The article deals with the results obtained by investigating the conditions for the development of flow landslides. Their manifestation is stipulated by the periodical deformation of the structure of water-saturated clayey soil with coagulation contacts between particles. It has been established that the structural deformation of soil is associated with a considerable increase in the pore-water pressure developed in the body of the landslide.

  • Corporate Authors:

    International Railway Congress Association

    17-21 rue de Louvrain
    1000 Brussels,   Belgium 
  • Authors:
    • Goldstein, M N
    • Turovskaya, A Y
  • Publication Date: 1975-1

Media Info

  • Features: Figures; References; Tables;
  • Pagination: p. 14-18
  • Serial:

Subject/Index Terms

Filing Info

  • Accession Number: 00095688
  • Record Type: Publication
  • Source Agency: Rail International
  • Files: TRIS
  • Created Date: Jul 15 1975 12:00AM