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<front>
<journal-meta>
<journal-id journal-id-type="publisher">NHESS</journal-id>
<journal-title-group>
<journal-title>Natural Hazards and Earth System Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">NHESS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Nat. Hazards Earth Syst. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1684-9981</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/nhess-4-187-2004</article-id>
<title-group>
<article-title>Design of a geodetic database and associated tools for monitoring rock-slope movements: the example of the top of Randa rockfall scar</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Jaboyedoff</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ornstein</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Rouiller</surname>
<given-names>J.-D.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Quanterra, Ch. de la Tour Grise 28, 1007 Lausanne, Switzerland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Centre de Recherches sur l’Environnement Alpin, 1950 Sion, Switzerland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>04</month>
<year>2004</year>
</pub-date>
<volume>4</volume>
<issue>2</issue>
<fpage>187</fpage>
<lpage>196</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2004 M. Jaboyedoff et al.</copyright-statement>
<copyright-year>2004</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 Generic License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by-nc-sa/2.5/">https://creativecommons.org/licenses/by-nc-sa/2.5/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://nhess.copernicus.org/articles/4/187/2004/nhess-4-187-2004.html">This article is available from https://nhess.copernicus.org/articles/4/187/2004/nhess-4-187-2004.html</self-uri>
<self-uri xlink:href="https://nhess.copernicus.org/articles/4/187/2004/nhess-4-187-2004.pdf">The full text article is available as a PDF file from https://nhess.copernicus.org/articles/4/187/2004/nhess-4-187-2004.pdf</self-uri>
<abstract>
<p>The need for monitoring slope movements increases with the increasing
need for new areas to inhabit and new land management requirements. Rock-slope
monitoring implies the use of a database, but also the use of other tools to facilitate
the analysis of movements. The experience and the philosophy of monitoring the top
of the Randa rockfall scar which is sliding down into the valley near Randa village in
Switzerland are presented. The database includes data correction tools, display
facilities and information about benchmarks. Tools for analysing the movement
acceleration and spatial changes and forecasting movement are also presented. Using
the database and its tools it was possible to discriminate errors from critical slope
movement. This demonstrates the efficiency of these tools in monitoring the Randa
scar.</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
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