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● Scientists began studying _____________ to determine the age of the Earth.
● Law of Uniformitarianism: the idea that _________, _________, and _________ laws operate today as they did long ago. Led to the idea of _________ dating.
● Relative Dating: used by scientists to tell the _________ of some rocks in a formation compared to _________ rocks. Cannot be used to determine the exact _________ of a rock. Scientists used relative dating to tell which _________ of rocks in the __________________ formed _________ or last. Several laws are used to find the relative ages of _________.
○ Law of Superposition: the _________ layers of rocks are at the bottom, the _________ rocks are at the top.
○ Law of Crosscutting: when a rock cuts through other _________ of rocks, the rock that is _________ through the other layers is _________ than the rocks it cuts through.
■ Layer A in the diagram is the ___________
■ Layer B in the diagram is the ___________
■ Layer C in the diagram is the ___________
○ Law of Inclusion: the rock _________ another
rock is _________ than the rock surrounding it.
● By using the process of correlation, scientists can match rocks at different ___________ that formed at the same _________ by the same _________ to draw conclusions. For example, if scientists found _________ of a marine animals in another state and the ____________, they could draw a _________ that both areas were covered by _________ at that time.
● Fossils: the ___________ remains or _________ of an _________ that lived in the _________. Only a ______ plants and animals become __________. Often _____________ decays before it can become _________. Being _________ or buried in rocks increases the chance of an organism becoming a fossil. The fossil record tells us what _________ and _________ lived on the Earth in the past and what the _________ was like.
● Scientists began studying _____________ to determine the age of the Earth.
● Law of Uniformitarianism: the idea that _________, _________, and _________ laws operate today as they did long ago. Led to the idea of _________ dating.
● Relative Dating: used by scientists to tell the _________ of some rocks in a formation compared to _________ rocks. Cannot be used to determine the exact _________ of a rock. Scientists used relative dating to tell which _________ of rocks in the __________________ formed _________ or last. Several laws are used to find the relative ages of _________.
○ Law of Superposition: the _________ layers of rocks are at the bottom, the _________ rocks are at the top.
○ Law of Crosscutting: when a rock cuts through other _________ of rocks, the rock that is _________ through the other layers is _________ than the rocks it cuts through.
■ Layer A in the diagram is the ___________
■ Layer B in the diagram is the ___________
■ Layer C in the diagram is the ___________
○ Law of Inclusion: the rock _________ another
rock is _________ than the rock surrounding it.
● By using the process of correlation, scientists can match rocks at different ___________ that formed at the same _________ by the same _________ to draw conclusions. For example, if scientists found _________ of a marine animals in another state and the ____________, they could draw a _________ that both areas were covered by _________ at that time.
● Fossils: the ___________ remains or _________ of an _________ that lived in the _________. Only a ______ plants and animals become __________. Often _____________ decays before it can become _________. Being _________ or buried in rocks increases the chance of an organism becoming a fossil. The fossil record tells us what _________ and _________ lived on the Earth in the past and what the _________ was like.
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● Scientists began studying **radioactive isotopes and decay** to determine the age of the Earth.
● Law of Uniformitarianism: the idea that **geological, physical, and chemical** laws operate today as they did long ago. Led to the idea of **absolute** dating.
● Relative Dating: used by scientists to tell the **relative ages** of some rocks in a formation compared to **other** rocks. Cannot be used to determine the exact **age** of a rock. Scientists used relative dating to tell which **layers** of rocks in the **strata** formed **first** or last. Several laws are used to find the relative ages of **rock layers**.
○ Law of Superposition: the **oldest** layers of rocks are at the bottom, the **youngest** rocks are at the top.
○ Law of Crosscutting: when a rock cuts through other **layers** of rocks, the rock that is **cutting** through the other layers is **younger** than the rocks it cuts through.
■ Layer A in the diagram is the **oldest**
■ Layer B in the diagram is the **younger**
■ Layer C in the diagram is the **youngest**
○ Law of Inclusion: the rock **inclusion** from another rock is **older** than the rock surrounding it.
● By using the process of correlation, scientists can match rocks at different **locations** that formed at the same **time** by the same **processes** to draw conclusions. For example, if scientists found **fossils** of marine animals in another state and the **original site**, they could draw a **conclusion** that both areas were covered by **water** at that time.
● Fossils: the **preserved** remains or **traces** of an **organism** that lived in the **past**. Only a **few** plants and animals become **fossils**. Often **organic material** decays before it can become **fossilized**. Being **buried** or buried in rocks increases the chance of an organism becoming a fossil. The fossil record tells us what **organisms** and **species** lived on the Earth in the past and what the **environment** was like.
Feel free to adjust any part based on your specific needs or preferences!
● Scientists began studying **radioactive isotopes and decay** to determine the age of the Earth.
● Law of Uniformitarianism: the idea that **geological, physical, and chemical** laws operate today as they did long ago. Led to the idea of **absolute** dating.
● Relative Dating: used by scientists to tell the **relative ages** of some rocks in a formation compared to **other** rocks. Cannot be used to determine the exact **age** of a rock. Scientists used relative dating to tell which **layers** of rocks in the **strata** formed **first** or last. Several laws are used to find the relative ages of **rock layers**.
○ Law of Superposition: the **oldest** layers of rocks are at the bottom, the **youngest** rocks are at the top.
○ Law of Crosscutting: when a rock cuts through other **layers** of rocks, the rock that is **cutting** through the other layers is **younger** than the rocks it cuts through.
■ Layer A in the diagram is the **oldest**
■ Layer B in the diagram is the **younger**
■ Layer C in the diagram is the **youngest**
○ Law of Inclusion: the rock **inclusion** from another rock is **older** than the rock surrounding it.
● By using the process of correlation, scientists can match rocks at different **locations** that formed at the same **time** by the same **processes** to draw conclusions. For example, if scientists found **fossils** of marine animals in another state and the **original site**, they could draw a **conclusion** that both areas were covered by **water** at that time.
● Fossils: the **preserved** remains or **traces** of an **organism** that lived in the **past**. Only a **few** plants and animals become **fossils**. Often **organic material** decays before it can become **fossilized**. Being **buried** or buried in rocks increases the chance of an organism becoming a fossil. The fossil record tells us what **organisms** and **species** lived on the Earth in the past and what the **environment** was like.
Feel free to adjust any part based on your specific needs or preferences!
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