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CROSSCUTTING RELATIONSHIPS Sequence of Events
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Page 1: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

CROSS‐CUTTING RELATIONSHIPS

Sequence of Events ‐

Page 2: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Steno's Laws

Nicholas Steno (1669)

• Principle of Superposition

• Principle of Original Horizontality

These laws apply to both sedimentary and volcanic rocks.

Page 3: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Principle of Superposition

In a sequence of undisturbed layered rocks, the oldest rocks are on the bottom.

Page 4: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Fig. 10.3

Page 5: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Principle of Original Horizontality

Layered strata are deposited horizontal or nearly horizontal or nearly parallel to the Earth’s surface.

Page 6: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Earth Issues 10.1

Page 7: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Sequence of Events

education.usgs.gov/lessons/schoolyard/CoolGeologyActivity.html

Page 8: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Cross‐cutting Relationships

earthscienceinmaine.wikispaces.com/11.2+Relative+Ages+of+Rocks

Page 9: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Cross‐cutting Relationships

evolution.berkeley.edu/evosite/evo101/IIE1Whathappenedwhen.shtml

Page 10: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Cross‐cutting Relationships

evolution.berkeley.edu/evosite/evo101/IIE1Whathappenedwhen.shtml

Page 11: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Cross‐cutting Relationships

volcano.oregonstate.edu/vwdocs/vwlessons/magma_pathways/act6.html

Page 12: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

Fig. Story 10.11

Page 13: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

PHYSICAL AND CHEMICAL WEATHERING

Page 14: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

13_05b.JPG

Page 15: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

13_10.JPG

Page 16: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

13_04au.jpg

Page 17: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

13_22.JPG

Page 18: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

13_20.JPG

Page 19: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

DEPOSITIONAL SYSTEMS

From: SEPM Sequence Stratigraphy Web: sepmstrata.org/exercises.html

Page 20: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

“Clastic Hierarchies”Christopher G. St. C. Kendall

Submarine Canyons & Deep Sea Fans

USGS Image

Offshore Los Angeles

Page 21: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

sepmstrata.org/deepwater/DeepwaterClasticArchitecture.html

Page 22: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

“Clastic Hierarchies”Christopher G. St. C. Kendall

Clastic Depositional SystemsClastic Depositional Systems

Page 23: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

“Clastic Hierarchies”Christopher G. St. C. Kendall

Clastic Depositional SystemsClastic Depositional Systems

Page 24: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

“Clastic Hierarchies”Christopher G. St. C. Kendall

Clastic Depositional SystemsClastic Depositional Systems

Page 25: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

sepmstrata.org/deepwater/DeepwaterClasticArchitecture.html

Page 26: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest
Page 27: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

“Clastic Hierarchies”Christopher G. St. C. Kendall

Tide‐Dominated Niger Delta

Page 28: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

“Clastic Hierarchies”Christopher G. St. C. Kendall

Geomorphologyof Coast

Page 29: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

“Clastic Hierarchies”Christopher G. St. C. Kendall

Delta Morphology

Page 30: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest
Page 31: CROSS CUTTING RELATIONSHIPS - Sahraweb.sahra.arizona.edu/education2/fossEH/PLC/SequenceofEvents.pdf · Principle of Superposition In a sequence of undisturbed layered rocks, the oldest

“Clastic Hierarchies”Christopher G. St. C. Kendall

Meandering Fluvial System

Allen, 1964


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