Examine the diagram above which shows the impact of folding on layers of rock during the Armorican fold mountain building period - Leaving Cert Geography - Question 2A - 2020
Question 2A
Examine the diagram above which shows the impact of folding on layers of rock during the Armorican fold mountain building period. Answer each of the following questi... show full transcript
Worked Solution & Example Answer:Examine the diagram above which shows the impact of folding on layers of rock during the Armorican fold mountain building period - Leaving Cert Geography - Question 2A - 2020
Step 1
Name the part of a fold, labelled A, that forms when layers of rock are pushed upwards.
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Answer
The part of a fold labelled A that forms when layers of rock are pushed upwards is known as an Anticline.
Step 2
Name the part of a fold, labelled B, that forms when layers of rock are pushed downwards.
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The part of a fold labelled B that forms when layers of rock are pushed downwards is known as a Syncline.
Step 3
Name one Irish mountain range that was formed as part of the Armorican folding.
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One Irish mountain range formed as part of the Armorican folding is the MacGillycuddy's Reeks.
Step 4
Name a different period of fold mountain building that shaped the Irish landscape over the last 400 million years.
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A different period of fold mountain building that shaped the Irish landscape is the Caledonian folding.
Step 5
Explain briefly the term compression as it relates to folding.
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Compression in the context of folding refers to the process where tectonic forces push rocks together, causing them to fold. This pressure is generally caused by the movement of tectonic plates, leading to the development of folds like anticlines and synclines in the Earth's crust.
Step 6
Name two types of fault.
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Two types of fault are: 1. Normal fault, where the hanging wall moves downward relative to the footwall. 2. Reverse fault, where the hanging wall moves upward relative to the footwall.
Step 7
Name two landscape features formed by faulting.
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Two landscape features formed by faulting are: 1. Fault scarps, which are steep surfaces created by fault movement. 2. Graben valleys, formed when land between two faults sinks.
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