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Roger N. Clark,
Joe Boardman,
Jack Mustard, Fred Kruse,
Cindy Ong, Carle Pieters,
And Gregg Swayze
IGARSS
August 1, 2006
Mineral Mapping
and Applications of
Imaging Spectroscopy
Mars
Cuprite 1-um 3d
This talk is like a drink from a fire hose………
Illustrating diverse mineral mapping
being done with Imaging Spectroscopy.
Cuprite 2um 3d
We honor Alex Goetz with (yet) another look at Cuprite
Mineral deposits.
Provide resources for
modern society.
Possible sources of
life.
Possible sources of
acidic water.
Cuprite, Nevada is
an ancient
hydrothermal
alteration system
(like yellowstone.)
A real-world example
Let’s look for
well-crystallized
kaolinite at Cuprite.
Mineral mapping and applications of imaging spectroscopy
Mineral mapping and applications of imaging spectroscopy
AVIRIS
Kaolinite
Hyperion
Kaolinite
Very similar results despite
Very different methods
Kruse analysis for Kaolinite
Group minerals (above):
ACORN, MNF transform.
Pixel Purity Index,
n-D Visualizer,
Spectral Analyst,
Classification and
subpixel analysis,
Mixture-Tuned-Matched-
Filtering (MTMF)
Clark et al. JGR 2003
Tetracorder analysis (left)
Mineral mapping and applications of imaging spectroscopy
Mineral mapping and applications of imaging spectroscopy
March 1, 2001
EO-1 Hyperion
Mineral Map
Kruse analysis:
ACORN, MNF transform.
Pixel Purity Index,
n-D Visualizer,
Spectral Analyst,
Classification and
subpixel analysis,
Mixture-Tuned-Matched-
Filtering (MTMF)
19 June 1997 AVIRIS
Spectrally Predominant
Mineral Map
Clark et al. JGR 2003 Tetracorder analysis
But How Better to Honor Alex Than to Find
Something New at Good Old Cuprite?
Buddingtonite, Even!
•MTMF applied to
1999 HyMap AIG
Cuprite data
•Finds NEW
Buddingtonite!
•Better algorithms +
better data = better
geologic results
New!
Alex’s
Buddingtonite
From Joe Boardman
MTMF Finds Buddingtonite at ~1% Abundance
(New location verified by Gregg Swayze)
purest
detection
weakest
detection
buddingtonite
feature
New discovery
after how many
years as a test
site?
If Cuprite still has secrets, we have only just begun!
From Joe Boardman
Yellowstone
Yellowstone thermal pool.
Colors indicate life living at
different temperatures.
Yellowstone
Major distinctive mineralogy from TES/THEMIS: Olivine
(Hoefen et al. (2003); Hamilton and Christensen (2005)
Hoefen et al. (2003)
Hamilton and Christensen (2005
Olivine
Mineral Mapping on Mars
Hoefen et al. (2003)
Regional map of Syrtis Major
region showing regions
enriched in olivine, High
Calcium Pyroxene (HCP) and
Low Calcium Pyroxene (LCP).
Results draped over MOLA
shaded relief
Mustard et al.,
Science, 2005
Mars:
Mineral
Mapping
with
OMEGA
0.4
0.5
0.6
0.7
0.8
1 1.2 1.4 1.6 1.8 2 2.2 2.4 2.6
Basalt HCP-enriched
Olivine-rich
LCP-enriched
Phyllosilicate
Wavelength (µm)
RelativeReflectance
Local map of Nili Fossae
region showing regions
enriched in olivine (red),
LCP (green) and
Phyllosilcate (blue).
Results draped over
HRSC imaging
Mustard
et al.,
2006
0
0.1
0.2
0.3
0.4
0.5
0.6
0.7
500 1000 1500 2000 2500 3000
Reflectance
Wavelength nm
Lunar Mineral Separates
Soils
Adsorbed
Water
Olivine
Pyroxenes
Plagioclase
Melt-G
Cr-Spinel
Melt-C
Moon Mineralogy Mapper (M3)
Chandrayaan-1 launches in early 2008
from India
– 100 km circular polar Orbit
– Two year mission duration
– PI: C. Pieters, Brown U.; Built by JPL
M3 is a pushbroom imaging spectrometer
– 40 km FOV, contiguous orbits
– 0.43 to 3.0 µm, high SNR
– 1 Gbyte/orbit
Targeted Mode: Optimum
– Resolution (100 km orbit):
• 70 m/pixel spatial
• 10 nm spectral [261 bands]
– 3 optical periods [10 - 30% coverage]
• 12 to 15 deg latitude/orbit
Global Mode: Full Coverage
– Resolution (100 km orbit):
• 140 m/pixel spatial
• 20 & 40 nm selected (87 bands,
~3x spectral averaging)
– 1 optical period [100%]
Clark et al., JGR (2003)
Ice shows a large
range of spectral
properties as a
function of
grain size. Phase
change shifts
bands. This allows
ice grain size and
melting snow to be
mapped.
Cassini VIMS Enceladus Ice Map
Brown et al., Science, 311, p. 1425-1428, 2006.
