hawaiian island geology

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Hawaiian Island Geology. Over 100 volcanoes in a volcanic island arc system. Meiji (3000 m deep). Big Island. Hawaiian Islands. Niihau. Kauai. Oahu. Molokai. Lanai. Maui. Hawaii. Bathymetric Profile of Hawaiian Emperor Chain. - PowerPoint PPT Presentation

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Page 1: Hawaiian Island Geology
Page 2: Hawaiian Island Geology

Over 100 volcanoes in a volcanic island arc system

Big Island

Meiji(3000 m deep)

Page 3: Hawaiian Island Geology

Hawaiian IslandsHawaiian Islands

Hawaii

Oahu

Kauai

Lanai Maui

Molokai

Niihau

Page 4: Hawaiian Island Geology

Bathymetric Profile of Hawaiian Emperor Chain

Page 5: Hawaiian Island Geology

Hawaii

(youngest)MauiOahuKauai(oldest)Pacific Plate

J. Tuzo Wilson (1963), a Canadian geophysicist ,came up the "hotspot" theory. volcanoes of the Hawaiian

chain should get progressively older and become more eroded the farther they travel beyond the hotspot.

Page 6: Hawaiian Island Geology

Age of Hawaiian Islands

Page 7: Hawaiian Island Geology

Much of the Hawaiian island arc is underwater and extends toward Midway

Moves in a northwesterly direction

Page 8: Hawaiian Island Geology

WE’VE GOT HOT SPOTS ALL OVER THE PLACEOther examples of hot spots include:

Cape Verde (off the coast of Senegal), Galapagos Islands (off the coast of Equator), Society Islands (French Polynesia), Tristan da Cunha (southern Atlantic), Yellowstone, Ethiopia Plateau, Lord How (near Sydney), Iceland, and many more.

Page 9: Hawaiian Island Geology

Older islands erode and subside

Page 10: Hawaiian Island Geology

Aging islands and coral:• Drilling and removing core sample• C14 dating

Page 11: Hawaiian Island Geology
Page 12: Hawaiian Island Geology
Page 13: Hawaiian Island Geology

Barrier Reef- separated from land by a lagoon

Fringing Reef- boarders coastline closely

Island subsides

Atoll- coral ring with central lagoon

lagoon is a shallow area with a sandy floor, patch reefs, and patches of seagrass

Darwin’s Theory of Coral Atoll Formation: Subsidence Theory

Page 14: Hawaiian Island Geology

Fringing Reef- Tahiti

Page 15: Hawaiian Island Geology

Fringing Reef

Reef Flat

Reef Front

Shoreline

Page 16: Hawaiian Island Geology

Barrier Reef Profile

reefslope

reeffront

outerreef flatlagoonpatch

reef

islandinnerreef flat

Page 17: Hawaiian Island Geology

Australia- Great Barrier Reef

Page 18: Hawaiian Island Geology

                                                            

Kaneohe Bay

Barrier Reef

Fringing Reef Patch Reef

Page 19: Hawaiian Island Geology

Reef Flat of a barrier reefReef Flat of a Barrier Reef

Reef Flat

Coral Island(Cay or Motu)

Reef Front

Lagoon

Open Ocean

Page 20: Hawaiian Island Geology

Cross Section of an Atoll

Page 21: Hawaiian Island Geology

Atoll

Belize- Blue Hole

Page 22: Hawaiian Island Geology

Kure Atoll (28° 25' N - 178° 20' W)Midway Atoll

Pearl & Hermes Atoll

Page 23: Hawaiian Island Geology

Inquiry

1. The oldest seamount in the Hawaiian Emperor Chain is _____?

2. What direction are our islands moving?

3. What seamount will be the newest Hawaiian Island?

4. Key features of a barrier reef are_____?

5. When an atoll subsides it often forms a _____?