Different ways to measure Plate Motion?

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Discussion Overview

The discussion focuses on the differences between various methods of measuring plate motion, specifically comparing GPS data with magnetic anomalies, fracture zones, and hot spots. It explores theoretical and practical aspects of these measurement techniques.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested
  • Homework-related

Main Points Raised

  • Some participants seek clarification on the differences between GPS data and other methods like magnetic anomalies, fracture zones, and hot spots for analyzing plate motion.
  • One participant suggests that GPS can provide high accuracy and immediate results, while other methods may depend on extensive field research and time.
  • Another participant proposes that magnetic anomalies may not directly indicate plate motion but can reflect geological features related to plate boundaries.
  • Fracture zones are mentioned as regions indicating relative motion between plates, resulting from the offset of mid-ocean ridge segments.
  • Hot spots are discussed as stationary features on the Earth's surface that provide evidence of plate motion as plates move over them.
  • Some participants express uncertainty about the limitations of using magnetic anomalies and fracture zones compared to GPS technology.

Areas of Agreement / Disagreement

Participants express various viewpoints on the effectiveness and limitations of different measurement methods, indicating that multiple competing views remain without a clear consensus on the best approach.

Contextual Notes

Participants note that the effectiveness of each method may depend on specific geological contexts and the nature of the data being analyzed, highlighting the complexity of measuring plate motion.

Who May Find This Useful

This discussion may be useful for students and researchers interested in geophysics, geology, and the methodologies used in studying plate tectonics and motion.

RJLiberator
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Homework Statement



What's the difference in using GPS Data vs. using Magnetic anomalies, fracture zones, hot spots to analyze plate motion?

Homework Equations

The Attempt at a Solution



Seems like a question with a direct answer.
What's the difference between the two? I am struggling to find any notes or information on it. This is in reference to a report that went into detail about a GPS study of plate motions.
I need to know the difference between the two measuring tools to understand what's going on.

Any help?
Thank you.
 
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"GPS" stands for what?
 
Global Positioning System
 
How do you find your position with GPS?
 
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I'm not entirely sure, but do you use 3 different GPS satellites to find your position? "trilateration" and then using trilateration with distance = rate x time you can measure the location.

Am I on the right path there?
 
Yes, with GPS system you can determine the position and detect motion (assuming it is fast enough and the accuracy of the position detection is good enough).

What about other methods? In what way do they prove the motion?
 
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This is purely a guess from my knowledge: But I would imagine in using fracture zones, magnetic anomalies, and hot spots, they use seismic data or relevant plate motion data to analyze it?
 
Can you use the Hawaiian Islands to watch/indicate MOR (mid-ocean ridge) movement relative to Iceland?
 
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Hm..

I take it that your question is a hint towards a limitation.
I would think not unless you use GPS devices. Is this the limitation of the magnetic anomalies/fracture zones/hot spots that this question was alluding too?
 
  • #10
Or, a suggestion that GPS can be applied anywhere, whereas hotspots, fracture zones, magnetic anomalies, and other gross physical features of "plates" are limited in distribution.
 
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  • #11
I see.
That makes sense.
Since GPS is long range, it can be applied anywhere over the earth.
While the fracture zones, magnetic anomalies, and hotspots are data that is driven by location.
 
  • #12
Also note: GPS gives pretty high accuracy and works here and now. What about other methods?
 
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  • #13
Also note: GPS gives pretty high accuracy and works here and now. What about other methods?

I see. GPS gives high accuracy and near immediate results by definition of how the technology works.

The other method is dependent on massive field research, perhaps Earth rumblings (seismic activity? or hot spot activity), and so is dependent on time.
Whereas, we can say "ok, load up the GPS data," we cannot say "ok, make the Earth rumble."

Is that a way to understand it?
 
  • #14
RJLiberator said:
What's the difference in using GPS Data vs. using Magnetic anomalies, fracture zones, hot spots to analyze plate motion?
Based on my limited knowledge of geology and geologic mapping, a common technique for analyzing plate motion is placing sensors on either side of the plate, and measuring (via GPS) their relative change in position.

Magnetic anomolies don't necessarily indicate plate motion, as far as I know. They can occur when there are large masses of some ferrous material beneath the surface. They can also occur in "stripes" on either side of a mid-ocean spreading site that is the junction of two plates. New ocean seafloor that is created at the spreading site extends out from the spreading site in two directions. The stripes of opposite polarity magnetism that appear on either side of the spreading zone are thought to occur due to the periodic switching of the Earth's magnetic field, and can be used to give an idea of how fast the seafloor is moving on either side of the spreading zone.

Fracture zones (see https://en.wikipedia.org/wiki/Fracture_zone) result "from the action of offset mid-ocean ridge axis segments.are regions in the ocean where there are numerous faults." (Taken from the wiki article.) These fracture zones indicate motion of one plate relative to another.

Hot spots, such as the one currently below Hawaii island (the "big island") and others, such as the one that is believed to cause massive outpourings of lava in Washington state before moving east to produce the caldera at Yellowstone) provide evidence of plate motion. The hot spots are believed to be stationary on the Earth's surface, while the plates slide across it. In the Hawaiian islands, the Pacific Plate is theorized as having moved NNW for a time, and then changing direction to about WNW (see https://en.wikipedia.org/wiki/Evolution_of_Hawaiian_volcanoes). The most recent volcanic action is off the coast of Hawaii, at Lo ihi sea mount. The oldest volcanoes in the chain are in the Emporor Sea Mounts, many of which are so eroded that they are no longer above sea level.
 
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  • #15
Great information Mark, I'll be exploring some of your thoughts as we discuss this topic in my course this week.
Thanks.
 

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