Transform faults are :
Strike-slip faults
Strike-slip faults option is correct.
Transform faults, first recognised by J. Tuzo Wilson in 1965, are plate-boundary structures along which two lithospheric plates slide horizontally past one another. Because the relative motion is parallel to the fault trace, the slip vector is horizontal and the fault is by definition a strike-slip fault; the San Andreas fault and the mid-ocean ridge offsets are the archetypal examples.
Reverse and thrust faults involve hanging-wall-up dip-slip motion under compression, producing crustal shortening — the mechanics of collisional belts, not of transform boundaries. Normal faults have hanging-wall-down dip-slip under extension, characteristic of rifts and passive margins. None of these produces the pure lateral offset that defines a transform.
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Important Questions from Mixed Topic (MH-SET)
.................... is a client server application that identifies each host on the internet with a unique user-friendly name.
Every OS has a ................ or .......... which primarily resides in the main memory of the computer to perform some of the basic functions of the OS.
(i) Kernel
(ii) Interface
(iii) Nucleus
(iv) Compiler
Codes:
Which of the following are referred to as low level language?
(i) Machine language
(ii) Assembly language
(iii) High level language
(iv) Natural language
Codes:
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List I List II (a) New York Public Library (i) Shelv AR (b) Miami University Augmented Research Group (ii) Smart library (c) Oula University Library (iii) Wolf Walk (d) North Carolina State University (iv) Find the future Codes:
Which part of the QR code represents the encoded data?
