Open Access. Powered by Scholars. Published by Universities.®
Physical Sciences and Mathematics Commons™
Open Access. Powered by Scholars. Published by Universities.®
Articles 1 - 6 of 6
Full-Text Articles in Physical Sciences and Mathematics
Zircon: Tiny Crystals With Long History And Big Uses, Jiawen Li
Zircon: Tiny Crystals With Long History And Big Uses, Jiawen Li
CLAS: Colby Liberal Arts Symposium
The first known written record about zircon dates back to c.1400. Zircon forms in felsic magmas and thus is commonly found in plutonic felsic rocks. Because of its physical resistibility to weathering and metamorphism, it is also often found in metamorphic and sedimentary rocks. zircon is an orthosilicate and therefore is made up of isolated silica tetrahedra with zirconium ions filling in the gaps. This common structure allows zircon to incorporate many trace elements, such as thorium and uranium. Zircons long physical and chemical durability and the trace elements give rise to its use in geochronology. Thorium in zircon retain …
The Limestone Neutralization Of Potential Acid Mine Drainage From Bald Mountain In Aroostook County, Maine, Brendan Cosgrove
The Limestone Neutralization Of Potential Acid Mine Drainage From Bald Mountain In Aroostook County, Maine, Brendan Cosgrove
CLAS: Colby Liberal Arts Symposium
Due to the loosening of environmental regulations in 2012, J.D. Irving, Limited may begin mining operations on massive Cu-Zn sulfide ored at Bald Mountain in Aroostook County, Maine. The Bald Mountain Project will positively and negatively impact the local economy with job creation, higher wages and income levels, but a potential decline in the recreational industry. The likely acid mine drainage (AMD) of the Bald Mountain Project can degrade aquatic ecosystems and reduce water quality and brook trout populations by metal contamination and acid loading in the local watershed. In West Virginia, in-stream limestone sand application has successfully restored streams …
Stratigraphy And Mapping Of Sandy River Floodplain Terraces, Franklin And Mercer County, Maine, Hannah Dhonau, Gift Ntuli
Stratigraphy And Mapping Of Sandy River Floodplain Terraces, Franklin And Mercer County, Maine, Hannah Dhonau, Gift Ntuli
CLAS: Colby Liberal Arts Symposium
Our project details the stratigraphy and chronology of floodplain terraces along the Sandy River in Franklin and Mercer Counties in Central Maine. Using field observations, USGS aerial photographs, and Google Earth imagery, we were able to identify three separate terraces and compare their locations to previous mapping projects in the area.
The Fluvial Sequence Of A Latest Changhsingian, Pre-Pt Extinction River Complex, Eastern Cape Province, South Africa, Tara Chizinski
The Fluvial Sequence Of A Latest Changhsingian, Pre-Pt Extinction River Complex, Eastern Cape Province, South Africa, Tara Chizinski
Honors Theses
The Permian–Triassic mass extinction, dated between 251.941 ± 0.037 and 251.880 ± 0.0371 Ma, is well documented in the marine record, but details of the event on land are still ambiguous and widely debated within the scientific community. This project focuses on the stratigraphic record leading up to the PT boundary at one of the critical sections in the Karoo Basin of South Africa, Wapadsberg Pass. A transition in river styles is reported to have occurred across the landscape from meandering Permian sandstone-dominated channels to Triassic braided complexes. This transition can be recorded by architectural elements, which reflect sensitive variations …
Deformation Mechanisms In The Metasedimentary Rocks Within The Kellyland Fault Zone, Washington County, Maine, Morgan E. Monz
Deformation Mechanisms In The Metasedimentary Rocks Within The Kellyland Fault Zone, Washington County, Maine, Morgan E. Monz
Honors Theses
This study focuses on a high-strain, strike-slip shear zone that juxtaposed metasedimentary rocks and a homogenous granite near the brittle-ductile transition, at a depth of 15-20 km. The metasedimentary rocks of the Flume Ridge Formation (FRF) exhibit a progressive deformation gradient of phase mixing and increasing fabric intensity across strike, northwest-to-southeast, approaching the center of the shear zone. Deformation mechanisms were controlled by metasomatic reactions in a fluid-rich fault zone. During deformation, biotite and potassium feldspar in the metasedimentary rocks reacted to form phengite—a much weaker phase. The nucleation and growth of weak phases, combined with phase mixing, decreased the …
Deformation Mechanisms In Mylonites At Fletcher Peak, Washington County, Me, Ariana S. Boyd
Deformation Mechanisms In Mylonites At Fletcher Peak, Washington County, Me, Ariana S. Boyd
Honors Theses
Mylonite formation and development is dependent on a number of factors including temperature, strain rate, and fluid fugacity. All three factors affect flow stress and viscosity; thus, a variance in each will affect the development of mylonites. This study focuses on factors leading to the formation of mylonite surrounded by ultramylonite of the same protolith, along-strike to one another at the center of a fault zone. The rocks in question are from the Deblois granite cut by the Kellyland fault zone, a ductile strike-slip fault zone within the larger Norumbega fault system in eastern Maine. The Deblois granite as a …