GEOL TEST 2
The Coast: Beaches and Shoreline Processes
Coastal hazards: Coastal Erosion and Hurricanes
why study coastal processes
75% of US population lives in coastal states
50 % lives within 100 miles of coastline
Hurricanes
Highly dynamic environment
Coastal problems will increase with population
Global warming
Coast- Area of contact between land and sea - Extend inland until meets a different geographic setting
Shoreline- Precise boundary where water meets adjacent dry land
East Coast
Passive Margin Coastlines
Barrier islands and maybe rocky coastlines
West Coast
Active Margin Coastlines
Sea cliffs and Rocky coastlines
Forces modifying coasts
Two major processes (forces) shape coastline
Waves
Waves do erosion (move sediment)
Tides
Twice daily rise and fall of sea level
Changes where waves act
Wave formation
Wind blowing over water
Size of waves depend on
Wind speed
faster=bigger waves
Wind duration
longer=bigger waves
Distance wind blows (fetch)
further=bigger waves
Wave Characteristics
Length (L)
Distance between crests or between troughs
Height (H)
Vertical distance between crest and trough
Period (T)
Time for successive waves to pass a fixed point
Types of Waves
Waves of Oscillation (unmoving; further from shore)
Waves of Translation (moving; closer to shore)

Wave Movement Near Shore
Wave refraction
waves bend as they approach the shore
Longshore currents
Currents parallel to the beach within the surf zone
They are the most important to modifying coastlines
Longshore (littoral) drift
Sediment carried by swash and backwash along the beach
Tides
Another force that occurs along every shoreline
They are the twice daily rise and fall of the sea, caused by the gravitational attraction of the Moon, and to a lesser degree, the sun
High Water- a water level maximum (high tide)
Low Water- a water level minimum (low tide)
Tidal Range- the difference between high and low tide
Spring Tide- full moon and new moon (14.77 days)
Neap Tide- 1st quarter and 3rd quarter (14.77 days)
The Bay of Fundy: Site of the worlds largest tidal range
Tidal energy is focused by shape and shallowness of bay
Maximum spring tidal range in Minas Basin
Waves and Tides
Waves do the erosion
Tides change level of beach that waves act on
Erosion takes place when waves interact with the bottom
Factors that impact coastlines
Tectonic setting
Materials present at the shore
Energy of water striking the coast
Coastal Processes
Rifted (Passive continental margins tend to be dominated by depositional features
Active continental margins tend to be dominated by erosional features
Erosional and depositional landforms result of the action of ocean waves
Erosional
Sea cliffs
Sea stacks
Sea arches
sea caves
Depositional
Beaches
Spit
Barrier Island
Erosional coasts
Wave energy is focused on headlands: prominent cliffs that jut out into deep water
attack the sides of headlands and form sea caves, sea arches, and sea stacks.
Depositional Coasts
Occurs when amount of sediment exceeds wave/current ability to transport it
Beaches - Relatively narrow strips of sand, pebbles, or cobbles deposited along a shoreline
90% of beach sediment comes from streams that drain to coast distributed by long shore currents
wave action erodes, deposits, and moves sediment
The beach is different every day
<aside> đź’ˇ Have enough of an understanding of the beach profile to recreate it
</aside>
Barrier Islands - Long, low, narrow islands parallel to the coastline made of sand that flank main shoreline and separate bays from open ocean. Created by long shore currents
Unstable environments
Easily washed over due to low relief
Sand migrates constantly with the wind
Constantly retreating landward with time
Spit - Narrow strip of sand that grows across the mouth of bay due to long shore current (hooks are hook shaped)
Similar to barrier island but it’s connected to mainland
Settlement in the Dynamic Environment
Wave - Continues eroding and modifying
Stability requires protections from waves
“Controlling” Coastal erosion
Structural approaches
Seawalls
Groins
Jetties
Non-structural approaches
Beach nourishment
Land use planning
Beach erosion factors
Supply e.g. Appalachian weathering
Erosion
Hurricanes
Climate Change
Landward push of a beach
Human interference
Controlling Sand supply
Enhance wave action
Human Interference Dam
Impacts
Coastal zone short of fresh water
Cutoff sand supply
erosion > deposition
Reduces protection
Groins - walls built along beach extending into water
block sand movement along beach
cause sand to accumulate on up-drift side of groin
Breakwater - A hard, rocky structure built parallel to shore and attached to the sea floor
A few feet above sea level
Designed to break waves and make quiet water behind for safe harbor
intercept waves and protect boat moorings
provide safe harbors
radically change shoreline creating sediment deposits
Jetties - Designed to stabilize channel
Protect channel from large waves and sand deposition
Constructed in pairs at mouth of a river or inlet
Beach Re-nourishment - Adding sand to beach
mimics nature but has to be redone
Aesthetically preferable
Controversial
expensive and temporary fix
Hazards in Coastal areas
Sea level rise
hurricanes
Tsunamis
Sea Level Rise
Sea level was 120 meters lower during the last ice age
About 18,000 years ago, sea level began to rise as the glacial ice melted
In NYC
Sea level has risen 40 cm since 1850
Global warming is predicted to increase the rate of sea level rise
Hurricanes
Tropical cyclones (hurricanes, typhoons, etc.)
Intense storms that form in tropical waters when ocean is warmest
What does a hurricane need?

They uplift water collum
High winds
Winds up to 200 mph damage buildings
Heavy rainfall
causes floods in area where storm passes over; also downstream
Most damaging if it coincides with high tide