In geological and geomorphological terms, a matureland refers to a landscape that has reached a "mature" stage of erosion. This concept was notably applied to the unique geography of northern Chile. The Geologic Concept

Use this as a prime example of a late-Tertiary rolling matureland at elevations of 2,200 to 2,700 feet, which was subsequently dissected by younger cycles. Andean Forearc (Chile/Peru):

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   Explain its role as a transitional state between "youth" (steep, rapid erosion) and "old age" (peneplanation). Thesis Statement: