Intrusions, Inclusions, Cross Cuts intrude include
Intrusions, Inclusions, Cross Cuts - liquid rock (magma) under the Earth’s surface pushes up into any cracks or spaces may take millions of years - small or as big as mountains…. Sierra Nevadas, Devils Tower
Intrusions, Inclusions, Cross Cuts - liquid rock (magma) under the Earth’s surface pushes up into any cracks or spaces may take millions of years - small or as big as mountains…. Sierra Nevadas, Devils Tower
Intrusions, Inclusions, Cross Cuts - liquid rock (magma) under the Earth’s surface pushes up into any cracks or spaces may take millions of years - small or as big as mountains…. Devils Tower, Sierra Nevadas a piece of geological detritus that becomes incorporated into another rock or sediment ‘clast’ in sedimentary rock ‘xenolith’ in igneous rock
The Principle of Intrusive Relationships - invading igneous rock is always younger than the rock it intrudes - several types of intrusions: sill – an intrusion that happens between layers laccolith – a more prominent sill
The Principle of Intrusive Relationships - invading igneous rock is always younger than the rock it intrudes - several types of intrusions: sill – an intrusion that happens between layers
The Principle of Intrusive Relationships - invading igneous rock is always younger than the rock it intrudes - several types of intrusions: dike – an intrusion that cuts across pre-existing rock
The Principle of Intrusive Relationships - invading igneous rock is always younger than the rock it intrudes - several types of intrusions: dike – an intrusion that cuts across pre-existing rock
The Principle of Intrusive Relationships - invading igneous rock is always younger than the rock it intrudes - several types of intrusions: batholith – a large irregular discordant intrusion
The Principle of Intrusive Relationships - invading igneous rock is always younger than the rock it intrudes - several types of intrusions: batholith – a large irregular discordant intrusion
The Principle of Intrusive Relationships - invading igneous rock is always younger than the rock it intrudes - several types of intrusions:
The Principle of Inclusions any inclusion is older than the rock or sediment into which it has been included
Cross Cuts any geologic feature that cuts across a rock or sediment could be faults, intrusions or erosion The Principle of Cross Cutting any cross cut must be younger than the rock or sediment it cuts across.
Sequence erosion E fault (normal) D (intrusion) A B C (oldest)
erosion F (normal) E D (intrusion: dike) C erosion (angular unconformity, nonconformity) B (intrusion: batholith) A (reverse) brown/gray layers, folding (oldest)
Geo 4&5 Practice 7 Geo 4&5 Practice 8 (challenge)
If there is an unconformity write ‘unconformity’ (+ which one). If there is folding write ‘folding’ (+ which type). If there a fault write ‘fault’ (+ which type).
If there is an unconformity write ‘unconformity’ (+ which one). If there is folding write ‘folding’ (+ which type). If there a fault write ‘fault’ (+ which type).
If there is an unconformity write ‘unconformity’ (+ which one). If there is folding write ‘folding’ (+ which type). If there a fault write ‘fault’ (+ which type).
If there is an unconformity write ‘unconformity’ (+ which one). If there is folding write ‘folding’ (+ which type). If there a fault write ‘fault’ (+ which type).
Sequence