chaiwoot boonyasiriwat julie willis jerry schuster chris duross

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Optical Stratigraphy of a Wasatch fault trench wall and a Maritian surface using watershed-based segmentation Chaiwoot Boonyasiriwat Julie Willis Jerry Schuster Chris Duross

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Optical Stratigraphy of a Wasatch fault trench wall and a Maritian surface using watershed-based segmentation. Chaiwoot Boonyasiriwat Julie Willis Jerry Schuster Chris Duross. Motivation for digital trench wall logging Algorithm for separating rocks from fill Statistics Mars. - PowerPoint PPT Presentation

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Optical Stratigraphy of a Wasatch fault trench wall

and a Maritian surface using watershed-based segmentation

Chaiwoot BoonyasiriwatJulie Willis

Jerry SchusterChris Duross

Motivation for digital trench wall logging Algorithm for separating rocks from fill Statistics Mars

Pre-earthquake

Earthquake

900 years later

Development of a colluvial wedge

Motivation for digital

trench wall logging

Mapleton, Utah

“mega-trench”

1 meter

• Develop a rock segmentation algorithm to separate clasts from matrix.

• Determine whether colluvial wedges, debris flows and channel deposits can be statistically differentiated.

Mapleton Trench Level 1

1 m

1 meter

Colluvial Wedge

Debris Flow

ChannelDeposit

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

10 cm

Channel Deposit 2

1 meter

Algorithm successfully separates rocks from fill – 80% accuracy.

• Can colluvial wedges, debris flows and channel deposits be statistically differentiated? Compare: Orientation, Eccentricity, Percent Rock

Mapleton Trench Level 1

1 m

Colluvial Wedge

Debris Flow

ChannelDeposit

Colluvial Wedge 1

Orientation? Eccentricity? Percent Rock?

Colluvial Wedge 3

Orientation? Eccentricity? Percent Rock?

Debris Flow 1

Orientation? Eccentricity? Percent Rock?

Channel Deposit 1

Orientation? Eccentricity? Percent Rock?

Eccentricity

2.8% < 0.2

12.5% < 0.2

2.5% < 0.2

Percent Rock

Channel Deposits: 32 %

Colluvial Wedge: 48 %

Debris Flow: 42 %

Clast Orientation

1 meter

Can colluvial wedges, debris flows and channel deposits be statistically differentiated?

Orientation – Colluvial Wedge

Eccentricity, Percent Rock – Channel Deposits

Mapleton Trench Level 1

1 m

Colluvial Wedge

Debris Flow

ChannelDeposit

1 meter

Future work: • Use the segmentation algorithm to objectively log trench walls and

build data for more rigorous statistics • Mars and beyond . . .

Mapleton Trench Level 1

1 m

Colluvial Wedge

Debris Flow

ChannelDeposit

? ?

?

?

Martian Surface

Clast Orientation

Mars Statistics

Eccentricity