Cassini ISS Image
of active plumes
Enceladus:
260 km in radius
Orbital radius:
4 Saturn radii
Active plumes
contribute to E-ring
Very bright surface.
Porco et al., Science,
2006.
Titan VIMS
Visible
Light
(Voyager)
VIMS
Environmental Studies of the World Trade Center
area after the September 11, 2001 attack.
Roger N. Clark, Robert O. Green,
Gregg A. Swayze, Greg Meeker,
Steve Sutley, Todd M. Hoefen,
K. Eric Livo, Geoff Plumlee,
Betina Pavri, Chuck Sarture,
Steve Wilson, Phil Hageman,
Paul Lamothe, J. Sam Vance, Joe
Boardman, Isabelle Brownfield,
Carol Gent, Laurie C. Morath,
Joseph Taggart,
Peter M. Theodorakos, and
Monique Adams
USGS NASA/JPL USEPA
AVIRIS sees the fires through
the smoke, making repeat
observations
• Sept 16th fire images were delivered
to the White House where agencies
were briefed on the results and
implications.
• Tuesday evening, Sept. 18: fire
fighting methods were changed.
CNN announces the firefighters are
changing from a rescue operation to
a recovery effort.
• Flights occur Sept 16, 18, 22, and
23, 2001.
• The fire fighting strategy helped.
• Spectral shape was used to
determine fire temperatures;
intensity the area of the fires.
• Analysis of fire temperatures
Indicated over 800o C on 9/16, but
mostly out by 9/23.
The debris has the same
composition as the rest
of the city
• The similarities in
composition makes mapping
WTC materials a challenge.
• The same materials can be
seen throughout the city.
• But one can use context to
see the debris cloud.
Mineral mapping and applications of imaging spectroscopy
Orange pixels indicate possible
serpentines.
Clark et al., American Chemical
Society, 2005.
Green to yellow: WTC dust.
Spectroscopy was done on each WTC
sample then each sample was chemically
and physically analyzed
(Swayze et al., ACS, 2005).
Synthesis of Results:
AVIRIS + Sample Analysis
Spectrometers: evolution in size
AVIRIS
Moon Mineral
Mapper
ASD Spectrometer
• Imaging Spectroscopy has matured
in the last few years showing abilities
to map materials in environmental
and disaster situations. As well as
geology and ecosystems.
• As reference reflectance spectral
libraries become mature, more
applications could be developed,
including screening methods, real
time monitoring, and post event
assessment.
• Applications could include detection
and mapping of minerals, organics,
mineral fibers, biota, fires and their
temperatures and many other
materials.
• Operational imaging spectrometers
are working throughout the Solar
System
Conclusions
A field spectrometer is used to measure the composition
of a mud pit in Yellowstone National Park (it is kaolinite).
Imaging Spectroscopy:
A powerful Tool
Thank
You
Alex!

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Mineral mapping and applications of imaging spectroscopy

  • 1. Roger N. Clark, Joe Boardman, Jack Mustard, Fred Kruse, Cindy Ong, Carle Pieters, And Gregg Swayze IGARSS August 1, 2006 Mineral Mapping and Applications of Imaging Spectroscopy Mars
  • 2. Cuprite 1-um 3d This talk is like a drink from a fire hose……… Illustrating diverse mineral mapping being done with Imaging Spectroscopy.
  • 3. Cuprite 2um 3d We honor Alex Goetz with (yet) another look at Cuprite
  • 4. Mineral deposits. Provide resources for modern society. Possible sources of life. Possible sources of acidic water. Cuprite, Nevada is an ancient hydrothermal alteration system (like yellowstone.) A real-world example Let’s look for well-crystallized kaolinite at Cuprite.
