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In the southwestern USA, relative motion between the Paci c and North American plates occurs at a rate of about 48 50 mm a 1 (DeMets & Dixon, 1999; Sella et al., 2002). Geodetic and seismologic data suggest that up to 70% of this motion presently may be accommodated by dextral slip on the San Andreas Fault (Argus & Gordon, 2001). Out of a total of approximately 1100 1500 km of strike-slip motion, since the Oligocene (Stock & Molnar, 1988), only 300 and 450 km of right lateral slip have accumulated along the southern and northern reaches of the San Andres Fault, respectively (Dillon & Ehlig, 1993; James et al., 1993). The remaining movements, therefore, must be accommodated elsewhere within the diffuse zone of deformation that stretches from the Coast of California to the Basin and Range (Fig. 8.1). Along its 1200 km length, the San Andreas Fault is divided into segments that exhibit different short-term mechanical behaviors. Some segments, such as those located north of Los Angeles and north of San Francisco, have ruptured recently, generating large historical earthquakes, and now exhibit little evidence of slip. These segments appear locked at depth and are now accumulating signi cant nonpermanent (elastic) strains near the surface, making them a major potential earthquake hazard (Section 2.1.5). Between the two locked segments is a 175-km-long fault segment in central California that is characterized by aseismic slip, shallow (<15 km depth) microearthquakes, and few large historical earthquakes. Along this segment, the aseismic slip re ects a relatively steady type of creep that results from frictional properties promoting stable sliding on the fault plane (Scholz, 1998). These different behaviors, and especially the occurrence of aseismic creep on or near faults at the surface, complicate the estimation of horizontal velocity elds (Section 8.5.3).

5-18

Directory Enter the directory in which publicly accessible documents are stored on the server. Typical host directory names are www/public/docs/ and public_html/. Your remote site root folder is a subfolder of the host directory. If you are unsure of the exact name of the host directory, check with your Web server administrator. Often, the FTP host connects to the correct directory automatically, and you can leave this field blank. the login name you have been assigned for access to the Web server. the password necessary for you to gain access to the Web server. Note that many servers are case-sensitive when it comes to logins and passwords!

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The following sections provide a summary of the software and other materials you ll find on the CD.

including passwords, host IDs, public key handshakes, Kerberos, and PAM, and can use strong authentication, such as SecurID tokens or smart cards SSH also transparently secures communication between existing clients and servers using port forwarding There are two versions of the SSH protocol Version 1, developed in 1995 by Tatu Yl nen at Helsinki University of Technology in Finland, and version 2, developed in 1998 by Yl nen and other members of the IETF Secure Shell working group The two versions are not compatible, and open source and commercial products for both protocols exist Although SSH is available for a wide variety of platforms, it is predominantly used on Unix SSH closes many security holes for Unix systems administrators by replacing the Berkeley remote r-commands: rsh, rcp, rlogin, rexec, and so on, with secure alternatives There are many websites on the SSH protocol and products including wwwsshcom, www.

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openSSHcom, and wwwf-securecom We also refer the reader to Barrett and Silverman s excellent and comprehensive book, SSH: The Definitive Guide [BS01] Administrators can use slogin instead of rlogin to connect to remote hosts, ssh instead of rsh to run shell commands on remote hosts, scp instead of rcp to copy files, sftp instead of FTP for secure file transfers, and so on Users launch a client process sshagent once during each login session The agent holds the unlocked private key and brokers all further ssh handshakes transparently SSH can perform TCP port forwarding to encrypt data passing through any TCP/IP connection, conduct reverse IP lookups to protect against DNS spoofing, provide access control on the server based on Unix user names or groups, and vendors provide some support for key management and OA&M (although not enough) SSH solves a specific security need in a transparent manner.

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