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Rockfall analysis programs  
Links Conefall 1.0  
Links softs Matterocking  
Mattercliff  
Thermic  
Contact THERMWAT 1D  
Quanterra
Dr. M. Jaboyedoff

Ch. Tour-Grise 28
1007 Lausanne
Switzerland
Tel: ++41 79 752 35 15
 
XRD Clay Mineralogy  
Patissier  
E-mail: mail@quanterra.org COLTOP-3D  

If an announced soft is needed, it is possible to contact Quanterra to obtain a beta versioin (excepted Coltop 3D).

Contact: support@quanterra.org

 
 
 

 

Open-report – soft - 01

Example displayed in Surfer program. In grayed the source pixel with black =0° and white for 360° (note that the contouring introduce artifacts). The contours indicate the number of contribution cones (yellow-red gradient).

CONEFALL 1.0 (download)

Download User's guide

Developed in collaboration with LMR in EPFL

The program CONEFALL is designed to estimate roughly the potential rock falls prone area.

Theory related to this program can be found in many different articles (Evans and Hungr, 1993, Toppe, 1984). The basics are described in an article: CONEFALL: CONEFALL: a program for the quick preliminary estimation of the rock-fall potential of propagation zones (Jaboyedoff and Labiouse, submitted).
The principle of the program is rather simple. A block can propagate if the slope is sufficiently steep. Physically consider that if the slope is steeper than a limit jp, then the block accelerates. If it is lower, it decelerates. Using the previous assumption, a block can propagate from its source to the point of intersection of the topography with line starting from the source point making an angle jp with horizontal. The space where a block can propagate from a grid point is located within a cone of slope jp with a summit placed at the source point (Fig. 1.1). This procedure is applied to all source points.
The source points can either be considered as the entire cliffs, the border of the cliff or its bottom. Using simple consideration it can be shown that the mean velocity of blocks is given a function of the difference in altitude Dh between the cone and the topography. Dh is proportional to the kinetic energy that may be acquired by the block during the fall.
Note that CONEFALL can be used to roughly define the potential propagation zone for a landslide.

Soft

Main window of the program, containing the five types of windows

MATTEROCKING

Written by Quanterra as subcontractor for the CREALP

Available on: www.crealp.ch

The program MATTEROCKING 2.0 is designed to estimate the average number of discontinuities on digitized topographic relief. This software is used for potential rock slope instabilities detection.

Theory can be found elsewhere in articles (Jaboyedoff et al., 1996; Rouiller et al., 1997; Jaboyedoff et al., 1999, Baillifard et al., 2001).
Using digital elevation model (DTM), the program Matterocking permits to compare structural data with topographic surface orientation in order to estimate the average number of discontinuities intersecting a topographic relief. Locations where rock-instabilities can occur by discontinuities or wedges that allow sliding can be spotted. Different functions are implemented such as estimates of potential sliding areas, surface number, and linear number of discontinuities within cell of the DTM.
Matterocking is designed to calculate and not to generate graphic outputs. Nevertheless, some visualization utilities exist to have a quick view of the results. The file format are chosen in order to be used in to standard visualization program: Surfer Golden software© and ArcView ESRI©.

Soft

 

MATTERCLIFF

Designed by M. Jaboyedoff as subcontractor for the CREALP

Written by J.-Y. Delèze at CREALP

Help on-line

Available on: www.crealp.ch

What is MatterCliff ?

MatterCliff is an interactive and simple to use tool for the characterization of discontinuities and the analysis of rock slopes stability. This software aims at the implementation of various geotechnical, statistical and probabistic methods in a multiple-document application comprising five major parts :

1. the statistical study of spatial distribution of discontinuity family using spacing histograms and variographic analysis
2. the semi-automatic digitization of discontinuities from scanned images or outcrop sketches
3. the analysis of simple probabilistic models
4. an utility for the pre-analysis of orientation data : angle conversions, coordinates calculations, intersection of planes
5. a tool for the computation of the volume generated by 2 or 3 families of discontinuities

Soft

PATISSIER (Download page)

Software to estimate the smectite content and number of consecutive illite layers in mixed-layer illite-smectite using illite crystallinity data

Open-report – soft - 02

Example of TOP3D display.

Soon available (May)!

COLTOP-3D

A pseudo-3D topographic analysis computer program.

This software COLTOP-3D can be used to analyze the structures, especially faults, shaping the morphology.
Maps as well as stereonets displaying colors depending on the orientation will be implemented. Histograms of topographic surface are planned. The design of tools useful to analyze topography in a structural way is planned. Faults tracing will be implemented based on orientation and surface points.

Soft

Soon available!

THERMWAT 1D

A 1D thermal modeling with water inflow