What are metamorphic and sedimentary rocks, and how are faults and folds formed and their impact on human activities?

You're on a roll — Here are the answers to your questions: 2.2 2.2.5: Examples of this rock are quartzite, marble and slate. These are all metamorphic rocks*. 2.2.6: The sand and mud build up on the ocean floor near the mouths of rivers to form a sedimentary rock*. 2.2.7: Coal is an example of a sedimentary rock*. 2.3 2.3.1: The type of force that resulted in landform X (normal fault) is tensional* force. 2.3.2: A normal fault (X) is formed by tensional forces where the hanging wall moves downward* relative to the footwall, causing an extension of the crust. A reverse fault (Y) is formed by compressional forces where the hanging wall moves upward* relative to the footwall, causing a shortening of the crust. 2.3.3: Folding occurs when rocks bend* under compressional stress without breaking, typically forming anticlines and synclines. Faulting occurs when rocks break* and there is a visible displacement or movement along the fracture surface due to stress. 2.3.4: Three positive influences of block mountains and rift valleys formed by faults on human activities are: Mineral deposits:* Faulting can expose valuable mineral ores, making them accessible for mining. Tourism:* Block mountains and rift valleys often create dramatic landscapes, attracting tourists for sightseeing, hiking, and other recreational activities. Geothermal energy:* Rift valleys, especially those with volcanic activity, can be sources of geothermal energy, providing a renewable power source. Fertile soils:* The floors of some rift valleys can accumulate rich alluvial soils, making them suitable for agriculture. Drop the next question 📸