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The AB Real Book C Bass-Clef Edition: Bass Clef Instruments
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Which usually takes one working day. Express delivery to the UK is via UPS and is guaranteed to be delivered the day after the order is despatched. A signature is required on delivery. Thibaud Simon-labric. Donna Whitney. David Shuster. Peter Reiners. Peter van der Beek. Low-temperature thermochronologic signature of range-divide migration and breaching in the North Cascades.
Brocard3, Christian Teyssier4, Peter A. Reiners5, David L. Shuster6,7, Kendra E.
Category:For cello, continuo
Murray5, and Donna L. Such migration is often inferred from existing asymmetries, but direct evidence for the migration is often lacking. New low-temperature apa- tite cooling ages from a transect across the northern North Cascades range Washington, NW USA and from two elevation profiles in the Skagit River valley record faster denudation on the western, wetter side of the range and lower denudation rates on the lee side of the range.
This difference has already been documented further south along another transect across the range; however, in the south, the shift from young cooling ages to older ages occurs across the modern drainage divide. Here, further north, the shift occurs along a range-transverse valley within the Skagit Gorge. It has been proposed that the upper Skagit drainage was once a part of the leeward side of the range but started to drain toward the western side of the range across the Skagit Gorge in Quaternary time.
In the m-deep, V-shaped Skagit Gorge, river stream power is still high, suggesting that incision of the gorge is still ongoing. Several other similar events have occurred along the range during the Pleistocene, supporting the proposed hypothesis that the repeated southward incursions of the Cordilleran ice sheet during this period triggered divide breaching and drainage reorganization by overflow of ice-dammed lakes at the front of the growing ice sheet.
Since these events systematically rerouted streams toward the wet side of the range and resulted in leeward migration of the divide, we propose that in fact the Cordilleran ice sheet advance essentially catalyzed the adjustment of the mountain chain topography to the current orographic precipitation pattern.
Such theoretical adjustment is et al. However, in Climate is thought to have a global effect on difficult to document in natural systems due to certain circumstances, the incision of deep can- the erosion and topography of mountain ranges the continuous erosion of the ridge crest dur- yons associated with drainage reorganization e. Divide migration is thought can leave a detectable footprint in the record of al. Many charac- to occur by progressive, diffusive lateral slope low-temperature cooling ages Flowers and Far- teristics of mountain topography are expected retreat or in successive discrete jumps by cap- ley, ; Karlstrom et al.
Physical al. In addition, north of Reconstruc- Cordilleran ice sheet Fig. The ice sheet blocked many of mountain ranges. As topography approaches distal proxies, such as changes in the routing of north-draining valleys, initiating reversals geomorphic steady state, divide migration river sediments sourced in specific areas e.
Numerous deeply incised results in a progressive decline in slope on the Craw et al. A Location of the northern Washington Cascades. Circles—new ages, squares—published ages Reiners et al. Black arrows— present-day river flow direction; white dashed arrow—paleoflow direction; blue dashed line—southern extent of the latest Pleistocene advance of the Cordilleran ice sheet south of the ice sheet, the range was occupied by locally fed valley glaciers.
C—D Two east-west transects across the North Cascades at latitudes One of them, the In this study, we use low-temperature ther- valley across the North Cascades and along two Skagit River Gorge, is a 2-km-deep, V-shaped mochronology to test this hypothesis and date elevation profiles in and upstream eastward of section of the Skagit River valley, a km- the drainage adjustment.
The million- long range-transverse valley crossing the North climate has been shown to strongly impact ero- year denudation pattern is well correlated with Cascades. Riedel et al. Orographic the orographic precipitation pattern across the gorge formed during the Pleistocene by west- precipitation appears to drive enhanced erosion range.
However, unlike in the southern part of ward overspill of a proglacial lake, and this of the wet, windward side of the range over the range at However, the marine isotope the ancestral upper Skagit when the Cordilleran divide. Age-elevation profiles along the Skagit record suggests that these are but a fraction of ice sheet invaded its lower reaches.
Booth et al. At its larg- at the current location of the Skagit Gorge. In effect, this event displaced the range drainage of the wet side of the range. Because lake lyzed drainage reorganization and forced long- phy of the Washington Cascades Mitchell and overspill is an efficient way to overcome high- term migration of the drainage divide toward the Montgomery, Aside from Quaternary stra- standing divides in deeply incised landscapes, it dry side of the range.
This correlation suggests that USA. Along the Miller et al.
The North Cas- V-shaped Skagit Gorge, which connects the reach of higher river gradient as it passes the cades range has not been affected by significant upper and lower U-shaped segments of the river Skagit Gorge Fig. It has been proposed that the lated to any active fault, lithological contact, Skagit Gorge is a recent topographic feature or junction of overdeepened glacial valleys. Originally, the paleo— area of the Skagit River.
We calculated mean The North Cascades currently block mois- upper Skagit River drained northward along a annual river power w W m—2 for the Skagit ture influxes from the Pacific Ocean in the west. Paleoclimate data Gorge Fig. Mathews, ; Haugerud, To account for the spatial ery, Locally sourced mountain glaciers nection to the lower Skagit River Riedel et al.
The river channel width decreases repeatedly spread southward over the northern addition, the modern pass between the upper, as slope increases within the Skagit Gorge and part of the Washington Cascades Fig. Because the reservoirs prevent any and Thorson, ; Clague, Deposits in upper, north-flowing branch of the Fraser River precise measurement of the channel width, we the Puget Lowland indicate that the Cordilleran is a nice example of wind gap, which localizes also estimated the stream power using an equa- ice sheet has spread over the western piedmont the paleoflow of the upper Skagit Fig.
A Topographic cross 15 - 20 6. D Com- parison of unit stream power W m—2 and AHe ages of valley- profile Drainage ar modern Skagit River ea floor samples.