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5.15: Intraplate Activity

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What would you think if you heard that all geological activity does NOT take place at plate boundaries?

These photos of fabulous geological activity are going to rock your world. Why? After all of these lessons in which you learned that volcanoes and earthquakes are located around plate boundaries, this last lesson in "Concept Plate Tectonics" doesn’t quite fit. These volcanoes are located away from plate boundaries. Two such locations are Hawaii and Yellowstone. Yellowstone is in the western U.S. and Hawaii is in the central Pacific.

Intraplate Activity

A small amount of geologic activity, known as intraplate activity , does not take place at plate boundaries but within a plate instead. Mantle plumes are pipes of hot rock that rise through the mantle. The release of pressure causes melting near the surface to form a hotspot . Eruptions at the hotspot create a volcano.

Hotspot volcanoes are found in a line ( Figure below ). Can you figure out why? Hint : The youngest volcano sits above the hotspot and volcanoes become older with distance from the hotspot.

An animation of the creation of a hotspot chain is seen here: http://earthguide.ucsd.edu/eoc/teachers/t_tectonics/p_hawaii.html .

Intraplate Activity in the Oceans

The first photo above is of a volcanic eruption in Hawaii. Hawaii is not in western North America, but is in the central Pacific ocean, near the middle of the Pacific Plate.

The Hawaiian Islands are a beautiful example of a hotspot chain in the Pacific Ocean. Kilauea volcano lies above the Hawaiian hotspot. Mauna Loa volcano is older than Kilauea and is still erupting, but at a slower rate. The islands get progressively older to the northwest because they are further from the hotspot. This is because the Pacific Plate is moving toward the northwest over the hotspot. Loihi, the youngest volcano, is still below the sea surface.

The Hawaiian Islands have formed from volcanic eruptions above the Hawaii hotspot.

Since many hotspots are stationary in the mantle, geologists can use some hotspot chains to tell the direction and the speed a plate is moving ( Figure below ). The Hawaiian chain continues into the Emperor Seamounts. The bend in the chain was caused by a change in the direction of the Pacific Plate 43 million years ago. Using the age and distance of the bend, geologists can figure out the speed of the Pacific Plate over the hotspot.

The Hawaiian-Emperor chain can be traced from Hawaii in the central Pacific north of the equator into the Aleutian trench, where the oldest of the volcanoes is being subducted. It looks like a skewed "L".

Intraplate Activity on the Continents

The second photo in the introduction is of a geyser at Yellowstone National Park in Wyoming. Yellowstone is in the western U.S. but is inland from the plate boundaries offshore.

Hotspot magmas rarely penetrate through thick continental crust, so hotspot activity on continents is rare. One exception is the Yellowstone hotspot ( Figure below ). Volcanic activity above the Yellowstone hotspot on can be traced from 15 million years ago to its present location on the North American Plate.

The ages of volcanic activity attributed to the Yellowstone hotspot.

Summary

  • Not all geological activity is found at plate boundaries. Some volcanic activity, with accompanying earthquakes, is located within a plate. This is called intraplate activity.
  • Intraplate activity occurs above mantle plumes that cause melting at a hotspot.
  • Hotspots erupt mostly on oceanic crust. Hawaii is an example. A few hotspots, like Yellowstone, erupt on continental crust. The difference is due to the thickness of the crust.
  • Hotspots can be used to tell the speed and direction that a plate is moving, since the hotspots are stationary within the mantle.

Practice

Use these resources to answer the questions that follow.

1. Where is Iceland located?

2. What causes the mantle to be forced up?

3. What does a constructive plate boundary form?

4. Where are most volcanoes found?

5. What are hotspots?

6. How do hotspots form volcanoes?

7. Where can a hotspot be seen today?

http://www.nps.gov/yell/naturescience/tracking_hotspot.htm

8. What direction is the North American Plate moving? How fast is it moving?

9. When did the McDermmit Volcanic Field erupt?

10. What was the most recent eruption of this hotspot? Where?

Review

1. What is a mantle plume and how is it related to a hotspot?

2. How do scientists use hotspot volcanism to tell the direction and speed of a plate?

3. Why are hotspot volcanoes much more common in the oceans than on continents?  

Vocabulary

hotspot

hotspot

A plume of hot material that rises through the mantle and can cause volcanoes.
intraplate activity

intraplate activity

Geologic activity that takes place away from plate boundaries.

