Deeper and Deeper How can we tell the
- Slides: 10
Deeper, and Deeper How can we tell the age of the earth? What do rocks tell us about life on earth and the earth itself?
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• Different rocks will form layers over time • This follows the Law of Superposition (superposition = placed above) • Lower layers were set down first. Upper layers were laid down on top of those below.
Different rocks form in different ways under different environmental conditions: <---- Limestone: Formed from skeletal fragments of marine animals such as coral, forams, and molluscs <----- Sandstone: Formed from breaking down of larger rocks in desert environments or near oceans, rivers, deltas, etc. <----- Shale (mudstone): Formed from compacted mud in lakes, lagoons, or river floodplains
• Over time different animals live in the environments that form the layers • When they die, they became buried in the ground • Just like the layers themselves, the deeper the animal, the longer ago it lived
Fossils • Most animal remains decompose and disappear • With the right conditions, an animals remains will become preserved in the rock
FIVE MAIN TYPES OF FOSSILS Petrified Fossils Molds and Casts Trace Fossils Carbon Films Preserved Remains
• Fossils become our snapshot of how animals have changed in the past • Without this record, we would know little about past animals • However, the fossil record is imperfect: • Most animals don’t fossilize: Less than “ 1 in a million” become fossils. • Only certain environments fossilize: Usually with nearby water like oceans, rivers, and deltas, or sudden volcanic eruptions • Fossils are difficult to find: Most fossils are deep underground and need plate tectonics to bring them to the surface over millions of years
Age of the Earth So, how old is the Earth? • According to the oldest fossils—stromatolites found in Western Australia—the earth must be at least 3. 48 billon years old. • Scientists argue that the Earth is actually 4. 6 billion years old from dating meteorites and moon rocks that have not been effected by plate tectonics but formed at the same time as the Earth.
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