Lithospheric foundering, or delamination, refers to the loss and sinking (foundering) of a portion of the lowermost lithosphere from the tectonic plate to which it was attached. The lower part of the lithosphere, called the mantle lithosphere, is denser than the asthenosphere below it. According to Wikipedia:
“Delamination occurs when the lower continental crust and
mantle lithosphere break away from the upper continental crust. There are two
conditions that need to be met in order for delamination to proceed:
· The
lower lithosphere must be denser than the asthenosphere.
· The
intrusion of more buoyant asthenosphere making contact with the crust and
replacing dense lower lithosphere must occur.
Density inversions are more likely to occur where there are
high mantle temperatures. This limits this phenomenon to arc environments,
volcanic rifted margins and continental areas undergoing extension.”
There are two main geological
effects of delamination: uplift of the crustal lithosphere into mountain ranges
and volcanism as hot mantle material breaks through the thinned lithosphere.
When Seismologist Deborah
Kilb was studying California Earthquake records, she noticed a series of quakes
that should have been too deep into the mantle for seismic activity due to the
high pressures and temperatures. The source of these quakes was nearly twice as
deep as the deepest California earthquake epicenters at about 11km (6 miles).
The deeper quakes were centered 18km (11 miles) below the surface. Some quakes
were 20-40km (12.4-25 miles) below the surface.
Kilb shared the earthquake
data with Vera Schulte-Pelkum, a research scientist at the Cooperative
Institute for Research in Environmental Sciences and an associate research
professor of geological sciences at the University of Colorado Boulder, who was
studying deep rock deformations under the Sierra Nevada. They then utilized a
seismic technique known as receiver function analysis to image the rocks below
the Sierra Nevada. The scientists found that in the central region of the
mountain range, Earth’s crust is currently peeling away from the bottom in the
process of delamination, or lithospheric foundering, with the lowest layers
melting deeper into the mantle.
Lithospheric foundering has
been studied in several places, including under the Andean plateau and under
Tibet. The process has been associated with batholiths – igneous rock
intrusions, usually granitic, and found near mountain fold belts. Knowledge of
lithospheric foundering can offer insights into the formation of continents.
There are indications of lithospheric foundering on Venus, where there is no
plate tectonics. Below is a map of faults and lithospheric structures under
Tibet, and below that is a similar map under the Central Andes.
“Lithospheric foundering is the process of the denser
materials being pulled to the bottom, while the less dense material emerges at
the top, resulting in land creation. “It’s dumping some of this denser stuff
into this gooey, solid mantle layer underneath and sort of basically detaching
it so it stops pulling on the less dense stuff above,” she {Kilb} explained.”
Under Sierra Nevada, they found a
distinct layer about 40 to 70 kilometers (25 to 43 miles) deep with
characteristics different from those of the rock around it. This is the layer
being peeled off.
There is an ongoing debate
about whether the mantle anomaly identified under the Sierra Nevada is due to
lithospheric foundering or subduction. There is scant evidence of lithospheric
foundering due to the difficulty of imaging at great depths. Thus, the new
research may offer some rare evidence. Graphics from the paper are below.
References:
Scientists
stumble across rare evidence that Earth is peeling underneath the Sierra Nevada.
Taylor Nicioli, CNN. April 18, 2025. Earth
is peeling underneath the Sierra Nevada, rare evidence shows | CNN
Earth's
crust is peeling away under California. Stephanie Pappas. Live Science.
February 1, 2025. Earth's
crust is peeling away under California | Live Science
Lithospheric
Foundering in Progress Imaged Under an Extinct Continental Arc. Vera
Schulte-Pelkum and Deborah Kilb. Geophysical Research Letters. Volume51, Issue 24.
December 13, 2024. Lithospheric
Foundering in Progress Imaged Under an Extinct Continental Arc - Schulte‐Pelkum
- 2024 - Geophysical Research Letters - Wiley Online Library
Crustal
bobbing in response to lithospheric foundering recorded by detrital proxy
records from the central Andean Plateau. B. Carrapa; G. Jepson; P.G. DeCelles;
S.W.M. George; M. Ducea; C. Campbell; R.R. Dawson (née Canavan). Geology (2025)
53 (1): 29–33. Crustal
bobbing in response to lithospheric foundering recorded by detrital proxy
records from the central Andean Plateau | Geology | GeoScienceWorld
Lithospheric
foundering and underthrusting imaged beneath Tibet. Min Chen, Fenglin Niu,
Jeroen Tromp, Adrian Lenardic, Cin-Ty A. Lee, Wenrong Cao & Julia Ribeiro. Nature
Communications volume 8, Article number: 15659 (2017). Lithospheric foundering and
underthrusting imaged beneath Tibet | Nature Communications
Delamination
(geology). Wikipedia. Delamination
(geology) - Wikipedia
Plateau
Formation Controlled by Lithospheric Foundering Under a Weak Crust. M.
McMillan, L. M. Schoenbohm, A. R. Tye. Geophysical Research Letters. Volume 50,
Issue16. August 22, 2023. Plateau
Formation Controlled by Lithospheric Foundering Under a Weak Crust - McMillan -
2023 - Geophysical Research Letters - Wiley Online Library
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