Barrier Islands Flashcards
What are in-between barrier islands?
Tidal Inlets (have bidirectional flow)
What are the major components that drive the morphology of barrier islands?
- Wave (more so)
- Tides
Draw and describe a wave-dominated barrier island system.
- Strong longshore currents
- Long skinny barrier islands.
- Influence of tides through the inlet will be much less (likely not going to have an ebb tidal delta but may have a small flood tidal delta)
example – outerbanks
Draw and describe a mixed energy barrier island system
- Barriers tend to be short and stubby
- A lot of tidal inlets
- Likely to have larger ebb tidal deltas
- Example : VA ESVA
What are the three main ways barrier islands form?
- Offshore Shole
- Beach that formed on the mainland
- Spit building
Barrier Island Formation: Draw offshore shole
Barrier Island Formation: Mainland Detachment
- Beach that formed on the mainland.
- Sea level rises and so it is no longer attached to shore as a beach
Barrier Island Formation: Spit Accretion
Draw and describe longshore transport
- When a wave crashes on a beach, it does just come parallel to shore. It does crash parallel to the shore.
- As the waves crash onto the beach at an angle, gravity then pulls it back out.
- This repeats.
The Bruun Rule
Associated with barrier island retreat (transgression) and the rate.
How far does the shore retreat in 100 yrs?
B=3m / S= 5 mm/yr / L= 4km /h=7m
L = 4000 m
4000m/3m+7m = 4000/10 = 400x0.0005x100 = 200m in 100 years (2m/yr)
Describe overwash
storm waves that crash over an island and deposit sand from the shoreface to the back-barrier
What are the three processes that barrier island systems move?
- Transgressive
- Aggradational
- Progradational
Draw and describe a core sample of a transgressive migration of a barrier island system
Transgressive – generally when sea level is rising and we experience large storms.
Draw and describe a core sample of a aggradational barrier island system
Would not have the same stratigraphy as transgressive
Aggradational – the island is accreting vertically (a lot of sediment supply and sea level is stable)