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Skip to Search Results- 2Aubet, Natalie
- 2Beckers, Justin F.
- 2Castro de la Guardia, Laura
- 2Davies, Joshua
- 2Funk, Sean P
- 2Furlong, Carolyn Marie
- 19Gingras, Murray (Earth and Atmospheric Sciences)
- 16Stachel, Thomas (Earth and Atmospheric Sciences)
- 14Alessi, Daniel (Earth and Atmospheric Sciences)
- 12Sanchez-Azofeifa, Arturo (Earth and Atmospheric Sciences)
- 11Sharp, Martin (Earth and Atmospheric Sciences)
- 10Herd, Christopher (Earth and Atmospheric Sciences)
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Climate Change Adaptation Planning at the Regional District Scale on Vancouver Island, British Columbia
DownloadSpring 2020
Society is currently faced with the complex and challenging task of responding to global climate change. Contemporary climate impacts include increasing temperatures, melting snow and ice, rising sea levels, and more extreme and variable weather events (IPCC, 2014). Vancouver Island has been...
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Spring 2020
Clay minerals are ubiquitous at the Earth’s surface and they impart a significant influence on numerous geochemical cycles due to their high surface reactivity. Aqueous pH and ionic strength (hereafter IS) are two major factors that affect clay surface reactivity and subsequently govern trace...
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Fall 2016
The increasing anthropogenic pressure on biodiversity in the tropics is resulting in changes to ecosystem structure and increasing species extinction rates (Collen et al. 2013). These issues are heightened in the tropics where 50% of the world’s biodiversity is held in 7% of the world’s...
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Circum-Arctic Glaciers, Past, Present, and Future: Current Trends in Mass Balance and Simulation of Mass Balance Sensitivity to Temperature and Precipitation Increase
DownloadSpring 2020
The circum-Arctic is a major contributor to sea level rise. Between 1991 and 2010, 70 % of eustatic sea level rise was attributable to glacier mass loss, 62 % of which was from glaciers in the circum-Arctic (Alaska, Arctic Canada North, Iceland, Svalbard, Scandinavia, and the Russian Arctic). In...
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Chemostratigraphy of the Boolgeeda Iron Formation and Turee Creek Group, Hamersley Basin, Western Australia
DownloadFall 2018
In the most general sense, the Great Oxygenation Event (GOE) refers to the transition from oxygen poor to oxygen rich conditions on ancient Earth (Holland, 2002; Holland, 2006). It has traditionally been defined as the sedimentary intervals in which the isotopic signature for mass independent...
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Chemostratigraphy and facies analysis of the Hare Indian Formation in the Mackenzie Mountains and Central Mackenzie Valley, Northwest Territories, Canada
DownloadFall 2020
The Hare Indian Formation, a Givetian aged organic rich mudstone, is the basal formation of the Horn River Group in the Northwest Territories, Canada. It is subdivided into two members: the basal Bluefish Member and the upper Bell Creek Member. Recent interest in unconventional resource plays...
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Characterizing the Impacts of Seismic Exploration Lines on the Hydrology and Vadose Zone for a Watershed in West-Central Alberta
DownloadFall 2023
Seismic lines are long linear cut lines through forests created for hydrocarbon exploration and comprise over 50 % of all linear disturbances in the Canadian Boreal Forest. They are known to impact local eco-hydrological conditions and show minimal regeneration back to pre-disturbance conditions....