Plate Tectonics

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The Earth's lithosphere is broken up into chunks called plates with densities around 3. Oceanic plates are made of basalts (cooled volcanic rock made of silicon, oxygen, iron, aluminum, & magnesium). Oceanic crust is only about 6 kilometers thick. The continental plates are made of another volcanic type of silicates called granite. Continental crust is much thicker than oceanic crust---up to 35 kilometers thick. Continental plates are less dense than the oceanic plates. The mantle convection causes the crustal plates to slide next to or under each other, collide against each other, or separate from one another in a process called plate tectonics. Plate tectonics is the scientific theory that describes this process and how it explains the Earth's surface geology. The Earth is the only planet among the terrestrial planets that has this tectonic activity. This is because plate tectonics probably requires liquid water to solidify the oceanic plates at the midocean ridges where seafloor spreading is happening (see below) and more importantly, the liquid water lubricates the aesthenosphere and softens the lithosphere enough so that the plates can slide past or under one another. Venus has enough interior heat to have convection in its mantle like the Earth, but through processes described in another section, Venus lost its water, so its plates are poorly lubricated at best.

Plate Tectonics Theory Evidence

Plate tectonics is a relatively recent theory having been proposed in the late 1960s and finally being verified enough so that it could be put in the introductory geology textbooks in the 1980s (remember all of the peer review, error-correction process that happens before something is fit to print in a textbook). What finally made scientists accept the theory? Today we can easily measure plate motion using GPS sensors on either side of plates. As in any robust scientific theory there are multiple lines of evidence supporting the theory. For plate tectonics, the evidence is continental motion, seafloor spreading, earthquake and volcano locations, and the difference between the seafloor crust and continental crust. I will give just a brief outline of the evidence for plate tectonics here. See the nice, detailed presentation from the USGS's Dynamic Earth online text.

Plate Tectonics Process

The figure below shows the boundaries of the major plates on top of a map of the Earth. The arrows show the direction of the plates with respect to each other. The white areas are elevations greater than 2400 meters (7900 feet) above sea level. This figure is an adaption of a map in the "Plate Tectonic Movement Visualizations" website of the Science Education Resource Center at Carleton College and the plate motion data from This Dynamic Earth of the USGS. Select the figure to bring up an enlarged version of it.

plate boundaries of the Earth

Places where warm rock from the asthenosphere rises along weak points in the lithosphere can push apart the lithosphere on both sides (see the figure below). These places are at the midocean ridges (such as the Mid-Atlantic Ridge that bisects the Atlantic Ocean) and continental rift zones (such as the East Africa Rift Zone). Sea-floor spreading caused the Atlantic Ocean to grow from a thin sliver 100 to 200 million years ago to its present size and now continues at a rate of about 25 kilometers per million years.

separating plates create midocean ridges and continental rift zones

This pushing apart of some plates from each other means that others will collide. The oceanic lithosphere is cooled by contact with the ocean water. When oceanic crust runs into oceanic crust or into continental crust, the denser lithosphere material slides under the less dense lithosphere material, eventually melting in the deepest layers of the mantle. The region where the lithosphere pieces contact each other is called a subduction zone and a trench is formed there. At the subduction zone, the right combination of temperature, pressure and rock composition can create small pockets or fissures of molten rock in the solid asthenosphere that then rise up through cracks in the crust to create a range of volcanoes (see the figure below). In another section you will see that this has a profound effect on regulating the climate of the Earth.

When two continental pieces bump into each other, they are too light relative to the asthenosphere and too thick for one to be forced under the other. The plates are pushed together and buckle to form a mountain range. It also possible for two plates to slide past each other at what is called a transform fault such as the San Andreas Fault in California and the Anatolian Fault in Turkey.

San Andreas + Garlock faults in California

Examples of ocean-continental plate subduction include the Juan de Fuca plate off the coast of northwestern United States subducting under the North American continental plate to create the Cascade volcano range, the Nazca plate subducting under the western edge of the South American plate to create the Andes range of volcanic mountains. An example of the ocean-ocean plate subduction are the chains of islands on the Asia side of the Pacific: the Aleutians, Japan, Philippines, Indonesia, and Marianas. An example of continent-continent plate collision is the Indian plate running into the Eurasian plate to create the Himalayas.

A lot of information and videos about Earth's plate tectonics are available on the EarthScope website. Students and teachers should also check out the IRIS Earth Science animations website for many high-quality and detailed animations of the plate tectonic activity occuring around the globe.

