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  2. River delta - Wikipedia

    en.wikipedia.org/wiki/River_delta

    A river delta is so named because the shape of the Nile Delta approximates the triangular uppercase Greek letter delta.The triangular shape of the Nile Delta was known to audiences of classical Athenian drama; the tragedy Prometheus Bound by Aeschylus refers to it as the "triangular Nilotic land", though not as a "delta". [8]

  3. Mississippi River Delta - Wikipedia

    en.wikipedia.org/wiki/Mississippi_River_Delta

    The delta cycle refers to a dynamic process whereby the river deposits sediment at its outfall, growing a delta lobe, then eventually, seeking a shorter path to the sea, abandons its previous course and associated delta. After the river changes course and abandons the delta headland, the region experiences land loss due to the processes of ...

  4. Diploma in Teaching English to Speakers of Other Languages

    en.wikipedia.org/wiki/Diploma_in_Teaching...

    In 1988, Cambridge English Language Assessment (then known as the University of Cambridge Local Examinations Syndicate (UCLES)) reached an agreement with the RSA to take over its suite of teacher training courses and qualifications. UCLES integrated DTEFLA and DOTE to launch the Cambridge DELTA (Diploma of English Language Teaching to Adults). [6]

  5. Category:River deltas of the United States - Wikipedia

    en.wikipedia.org/wiki/Category:River_deltas_of...

    Sacramento–San Joaquin River Delta (4 C, 48 P) Pages in category "River deltas of the United States" The following 10 pages are in this category, out of 10 total.

  6. Category:River deltas by continent - Wikipedia

    en.wikipedia.org/wiki/Category:River_deltas_by...

    This page was last edited on 30 December 2016, at 19:35 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike License 4.0; additional terms may apply.

  7. Avulsion (river) - Wikipedia

    en.wikipedia.org/wiki/Avulsion_(river)

    An example of a deltaic lobe is the bird's-foot delta of the Mississippi River, pictured at right with its sediment plumes. As the deltaic lobe advances, the slope of the river channel becomes lower, as the river channel is longer but has the same change in elevation. As the slope of the river channel decreases, it becomes unstable for two reasons.

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