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Palouse Falls

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Series: GSA Field Guide
Published: 01 January 2016
DOI: 10.1130/2016.0041(02)
EISBN: 9780813756417
... Abstract This one-day field trip of geologic and historical significance goes from Washtucna, Washington, through Palouse Falls State Park, Lyons Ferry State Park, and Starbuck, and ends in the Tucannon River valley. At Palouse Falls, it is readily apparent why Native Americans crafted...
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Series: GSA Special Papers
Published: 07 February 2019
DOI: 10.1130/2018.2538(02)
EISBN: 9780813795386
... across a single flow field to determine the internal spatio-temporal development of the Palouse Falls flow field, a lava produced by an individual Columbia River flood basalt eruption. Geochemical analyses of samples from constituent lobes of the Palouse Falls lava field demonstrate that systematic...
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Series: GSA Special Papers
Published: 01 August 2013
DOI: 10.1130/2013.2497(06)
... on the new data, the Basalts of Palouse Falls, Ginkgo, Sand Hollow, and Sentinel Gap are significantly more voluminous than previously indicated, while the Basalt of Silver Falls is significantly smaller. We have also reduced the number of units within the Frenchman Springs Member to five. The Basalt...
Journal Article
Published: 09 July 2014
Canadian Journal of Earth Sciences (2014) 51 (8): 809–824.
... (Rattlesnake Hills, Palouse Falls, and lower Ringold). The statistical similarity of Miocene floras east and west of the Cascade Range axis demonstrates that a similar mesic, warm climate across the Pacific Northwest existed during the Middle and Late Miocene. These floras represent mixed hardwood–conifer...
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Series: GSA Field Guides, GSA Field Guides
Published: 01 January 2017
DOI: 10.1130/2017.0049(09)
EISBN: 9780813756493
... the eolian supply system. Turn around and head west on Highway 261. You will cross the bridge at the Snake River and climb onto scabland topography. Turn right on Palouse Falls Road and continue to the park. An entrance fee is required. We plan to stop at Palouse Falls for lunch. This stop has a number...
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Journal Article
Published: 01 August 2002
Vadose Zone Journal (2002) 1 (1): 150–157.
... constituent in pore waters of heterogeneous materials. We measured pore-water Cl − in loess deposits of the eastern Palouse region in northern Idaho, where multiple sequences of buried soils extend to ∼20 m depth. Three cores were collected to bedrock at summit, side slope, and valley positions. Pore-water Cl...
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Journal Article
Published: 01 August 2004
Geochemistry: Exploration, Environment, Analysis (2004) 4 (3): 227–241.
...Bethany J. Nelson; Scott A. Wood; James L. Osiensky Abstract Concentrations of rare earth elements (REE) were determined in groundwaters from the Palouse Basin, located in northern Idaho and eastern Washington. Samples were taken from wells and springs tapping waters in four different rock units...
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Journal Article
Journal: Geology
Published: 01 August 2004
Geology (2004) 32 (8): 705–708.
...-cemented A-horizon cicada-burrow fabrics. The presence of the anticyclone and the suppression of dust-transporting winds generated the antiphased relationship in dust accumulation and soil formation in the Palouse compared to places like the Great Plains and Europe where thick loess accumulated during...
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Journal Article
Published: 01 May 2009
Vadose Zone Journal (2009) 8 (2): 426–436.
.... Madsen) after spring barley ( Hordeum vulgare L.)—were established at the USDA-ARS Palouse Conservation Field Station, Pullman, WA. The plots were monitored for runoff, erosion, soil temperature, water content, and depths of snow and freeze–thaw during October to May of 2003–2004 through 2006–2007...
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Series: GSA Field Guide
Published: 01 January 2016
DOI: 10.1130/2016.0041(05)
EISBN: 9780813756417
... to the east of the high from a thin layer to the west. Disrupted by lava flows, streams were pushed from a west-flowing direction to a north-northwest orientation and drained the basin through a gap between steptoes toward Palouse, Washington. Emplacement of the Roza flow of the Wanapum Basalt against...
