Transcurrent Fault (Strike-Slip Fault) - Vertically dipping fault that results from horizontal shear stress. Slip movement during an earthquake is sideways rather than up or down.

Transcurrent Fault (Strike-Slip Fault)

Vertically dipping fault that results from horizontal shear stress. Slip movement during an earthquake is sideways rather than up or down.

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Word of the Week – Vadose Zone

Word of the Week – Vadose Zone

Vadose Zone A hydrogeological term that represents the volume of rock and unconsolidated materials between the ground surface and the underlying water table, in which pores and cracks are...

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Word of the Week – Wairakite

Word of the Week – Wairakite

Wairakite A zeolite mineral of hydrothermal origin that was first identified in the Wairakei geothermal field in New Zealand by Alfred Steiner. It forms clear to white prismatic crystals,...

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