In physiography and geology, a horst is an elevated fault segment restricted by common faults. In other words, a horst is an elevated block of the Earth's crust that has raised or has endured stable, while the area on either surface (graben) has sunk. The horsts may have both regular and asymmetrical cross-sections.
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In physiography and geology, a horst is an elevated fault segment restricted by common faults. In other words, a horst is an elevated block of the Earth's crust that has raised or has endured stable, while the area on either surface (graben) has sunk. The horsts may have both regular and asymmetrical cross-sections.