Conclusions

To end the Planet Interiors section, here is a summary of the terrestrial planet surface shaping agents at work today.
Surface Shaper Agent Mercury Venus Earth Moon Mars
Impact Cratering Yes Minor Minor Yes Yes
Volcanism (needs internal heat) No (only long ago) Yes Yes No (only long ago) No (only in the past)
Tectonics (needs internal heat) No (only long ago) Yes Yes No No (only in the past)
Erosion No (no liquid or atmosphere) No (no surface winds) Yes (ice, water, air) No (no liquid or atmosphere) Yes (air today + water in past)

Looking at the table, we can draw some conclusions as to what planet properties will determine the type of planet surfacing that can occur. Impact cratering can occur on any object with a solid surface at any time. If a planet has an atmosphere and is still geologically active, then the effects of impact cratering will be erased. Volcanism and Tectonics require the planet to be of sufficient size to still have heat in its interior. Erosion requires an atmosphere with winds to work efficiently. Even better is if liquid can be present to add to the weathering by the atmosphere. Erosion works best on Earth. Earth is of sufficient size to hang on to its atmosphere (unlike the Moon). Earth is at a good distance from the Sun so it is not too hot for its atmosphere to either evaporate away or become excessively thick that winds will not blow on the surface (as is the situation with Venus). Also, its good distance from the Sun enables the surface temperatures to be warm enough for liquid water to flow (unlike Mars) and so its atmosphere does not freeze out on its surface as happens with Mars. Earth's rotation is fast for its size (unlike Venus), so it can create complicated air circulation (wind) patterns as well as ocean currents. Also, rapid rotation enables the creation of the magnetic field shield to protect a planet's atmosphere from the solar wind.

Vocabulary

erosion impact cratering plate tectonics
tectonics volcanism  

Review Questions

  1. Why are almost all impact craters round?
  2. How can you use the number of craters to determine the age of a planet's or moon's surface?
  3. The lunar highlands have about ten times more craters on a given area than do the maria. Does this mean that the highlands are ten times older? Explain your reasoning.
  4. What determines if volcanism will make a steep-sided mountain or something with a gentler slope?
  5. How do shield volcanoes compare in size to stratovolcanoes in diameter and height?
  6. How do volcanic eruptions affect a planet's atmosphere?
  7. What does volcanism require as far as interior conditions?
  8. How does erosion change the surface of a planet (or moon)?
  9. What is the difference of a valley carved by glaciers vs. one carved by flowing water?
  10. Besides wearing away geological features, what does the process of erosion do?
  11. How is tectonics different than plate tectonics?
  12. What does tectonics require as far as interior conditions?
  13. How does the plate tectonics theory explain such things as the widening of the Atlantic Ocean, the Andes of South America and the Cascades of the northwestern U.S, and the high mountain ranges such as the Himalayas and the Rocky Mountains?
  14. What is the evidence for plate tectonics?
  15. What properties of a planet will determine what type of planet shaping can occur on it?
  16. What type of planet shaping occurs on Mercury, on Venus, on Mars, and on the Earth and the Moon?

Earthquake Resources

I teach in a college located in the southern end of the San Joaquin Valley of California. We are very aware that we live in a place where a serious earthquake can occur and every October the college participates in the Great ShakeOut. Below is a list of some resources for preparing for and recovering from earthquakes. Thanks to Astronomy Notes reader Katie Cook for locating several of these resources.

  1. Putting Down Roots in Earthquake Country put out by the Earthquake Country Alliance.
  2. FEMA's Earthquake Publications geared to various types of audiences. FEMA Earthquake Safety at School website. Other FEMA earthquake website geared to other audiences can be accessed from the top FEMA Earthquake page.
  3. The Great ShakeOut drills website.
  4. Central United States Earthquake Consortium's Drop, Cover, & Hold webpage is helpful for what to do DURING an earthquake. Also, follow the links to how to prepare for an earthquake and what to do after an earthquake.
  5. The HomeAdvisor Earthquake Recovery Resource Guide.
  6. SafeSoundFamily has a nice description of earthquake preparation and surviving that draws upon the the material from the websites listed above on its "Keeping Your Family Safe During an Earthquake" webpage.

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last updated: October 5, 2016

Is this page a copy of Strobel's Astronomy Notes?

Author of original content: Nick Strobel