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White (1952) investigated the flow direction of a depositing stream from the Houghton conglomerate with respect to the initial imbrication of pebbles.
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Note that the stream across the debris flow deposit (Stream L) is colored gray, even 9 days after the eruption.
The presence of a delta represents the continuing ability of rivers to deposit stream-borne sediments more rapidly than they can be removed by waves and ocean currents.
The mineral zircon, which is generally found in alluvial deposits in stream beds, ocean beaches, or old lake beds, is the only commercial source of zirconium.
Other fossil placers (i.e., deposits whose stream waters have long disappeared) have been discovered at Serra de Jacobina in Brazil (gold) and Blind River, Ontario, Canada (uranium), but nowhere has a deposit been found equal to Witwatersrand.
The aim of the present study was to evaluate the effect of volcanic ash deposits on stream ecosystems four years after the eruption, comparing biofilm stoichiometry, alkaline phosphatase activity, and primary producer's assemblage in streams which were severely affected by the volcano with unaffected streams.
We know that these sediments were deposited by streams and rivers.
These sediments were deposited by streams, and the shoreline migrated westward.
About 11 million years ago, sand and pebbles were deposited by streams.
The development of debris tongue deposits divert streams and increase thermoerosion to initiate adjacent slumps.
The rich soils of the Great Plains, for example, are largely derived from the silt deposited by streams of glacial meltwater.
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