A Graben can produce a Normal Fault.
Normal
Horsts and grabens
it made up of normal faults, grabens and horsts
Peter Eric Johnson has written: 'The origin of the Chiwaukum graben, Chelan County, Washington' -- subject(s): Grabens (Geology)
Rift basins are depressions within the crust and lithosphere that are associated with extensional tectonics. The presence of active normal faulting itself, creates the accomodation space for sedimentary infill within grabens and half graben structures.
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A Graben is the result of a block of land being downthrown producing a valley with a distinct scarp or "escarpment" on each side. An example would be a rift valley such as the Jordan valley (containing the dead sea) or the East African rift valley system or the Rio Grande Rift in New Mexico and west Texas.Grabens often occur side-by-side with Horsts. (see related link below).A Horst is the reverse of a Graben, it forms as a residual elevated block of land left between the formation of two parallel Graben. An example of a Horst would be the Black Forrest mountains, and the Ruwenzori Range.
By plate tectonics. Continental collision compresses, folds, faults and lifts the land. Crustal tension stretches the basement rock, causing down-warping and faulting, grabens, etc.
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What to produce is one of the high economic problem
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Actually it is not those questions. They are: What to produce?How to produce? i.e: where? what techonolgy? labour? etc.For whome to produce?