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Difficulty Level:

At Grade

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Date Created:

Feb 24, 2012

Last Modified:

Aug 25, 2014
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\n

\n Introduction\n

\n

\n \"\"\n

\n

\n But it all seems so solid!\n

\n

\n Besides flying around on a ball of rock — orbiting a giant ball of burning gas and spinning in circles about an axis — the ground you sit on is moving! Just as Copernicus, Kepler, and Galileo had trouble convincing people that Earth orbited the Sun when it clearly seemed that Earth was at the center of the universe and everything moved around it, early adherents to the idea that continents could move had to fight against, well, common sense. Over the past century the idea that continents could move was proposed, studied, abandoned, and finally accepted.\n

\n

\n We’ll start this concept with a field trip back in time to the scientists that developed plate tectonics theory. First, we’ll visit Wegener, and then we’ll get aboard ship to learn about seafloor spreading. Finally, we’ll travel around western North America to see the features created by the different types of plate boundaries there.\n

\n
\n
\n \n
\n
\n

\n Summary\n

\n

\n In the early 20th century, Alfred Wegener was the first persistent scientist to propose the idea that continents move around on Earth’s surface. The meteorologist amassed a tremendous amount of evidence but could not think of a mechanism that others would accept to explain how solid continents could plow through ocean basins. Wegener’s idea was abandoned. His continental drift idea was resurrected after World War II when scientists started to put together data about the seafloor. The astonishing features of the seafloor, the strange pattern of rock ages across the seafloor, and the history of the magnetic north pole on land, gave scientists in the early 1960s a great deal to mull over. From this work Harold Hess propose seafloor spreading as a mechanism for drifting continents. The resulting theory of plate tectonics is the explanation of what happens as plates of Earth’s lithosphere interact at different types of plate boundaries.\n

\n
\n \n\n", "chapterSummary": "

\n Summary\n

\n

\n In the early 20th century, Alfred Wegener was the first persistent scientist to propose the idea that continents move around on Earth’s surface. The meteorologist amassed a tremendous amount of evidence but could not think of a mechanism that others would accept to explain how solid continents could plow through ocean basins. Wegener’s idea was abandoned. His continental drift idea was resurrected after World War II when scientists started to put together data about the seafloor. The astonishing features of the seafloor, the strange pattern of rock ages across the seafloor, and the history of the magnetic north pole on land, gave scientists in the early 1960s a great deal to mull over. From this work Harold Hess propose seafloor spreading as a mechanism for drifting continents. The resulting theory of plate tectonics is the explanation of what happens as plates of Earth’s lithosphere interact at different types of plate boundaries.\n

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\n Introduction\n

\n

\n \"\"\n

\n

\nBut it all seems so solid!\n

\n

\n Besides flying around on a ball of rock — orbiting a giant ball of burning gas and spinning in circles about an axis — the ground you sit on is moving! Just as Copernicus, Kepler, and Galileo had trouble convincing people that Earth orbited the Sun when it clearly seemed that Earth was at the center of the universe and everything moved around it, early adherents to the idea that continents could move had to fight against, well, common sense. Over the past century the idea that continents could move was proposed, studied, abandoned, and finally accepted.\n

\n

\n We’ll start this concept with a field trip back in time to the scientists that developed plate tectonics theory. First, we’ll visit Wegener, and then we’ll get aboard ship to learn about seafloor spreading. Finally, we’ll travel around western North America to see the features created by the different types of plate boundaries there.\n

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\n Front Matter\n

\n

\n Foreword\n

\n

\n The study of Earth Science is the study of the Earth. Earth Science Concepts presents Earth Science as a set of concepts, with each concept centered around a specific category, such as the Earth's crust or plate tectonics. Each concept is comprised of a series of lessons, with each lesson focusing on one specific topic. The complete Earth Science Concepts is comprised of over 320 lessons.\n

\n

\n Preface\n

\n

\n Dedication\n

\n

\n Chapters\n

\n

\n \"\"\n

\n
\n \n
\n

\n Back Matter\n

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\n Front Matter\n

\n

\n Foreword\n

\n

\n The study of Earth Science is the study of the Earth. Earth Science Concepts presents Earth Science as a set of concepts, with each concept centered around a specific category, such as the Earth's crust or plate tectonics. Each concept is comprised of a series of lessons, with each lesson focusing on one specific topic. The complete Earth Science Concepts is comprised of over 320 lessons.\n

\n

\n Preface\n

\n

\n Dedication\n

\n

\n Chapters\n

\n

\n \"\"\n

\n
\n \n
\n

\n Back Matter\n

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Original text