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Journal Article
Journal: GSA Bulletin
Published: 01 December 1992
GSA Bulletin (1992) 104 (12): 1650–1671.
... deposits indicate a complex sequence of events accompanied by lava fountaining and deposition of tephra and spatter- fed flows. Deformation of the vent ramparts and breccia deposits in the vent complex suggest several lava rise/fall cycles that led to fissure widening by wall collapse. A lava pond formed...
Journal Article
Published: 01 January 2006
Vadose Zone Journal (2006) 5 (1): 261–272.
... such unconsolidated soil may result even from low intensity rainfall and saturation excess runoff ( Van Klaveren and McCool, 1998 ). Formanek et al. (1984) performed a series of shear strength experiments in both the laboratory and field with a fall-cone device. They found that, for the Palouse silt loam soil under...
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Journal Article
Journal: Geology
Published: 01 April 2004
Geology (2004) 32 (4): 297–300.
... of Quaternary paleosols in the Palouse Loess of eastern Washington ( Figs. 1 and 2 ). The Oligocene upper John Day Formation ( Retallack, 2004 ) and Quaternary Palouse Loess ( Busacca et al., 1998 ) are sequences of silt-sized, air-fall and redeposited rhyodacitic volcanic ash. Fresh volcanic ash...
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Series: Field Guide
Published: 01 January 2003
DOI: 10.1130/0-8137-0004-3.1
EISBN: 9780813756042
... Miles (km) Description 0.0 (0.0) Thompson Falls, Montana. Continue west on Highway 200. 10.2 (16.4) Turn left on Beaver Creek Road and proceed 2.1 mi (3.4 km) to the gravel pit adjacent to the road. 12.3 (19.8) Stop 1. Figure 4. Generalized map of trip route...
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Journal Article
Published: 01 November 2013
Vadose Zone Journal (2013) 12 (4): vzj2012.0200.
...I.N. Leslie; R. Heinse Abstract Soil pipes are important hillslope–hydrology features affecting mechanistic processes such as subsurface drainage, streamflow, erosion, hillslope stability, and discharge response to rain fall and snow melt. However, the limited capacity to characterize...
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Journal Article
Journal: Paleobiology
Published: 27 March 2013
Paleobiology (2013) 39 (3): 345–359.
... meets these expectations. Body-mass clumps displayed by the Marmes PHT mammal fauna fall between those of closed forests and open shrub-steppe habitats in terms of clump richness and breadth, and in terms of gap width. Marmes PHT body-mass clumps are very similar to those for the mixed habitat...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2014
GSA Bulletin (2014) 126 (7-8): 875–891.
... minimum heights up to ∼160 m, and are composed of dominantly coarse-grained, moderately to densely agglutinated and welded spatter and scoria that extend up to 750 m away from the vent. Thick, well-sorted fall deposits composed of moderately to highly vesicular scoria lapilli extend away from some vents...
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Image
Sample ordination using correspondence analysis of the interbeds examined. ...
Published: 01 September 2008
Fig. 4.  Sample ordination using correspondence analysis of the interbeds examined. The linear orientation of these data is correlated to vent proximity ( Fig. 5 ). Overall decreasing proximity trends are seen in samples from Mill Creek Road, Palouse Falls, Douglas Canyon and Locke Lake; the last
Journal Article
Published: 01 February 2013
Vadose Zone Journal (2013) 12 (1): vzj2012.0089.
...-water content and matric potential in the near surface (top 30 cm) captured the hydrologic state in both burned and unburned hillslopes during the first spring through fall period (1 June–1 Oct. 2011) after the 2010 Fourmile Canyon Fire near Boulder, CO. This time span included different hydrologic...
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Image
(A) Cliffed section of the 2660 km 3  (M8.86) Sand Hollow flood basalt flow...
Published: 01 January 2013
Figure 4. (A) Cliffed section of the 2660 km 3 (M8.86) Sand Hollow flood basalt flow from the Columbia River large igneous province (Palouse Falls, Washington), illustrating the internal morphology and potential thickness (∼60 m height) of a single, large-magnitude sheet lobe (from Bryan et al