  • 7. AVIRIS Kaolinite Hyperion Kaolinite Very similar results despite Very different methods Kruse analysis for Kaolinite Group minerals (above): ACORN, MNF transform. Pixel Purity Index, n-D Visualizer, Spectral Analyst, Classification and subpixel analysis, Mixture-Tuned-Matched- Filtering (MTMF) Clark et al. JGR 2003 Tetracorder analysis (left)
  • 10. March 1, 2001 EO-1 Hyperion Mineral Map Kruse analysis: ACORN, MNF transform. Pixel Purity Index, n-D Visualizer, Spectral Analyst, Classification and subpixel analysis, Mixture-Tuned-Matched- Filtering (MTMF) 19 June 1997 AVIRIS Spectrally Predominant Mineral Map Clark et al. JGR 2003 Tetracorder analysis
  • 11. But How Better to Honor Alex Than to Find Something New at Good Old Cuprite? Buddingtonite, Even! •MTMF applied to 1999 HyMap AIG Cuprite data •Finds NEW Buddingtonite! •Better algorithms + better data = better geologic results New! Alex’s Buddingtonite From Joe Boardman
  • 12. MTMF Finds Buddingtonite at ~1% Abundance (New location verified by Gregg Swayze) purest detection weakest detection buddingtonite feature New discovery after how many years as a test site? If Cuprite still has secrets, we have only just begun! From Joe Boardman
  • 13. Yellowstone Yellowstone thermal pool. Colors indicate life living at different temperatures. Yellowstone
  • 14. Major distinctive mineralogy from TES/THEMIS: Olivine (Hoefen et al. (2003); Hamilton and Christensen (2005) Hoefen et al. (2003) Hamilton and Christensen (2005 Olivine Mineral Mapping on Mars Hoefen et al. (2003)
  • 15. Regional map of Syrtis Major region showing regions enriched in olivine, High Calcium Pyroxene (HCP) and Low Calcium Pyroxene (LCP). Results draped over MOLA shaded relief Mustard et al., Science, 2005 Mars: Mineral Mapping with OMEGA
  • 16. 0.4 0.5 0.6 0.7 0.8 1 1.2 1.4 1.6 1.8 2 2.2 2.4 2.6 Basalt HCP-enriched Olivine-rich LCP-enriched Phyllosilicate Wavelength (µm) RelativeReflectance Local map of Nili Fossae region showing regions enriched in olivine (red), LCP (green) and Phyllosilcate (blue). Results draped over HRSC imaging Mustard et al., 2006
  • 17. 0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 500 1000 1500 2000 2500 3000 Reflectance Wavelength nm Lunar Mineral Separates Soils Adsorbed Water Olivine Pyroxenes Plagioclase Melt-G Cr-Spinel Melt-C Moon Mineralogy Mapper (M3) Chandrayaan-1 launches in early 2008 from India – 100 km circular polar Orbit – Two year mission duration – PI: C. Pieters, Brown U.; Built by JPL M3 is a pushbroom imaging spectrometer – 40 km FOV, contiguous orbits – 0.43 to 3.0 µm, high SNR – 1 Gbyte/orbit Targeted Mode: Optimum – Resolution (100 km orbit): • 70 m/pixel spatial • 10 nm spectral [261 bands] – 3 optical periods [10 - 30% coverage] • 12 to 15 deg latitude/orbit Global Mode: Full Coverage – Resolution (100 km orbit): • 140 m/pixel spatial • 20 & 40 nm selected (87 bands, ~3x spectral averaging) – 1 optical period [100%]
  • 18. Clark et al., JGR (2003) Ice shows a large range of spectral properties as a function of grain size. Phase change shifts bands. This allows ice grain size and melting snow to be mapped.
  • 19. Cassini VIMS Enceladus Ice Map Brown et al., Science, 311, p. 1425-1428, 2006. Cassini ISS Image of active plumes Enceladus: 260 km in radius Orbital radius: 4 Saturn radii Active plumes contribute to E-ring Very bright surface. Porco et al., Science, 2006.
  • 21. Environmental Studies of the World Trade Center area after the September 11, 2001 attack. Roger N. Clark, Robert O. Green, Gregg A. Swayze, Greg Meeker, Steve Sutley, Todd M. Hoefen, K. Eric Livo, Geoff Plumlee, Betina Pavri, Chuck Sarture, Steve Wilson, Phil Hageman, Paul Lamothe, J. Sam Vance, Joe Boardman, Isabelle Brownfield, Carol Gent, Laurie C. Morath, Joseph Taggart, Peter M. Theodorakos, and Monique Adams USGS NASA/JPL USEPA
  • 22. AVIRIS sees the fires through the smoke, making repeat observations • Sept 16th fire images were delivered to the White House where agencies were briefed on the results and implications. • Tuesday evening, Sept. 18: fire fighting methods were changed. CNN announces the firefighters are changing from a rescue operation to a recovery effort. • Flights occur Sept 16, 18, 22, and 23, 2001. • The fire fighting strategy helped. • Spectral shape was used to determine fire temperatures; intensity the area of the fires. • Analysis of fire temperatures Indicated over 800o C on 9/16, but mostly out by 9/23.
  • 23. The debris has the same composition as the rest of the city • The similarities in composition makes mapping WTC materials a challenge. • The same materials can be seen throughout the city. • But one can use context to see the debris cloud.
  • 25. Orange pixels indicate possible serpentines. Clark et al., American Chemical Society, 2005. Green to yellow: WTC dust. Spectroscopy was done on each WTC sample then each sample was chemically and physically analyzed (Swayze et al., ACS, 2005). Synthesis of Results: AVIRIS + Sample Analysis
  • 26. Spectrometers: evolution in size AVIRIS Moon Mineral Mapper ASD Spectrometer
  • 27. • Imaging Spectroscopy has matured in the last few years showing abilities to map materials in environmental and disaster situations. As well as geology and ecosystems. • As reference reflectance spectral libraries become mature, more applications could be developed, including screening methods, real time monitoring, and post event assessment. • Applications could include detection and mapping of minerals, organics, mineral fibers, biota, fires and their temperatures and many other materials. • Operational imaging spectrometers are working throughout the Solar System Conclusions
  • 28. A field spectrometer is used to measure the composition of a mud pit in Yellowstone National Park (it is kaolinite). Imaging Spectroscopy: A powerful Tool Thank You Alex!