1-16 OF 16 RESULTS FOR

Heumoes Slope

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 December 2013
Journal of Environmental and Engineering Geophysics (2013) 18 (4): 269–280.
...Marco Walter; Joan Gomberg; William Schulz; Paul Bodin; Manfred Joswig Abstract In this study, we describe conditions for slidequake generation at three different creeping softrock landslides: the Slumgullion landslide in the San Juan Mountains, Colorado, U.S., the Heumoes slope in the Austrian...
FIGURES | View All (10)
Journal Article
Published: 01 May 2011
Vadose Zone Journal (2011) 10 (2): 487–495.
... Heumoes slope consists of weak sediments (loamy scree and glacial till) and moves an average of a few centimeters per year at the surface. The seismic detection of single fracture processes or initial stress relief resolves the creeping movement of the slope into discrete rupture episodes. The spatial...
FIGURES | View All (9)
Image
General set-up of the <b>Heumoes</b> <b>slope</b>, average sliding velocities (after  Dep...
Published: 01 December 2013
Figure 2 General set-up of the Heumoes slope, average sliding velocities (after Depenthal and Schmitt, 2003 ), and locations of installed seismometer stations of the permanent seismic network.
Image
Locations and magnitudes of observed slidequakes at <b>Heumoes</b> <b>slope</b> during fi...
Published: 01 December 2013
Figure 7 Locations and magnitudes of observed slidequakes at Heumoes slope during field campaigns between 2005 and 2008 (light grey dots) and the permanent seismic monitoring between July 2009 and May 2011 (dark grey dots).
Image
Location of the <b>Heumoes</b> <b>slope</b> and general setup, with locations of the well...
Published: 01 May 2011
Fig. 1. Location of the Heumoes slope and general setup, with locations of the well, the weather station, and drillings. The movement velocities determined by global positioning system and terrestrial measurements are after Lindenmaier et al. (2005) .
Image
Epicenters of the localized fracture processes at the <b>Heumoes</b> <b>slope</b> during ...
Published: 01 May 2011
Fig. 8. Epicenters of the localized fracture processes at the Heumoes slope during the field campaigns between 2005 and 2008.
Image
The <b>Heumoes</b> <b>slope</b> in Ebnit, Voralberg (Austria): (A) top view and views fro...
Published: 01 May 2011
Fig. 12. The Heumoes slope in Ebnit, Voralberg (Austria): (A) top view and views from (B) east to west and (C) southeast.
Image
The <b>Heumoes</b> <b>slope</b> with indicated representative cross-sections (red lines) ...
Published: 01 May 2011
Fig. 13. The Heumoes slope with indicated representative cross-sections (red lines) and boreholes (HH04 and KB03); gray denotes post glacier, yellow denotes moraine, and green is solid rock. Figure adapted from Lindenmaier (2008) .
Image
Representative cross-sections through the <b>Heumoes</b> <b>slope</b> from (A) north to s...
Published: 01 May 2011
Fig. 14. Representative cross-sections through the Heumoes slope from (A) north to south and (B) west to east; \batchmode \documentclass[fleqn,10pt,legalpaper]{article} \usepackage{amssymb} \usepackage{amsfonts} \usepackage{amsmath} \pagestyle{empty} \begin{document} \({\bar{h}}_{p}^{\mathrm{W
Journal Article
Published: 01 May 2011
Vadose Zone Journal (2011) 10 (2): 512–525.
...Fig. 12. The Heumoes slope in Ebnit, Voralberg (Austria): (A) top view and views from (B) east to west and (C) southeast. ...
FIGURES | View All (17)
Image
Schematic illustration of preferential slidequake generation at <b>Heumoes</b> slo...
Published: 01 December 2013
Figure 8 Schematic illustration of preferential slidequake generation at Heumoes slope (landslide and bedrock geometry modified after Walter et al., 2011 ).
Image
Comparison of typical seismograms and sonograms of observed slidequakes wit...
Published: 01 December 2013
Figure 4 Comparison of typical seismograms and sonograms of observed slidequakes with local earthquakes. (a) Slidequake observed at Heumoes slope (M L  =  −1.4 in ∼180 m distance). (b) Slidequake observed in Super-Sauze (M L  =  −2.4 in ∼100 m distance). (c) Slidequake observed at Slumgullion
Journal Article
Published: 01 September 2014
Journal of Environmental and Engineering Geophysics (2014) 19 (3): 139–155.
... landslide characterization and hazard potential classification of similar glacial deposits on slopes in the Adirondacks region. During the late Wisconsinan, ice retreated across New York State while the glacier acted as a dam at the north end of Keene Valley and impounded water in the valley. Glacial Lake...
FIGURES | View All (8)
Journal Article
Published: 01 December 2013
Journal of Environmental and Engineering Geophysics (2013) 18 (4): 201–203.
... and French Alps and in the San Juan Mountains of Colorado, U.S. Their paper “ Slidequake generation versus viscous creep at soft rock landslides: Synopsis of three different scenarios at Slumgullion landslide, Heumoes slope, and Super-Sauze mudslide ” discusses the origin of the process and how it might...
Journal Article
Published: 01 April 2020
Seismological Research Letters (2020) 91 (3): 1820–1830.
... different scenarios at Slumgullion Landslide, Heumoes Slope, and Super‐Sauze Mudslide Slidequake Generation vs. Viscous Creep at Softrock‐landslides , J. Environ. Eng. Geophys. 18 , no.  4 , 269 – 280 . Wang T. Shi Q. Nikkhoo M. Wei S. Barbot S. Dreger D. Bürgmann R...
FIGURES | View All (10)
Journal Article
Journal: Interpretation
Published: 11 February 2014
Interpretation (2014) 2 (1): SB27–SB44.
... into five subtypes by comparing the geometric relationship of the slope of the pore pressure gradient and two prominent benchmark gradient trends, lithostatic and hydrostatic (Figure  2 ). Hydrostatic pressure is the weight of a column of water, usually of varying salinity and density, which extends from...
FIGURES | View All (16)