Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.

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Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US Tempat Pelaksanaan: Ruang Pangea, Laboratorium Gempabumi (LabEarth) – Puslit Geoteknologi LIPI dan Kuliah lapangan akan dilakukan disekitar Sesar Lembang, Jawa Barat. * Lebih jelas baca TOR/KAK dan daftar acara

Subduction II: Sumatra Outline of this lecture Reminder of coral microatolls 1935 earthquake (microatolls) 1833 earthquake (microatolls) 2004 earthquake (coseismic and post seismic from GPS) Supercycles on the Sumatran interface

Subduction zones and earthquakes induce coastal uplift and subsidence Indonesian fore arc islands Alaskan forest Honshu coast umatra/educational.html And McAllpin

1964 Great Alaska earthquake

Porites coral grows in annual rings, much like a tree. It prefers to be just below the sea surface. /highlights/sumatra/coral.html Coral Microatolls: natural geodesy

Burbank and Anderson, 2011, Tectonic Geomorphology, Chapter 5

--Credit: Danny Natawidjaja, Kerry Sieh, Tectonics Observatory

Burbank and Anderson, 2011, Tectonic Geomorphology, Chapter 6

The large yellow arrows in the lower panel point to small emergences due to three distant giant earthquakes (1797, 1833, and 1861; >M8.5), as well as a large emergence due to a local large earthquake (1935; M7.7). Credit: Danny Natawidjaja's Caltech thesis, 2002; Cross section of a Porites coral along with the resulting analysis of uplift and subsidence

Burbank and Anderson, 2011, Tectonic Geomorphology, Chapter 6

Zachariasen, et al., 1999

Sieh, et al. 2008

Subduction II: Sumatra Outline of this lecture Reminder of coral microatolls 1935 earthquake (microatolls) 1833 earthquake (microatolls) 2004 earthquake (coseismic and post seismic from GPS) Supercycles on the Sumatran interface

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