• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/9

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

9 Cards in this Set

  • Front
  • Back
Deltas
form where rivers enter lakes, seas, oceans.
-- supple seds. more rapidly that can be redistributed
alluvial deltas--3 main influences on depositional geometry in terms of high energy
1. fluvial dominated
2. Tide dominated
3. wave dominated
Fluvial Dominate
dominated by type of flow (mixing of water)
--homopychal (same density)
--similar densities--rapid mixing and abrupt depostion
Progradation
--building outwards into basin
--synonymous with marine regression
hyperpycnal
high sed load river water entering
--under flows-->turbidy currents
---commonly on steep sided basins
hypopucnal
less dense--marine deltas/ Fresh river water enters marine water
--large active de;ta fronts w/ foresets dipping
Tide dominate deltas
large tidal range; minimal wave power; distributaries are tidal channels that show bi-directional flow and rapid migration distributary mouth ars are re-worked into tidal bars-->example: ganges-Brahmaputra delta-tidal range = 4m
wave dominated deltas
large wave power; distributary mouth bars are reworked by longshore currents and wave processes
-->smooth delta front with wave-buil beaches, barrier island and spits; example: sa francio delta, Brazil range = 2 m
Barrier islands form by (2)
split segmentation

drwoning of shoreline during sea level rise