Hot Spots - PowerPoint PPT Presentation

1 / 15
About This Presentation
Title:

Hot Spots

Description:

Looking at Hawai'i, and volcanic seamounts nearby (underwater volcanic islands) Current Hawaiian. Islands. What is a hot spot? ... – PowerPoint PPT presentation

Number of Views:248
Avg rating:3.0/5.0
Slides: 16
Provided by: chrisd58
Category:
Tags: hawaiian | hot | islands | spots

less

Transcript and Presenter's Notes

Title: Hot Spots


1
Hot Spots
2
Intraplate Volcanism
USGS
3
Hawaii
  • Best example of intraplate volcanism
  • More lava is extruded here constantly than
    anywhere else on Earth!

4
A Bigger Picture
  • Looking at Hawaii, and volcanic seamounts nearby
    (underwater volcanic islands)

Current Hawaiian Islands
5
What is a hot spot?
  • Some mantle anomaly allows the oceanic or
    continental lithosphere to melt where it would
    not normally melt
  • The anomaly (usually) stays stationary
  • The plate moves over it

6
The Hawaiian Hot Spot
University of North Dakota
7
  • Islands and seamounts get older as you move away
    from the hotspot

8
Mantle Plumes
  • The mantle anomaly thought to cause hot spots
  • Numerous theories as to what plumes are, and
    whether they even exist

9
Convection Model
  • Plumes are areas of convective upwelling
  • Same mechanism that drives plate motion causes
    mid-plate lithosphere to melt

USGS
10
Problem with Convection Model
  • Lavas at rift zones contain very little 3He
    (Helium-3)
  • Hawaiian lavas contain lots of 3He
  • 3He is not produced on Earth by any natural
    process
  • Formed in Big Bang
  • 3He was trapped in the core during the formation
    of the earth
  • Plumes must have a deeper source than the same
    mantle convection that drives plate motion
  • Or there needs to be some explanation for
    anomalous 3He in Hawaiian lavas

11
Deep Mantle Plumes
  • Plumes originate from or near the core-mantle
    boundary
  • Represent the mechanism by which heat is lost
    from the core

12
What would cause a deep mantle plume?
  • Ultra-low velocity zones
  • Areas of liquid/crystal mush at the core-mantle
    boundary
  • Cover 12 of the globe, and 1/3 of all hotspots
    lie above them, including ALL the major ones
  • Liquid/crystal mush conducts heat 100x better
    than solid mantle rock
  • Sets up perhaps a deeper convection than that
    which drives plate tectonics

Solid plastically- deforming mantle
Liquid/Crystal Mush
Liquid Outer Core
Williams 1997
13
Areas of ULVZ
Williams 1997
Yellow major hotspots Red ULVZ locations
14
Two-layer convection?
Leeds University
15
New Research
  • Finding plumes
  • Seismic techniques that detected
  • Layers of Earth
  • ULVZs
  • Not sensitive enough to detect plumes
  • Too small a feature?
  • And/or plumes arent what we think they are
  • Perhaps more than one type of plume
Write a Comment
User Comments (0)
About PowerShow.com