WHAT ARE TRANSFORM BOUNDARIES (FAULTS)?
At some locations on the surface of the Earth, plates are neither moving away from (diverging) or towards (converging)one another. At these points sections of the Earth slide horizontally past one another.
WHAT ARE TRANSFORM BOUNDARIES (FAULTS)? At some locations on the surface of the Earth, plates are neither moving away from (diverging) or towards (converging)one another. At these points sections of the Earth slide horizontally past one another. These zones are “necessary” because:
WHAT ARE TRANSFORM BOUNDARIES (FAULTS)? At some locations on the surface of the Earth, plates are neither moving away from (diverging) or towards (converging)one another. At these points sections of the Earth slide horizontally past one another. These zones are “necessary” because: 1.The Earth’ s surface is curved
WHAT ARE TRANSFORM BOUNDARIES (FAULTS)? At some locations on the surface of the Earth, plates are neither moving away from (diverging) or towards (converging)one another. At these points sections of the Earth slide horizontally past one another. These zones are “necessary” because: 1.The Earth’ s surface is curved. 2.Not all plate boundaries interact with each other in a simple geometric fashion. 3.
WHAT ARE TRANSFORM BOUNDARIES (FAULTS)? At some locations on the surface of the Earth, plates are neither moving away from (diverging) or towards (converging)one another. At these points sections of the Earth slide horizontally past one another. These zones are “necessary” because: 1.The Earth’ s surface is curved. 2.Not all plate boundaries interact with each other in a simple geometric fashion. 3.Rates of divergence and convergence vary globally.
03.06.a2 TRANSFORM FAULT
TRANSFORM FAULT San Andreas Fault, California
San Francisco Los Angeles Published by AAAS O. Zielke et al., Science 327, (2010)
Los Angeles San Francisco Oakland San Diego Eureka Sacramento Science 20 May 2011: Vol. 332 no pp
SAN ANDREAS FAULT
Fig. 1 Setting of El Mayor–Cucapah earthquake surface rupture and LIDAR scan. M E Oskin et al. Science 2012;335: Published by AAAS
03.07.b1 TRANSFORM FAULT - HAITI
10.13.a1 HAITI 2010
JAMAICA
PORT ROYAL JAMAICA, 1692 KINGSTON, JAMAICA, 1907
10.13.a1 LESSER ANTILLES Island Arc
SOUFRIERE HILLS MONTSERRAT