territories. This study will use sedimentological analyses and radiocarbon datation to determine the nature and age of sediment in which massive ice is included. Radardsat 2 image from the summer 2009 will be used to eva...
Water Quality in the Richardson Mountain catchments
Principal Investigator: CLARK, Ian D.
Licensed Year(s): 1997
Summary: The objectives of this research are to study the chemistry of the groundwaters that flow into the Little Fish River near the Cache Creek overwintering hole. The role of carbonate rocks is important as there is a lot of subsurface flow in this rock type. The presence of the aufeis (winter icing) on Cache Creek is a sign of groundwater flow, and is one of the reasons that this site was chosen. We...
Licensed Year(s): 1997
Summary: The objectives of this research are to study the chemistry of the groundwaters that flow into the Little Fish River near the Cache Creek overwintering hole. The role of carbonate rocks is important as there is a lot of subsurface flow in this rock type. The presence of the aufeis (winter icing) on Cache Creek is a sign of groundwater flow, and is one of the reasons that this site was chosen. We...
TOTAL PAGES: 1
