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These basins captured interior-bound sediment eroded from the mountains.
Clastic sediments eroded from this source were deposited in the Hazen Trough.
Sediment was eroded from the continents and deposited in adjacent seas.
Closed magnetic field lines are eroded from the dayside and added to the polar caps, increasing their diameter.
Ancient marine and lake basins were filled with a variety of sedimentary and volcanic debris eroded from primeval lands.
The Queenston Delta was produced as sediments that were eroded from a rising landmass in the present Appalachian Mountain region.
As material eroded from the Rockies millions of years ago, it was deposited in layers and cemented into sandstone.
Sediments eroded from a landmass and deposited in an adjacent sea change from coarse- to fine-grained with increasing depth of water and distance from shore.
This process cannot go on indefinitely, as geomagnetic field lines will be continuously eroded from the dayside unless they are replaced by an internal flow.
Foreland basins usually exist as subsurface features that have been filled with debris eroded from the advancing overthrust slice of crust.
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Rock debris enters fluvial systems either as fragments eroded from rocky channels or in dissolved form.
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CEO of Professional Science Editing for Scientists @ prosciediting.com