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- W779833975 abstract "AN INVESTIGATION CONDUCTED TO DETERMINE THE LOCALIZATION OF THE SLIDE MASS, THE MAGNITUDE AND DIRECTION OF SURFACE DISPLACEMENT, GEOLOGICAL CHARACTERISTICS, FORM AND DEPTH OF SLIDE SURFACE AND GROUNDWATER CONDITIONS, REVEALED THAT THE SLIDES OCCUR AT THE SITES OF ANCIENT FAILURES COVERED BY TALUS UPON WHICH EMBANKMENTS HAVE BEEN CONSTRUCTION. THE SLIDE SURFACE WAS SEEN TO DEVELOP AT THE LINE OF CONTACT BETWEEN THE TALUS AND THE UNDERLYING SEDIMENTARY ROCKS. THEY MAY OCCASIONALLY DEVELOP WHERE WEATHERED SHALES ARE IN CONTACT WITH UNWEATHERED MATERIAL. THE VELOCITY OF DISPLACEMENTS REVEALS A CYCLIC LAW WHERE THE MAXIMUM MOVEMENT CORRESPONDS TO THE RAINY SEASON, WITH A LAG OF 1-2 MONTHS, AND THE MINIMUM CORRESPONDS TO THE DRY SEASON. THE TWO MAIN CAUSES FOR THE ACTIVATION OF THE SLIDES WERE IDENTIFIED AS: THE WEIGHT OF THE EMBANKMENTS WHICH INCREASES THE ACTUATING FORCES; AND THE ACTION OF WATER WHICH INFILTRATES THE HIGHLY PERMEABLE TALUS. THE METHODS EMPLOYED FOR THE CORRECTION OF THE SLIDES HAVE ELIMINATED DISPLACEMENTS OF THE FAILING MASS, AND DAMAGE TO THE ROADWAY SO ENSURING NORMAL TRAFFIC-FLOW. THE CORRECTED AREAS HAVE NOT CONTRIBUTED TO EXTRA MAINTENANCE COSTS FOR OVER FOUR YEARS. THE OBSERVATION IS MADE THAT UNDER THE PRESENT CONDITIONS OF FAILURES, ANY SO- LUTION WILL INVOLVE A DEGREE OF RISK DEPENDENT UPON THE LEVEL OF PERFORMANCE WHICH IS DESIRED. THE GEOLOGY OF THE PENINSULA AND OF THE SLIDE AREA ARE DESCRIBED AND THE FIELD CONSTRUCTION PROCEDURE IS REVIEWED." @default.
- W779833975 created "2016-06-24" @default.
- W779833975 creator A5002437105 @default.
- W779833975 date "1972-04-01" @default.
- W779833975 modified "2023-09-26" @default.
- W779833975 title "EMBANKMENT FAILURES ON THE TIJUANA-ENSENADA TURNPIKE IN THE LOWER CALIFORNIA PENINSULA, MEXICO" @default.
- W779833975 hasPublicationYear "1972" @default.
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