15 research outputs found
Chemistry of thermal waters and mineralogy of the new deposits at Mount St. Helens: a preliminary report
After May 18, 1980 eruption of Mount St. Helens, Washington, interactions between the hot deposits and shallow ground water produced ephemeral phreatic eruptions and thermal ponds and streams. In early June water and sediment samples were collected from about 20 sites in the devastated zone to study the initial alteration of the new deposits, and the effects of the eruption on water chemistry. The levels of certain trace elements in thermal waters, and whether these mineralized waters were reaching the North Fork Toutle River in appreciable quantities were studied. Collection and analysis procedures, the mineralogy of the new deposits, and the chemistry of the thermal waters are discussed. Finally, the chemistry of water from different deposits is compared, alteration reactions suggested by the water chemistry, and the mineralogy of the deposits is discussed
Basins and bedrock: spatial variation in 10Be erosion rates and increasing relief in the southern Rocky Mountains, USA
We used measurements of cosmogenic 10Be in alluvium to estimate
erosion rates on a 103–104 yr time scale for small (0.01–47 km2),
unglaciated basins in northern Colorado, southern Wyoming, and
adjacent western Nebraska (western United States). Basins formed
in Proterozoic cores of Laramide ranges are eroding more slowly (23
± 7 mm k.y.–1, n = 19) than adjacent basins draining weakly lithifi ed
Cenozoic sedimentary rocks (75 ± 36 mm k.y. –1, n = 20). Erosion
rates show a relationship to rock resistance and, for granitic rocks,
to basin slope, but not to mean annual precipitation. We estimated
longer-term (>105 yr time scale) erosion rates for the granitic core of
the Front Range by measuring the concentration of 10Be and 26Al produced
mainly by muon interactions at depths 1.7–10 m below the surface.
Concentrations imply erosion rates of 9–31 mm k.y. –1, similar to
shorter-term erosion rates inferred from alluvial sediment. The spatial
distribution of erosion rates and stratigraphic evidence imply that
relief in the southern Rocky Mountains increased in the late Cenozoic;
modern relief probably dates from post-middle Miocene time