Unit 2 Lesson 1 Flashcards
Uniformitarianism
James Hutton proposed this theory in the late 1700’s
Geologic processes that happened in the past can be explained by current geologic processes . Geologic changes can be gradual (slow) or sudden (fast)
Example processes like volcanos and erosion that happen today also happened in the Past
Fossils
Traces or remains of an organism that lived long ago.
They are most commonly preserved in sedimentary rock
2 groups of fossils: trace fossils and body fossils
Ways that organisms become preserved as fossils ( Body Fossils)
A. Trapped in amber. Amber is formed when hardened tree sap is buried and preserved in sediment
B. Trapped in asphalt - which is sticky, thick tar which hardens. Organisms can be trapped
C. Buried in rock - organisms become buried in sediment. Then the sediment over time becomes rock. Bones and shells will become part of the rock
D. Become frozen - in very cold places animals that die may become frozen and preserved
E. Become petrified - when an organism’s tissues are replaced by minerals
Trace fossil
A fossilized structure that is formed in sedimentary rock by animal activity or in soft sediment
Examples: footprints, burrows, animal dung
Fossil record
All the fossils that have been discovered on Earth
Shows part of the history of life on earth
What can fossils tell us?
- About environmental changes over time
- How life forms have changed over time
How do scientists classify sedimentary rock
Composition - what it’s made of
Texture - tells the environment of the sediment
Features like ripples marks - tell us the motion of wind or water over the sediment
Features like mud cracks - show that an ancient lake or stream was part of an area
Climate
Describes the weather conditions in the area over a long period of time
Determined by temperature and precipitation
Ice core
A long cylinder of ice obtained from drilling through ice caps or sheets.
How do we study how climate has changed over time?
Trees. - tree rings tell us the age of the tree. Thick rings mean growing conditions were good. Thin rings mean that there were poor growing conditions
Sea floor sediment- the chemical composition and microorganisms in sediment tells us the climate when the organisms were alive
Ice cores - tell us the amounts of precipitation in the past