Contemporary Uplift and Erosion of the Southern Alps, New Zealand¶
Adams. (1980). Contemporary Uplift and Erosion of the Southern Alps, New Zealand. GSA Bulletin.
Cited by¶
1 citation across 1 artifact.
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Domain-specific¶
- Uplift
- Adams (1980) estimated that erosional mass loss approximately balances tectonic rock uplift across the belt, so the range sits close to flux steady state: high rock uplift and high exhumation coexist with near-zero surface uplift.
This sourceReports quantified uplift and erosion rates for the Southern Alps over the past ~2 m.y., both high enough that man-accelerated erosion is negligible.
Supported in partVerified against the publisher's abstract
“In the South Island of New Zealand, the pattern of uplift is relatively simple, and the uplift and erosion rates are so high that man-accelerated erosion is a negligible part.”
- Adams (1980) estimated that erosional mass loss approximately balances tectonic rock uplift across the belt, so the range sits close to flux steady state: high rock uplift and high exhumation coexist with near-zero surface uplift.
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Registry ID ref:0569c25309c0 · see in the full table