Abstract
The Kirikubo Landslide is a Late Pleistocene large-scale landslide in the northern Nagano Prefecture, central Japan. The Tateyama E Tephra Bed just conformably overlies the main slip scarp, suggesting that the Kirikubo Landslide occurred primarily at 60 to 75 Ka. Secondary smaller-scale landslide cut the primary landslide mass at 7 to 10 Ka, based on the age of archaeological site on the slide blocks.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
