Wave Erosion and Marine Geology

Steven Dutch, Professor Emeritus, Natural and Applied Sciences, University of Wisconsin - Green Bay

Marine Geology

Sea Water

Element Weight %: 1%=10 gm/liter
Cl 1.9
Na 1.05
Mg 0.135
S 0.0885
Ca 0.040
K 0.038
Br 0.0065
C 0.0028
Sr 0.00081
B 0.00096
Si 0.00030
F 0.00013


Storm Waves: Galveston, Texas, 1900

The worst disaster in U.S. history took place September 8, 1900 when a hurricane struck Galveston, Texas, killing an estimated 6,000-8,000 people

galveston 1900 Storm waves flooded the Gulf shore of Galveston almost 16 feet deep, and surged into Galveston Bay, flooding the "sheltered" shore ten feet deep. The waves demolished everything, pushing it inland until the debris wall was thick enough to resist the waves.
galveston 1900 After the disaster, a seawall was built along the Gulf shore, and virtually the entire city was raised anywhere from six inches to 17 feet. A canal was dug behind the seawall. Dredges excavated sand from the bay, sailed in along the canal and pumped sand into low-lying areas. Buildings were raised on pilings and people got around on board walks looking, as one author put it, "like something from Doctor Seuss." It typically took several weeks to fill any given area.
GAlveston 1900 The design of the seawall was unusually well thought-out. Instead of attempting to resist waves by brute force, the seawall has a concave face to direct waves upward. A long gentle slope behind the wall allows for the inevitable wave overflow to dissipate itself and run back. The seawall has resisted several storms that survivors thought were actually worse than the 1900 storm.

In the long run, nothing is as futile as trying to resist shoreline change. Change can be resisted for a while, but when the water wants something badly enough, it will come in and take it.

Freak Waves

Long rumored to exist by seamen, freak waves are a reality. They occur when waves of several frequencies superimpose. Typically, a ship encounters a steep trough often likened to a "hole in the ocean" followed by a steep crest. These events can occur quickly enough to sink a ship before any distress call can be sent. During World War II, a freak wave struck the ocean liner Queen Mary in the North Atlantic, rolling it on its side to within a hair of capsizing. Had it capsized, it would have been by far the worst marine disaster ever. There were 15,000 soldiers aboard bound for Europe - it would have been ten times worse than the Titanic disaster. Computer modeling indicates that freak waves up to almost 200 feet high can occur in the Gulf of Alaska.

Freak Waves Here, waves of three different frequencies combine to produce very high crests and very deep troughs (bottom)

What was the worst marine disaster ever?

Marine Erosion

Longshore and Beach Drift

Most Beach Sand Is Created by Weathering and Carried to Coasts by Rivers

Beach Sand Moves along the Coast by Longshore and Beach Drift

Longshore Drift

Types of Coast

Degree of Modification

Primary - Not Modified Much by Wave Action
Secondary - Highly Modified by Wave Action


Emergent - Land Rises or Water Level Falls
Submergent - Land Sinks or Water Level Rises

Dominant Process


Secondary Coasts Are Modified by Marine Erosion or Deposition

secondary coasts

End state in both situations is a regular coastline with gentle curves and cusps.


Once the sea cliffs retreat a few hundred meters, wave energy is largely dissipated crossing the wave-cut terrace. Meanwhile, the cliffs become higher, meaning more material to move. Erosion rate becomes very slow.


Primary Coastlines Are Very Common

Sea Level Has Risen 100-200m (300-600 Ft) since the Pleistocene

submerged river valleys Submerged river systems can still be recognized on the sea floor of Indonesia. This shallow sea bottom was dry land during the Pleistocene.

Other Ways Primary Coasts Can Form

Cape Hatteras The North Carolina coast exhibits both primary and secondary coastlines. The inner shore is a series of estuaries that resulted from flooding of river valleys during the post-Pleistocene rise in sea level. It is a primary coastline. The Outer Banks, the narrow offshore islands, are a secondary coastline created by wave action.

Reefs Are a Major Type of Coast in Tropical Areas

Many Volcanic Islands in the Pacific have sunk, producing a sequence of reef types


Reefs Also Form along the Edges of Large Islands and Continents

These Are Barrier Reefs

Deep Ocean Phenomena

Turbidity Flows

turbidity flow A powerful earthquake off Newfoundland in 1929 caused a submarine landslide on the edge of the continental shelf. Submarine cables in the slump area broke immediately but cables downslope broke up to several hours later. Apparently a dense current of suspended sediment traveled several hundred kilometers across the sea floor.

This disaster also generated one of the most significant Atlantic tsunamis. Damage occurred in Newfoundland and Nova Scotia and the wave showed up on tide gauges as far away as the West Indies and Portugal. 27 people died in Newfoundland and one other person died several years later of injuries.

The Worst Marine Disaster Ever

The Titanic wasn't even the worst "natural" marine disaster ever, that is, without the ship being deliberately sunk (few marine disasters are wholly natural). A collision between the Philippine ferry Dona Paz and the tanker Victor killed 4,341 on December 20, 1987. The worst sinking ever took place in the closing months of World War II. A German ship, the Wilhelm Gustloff, sailed from Danzig filled to overflowing with German refugees fleeing the advancing Russians. It was torpedoed by a Russian submarine in the Baltic. About 900 survivors were rescued and an estimated 8,000-9,000 people died. Less than two weeks later the same Soviet sub sank another vessel in which 3,000-4,000 people died.

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Created 21 May 1997, Last Update 4 May 2000