Answer:
C. Metallic and non-metallic
Explanation:
The two types of geologic resources are Metallic and non-metallic
1. Mount Mayon- Albay
2. Taal Volcano - Batangas
3. Mount Kanlaon - Negros Oriental
4. Mount Bulusan - Sorsogon
5. Mount Makaturing- Lanao del Sur
6a. Musuan Volcano - Bukidnon
6b. Mount Ragang- Lanao del Sur
7a. Didicas Volcano - Cagayan
7b. Hibok-Hibok- Camiguin
8. Smith Volcano - Cagayan
9a. Babuyan Claro - Cagayan
9b. Mount Banahaw- Quezon
10a. Dequey- Batanes
10b. Mount Parker- Cotabato
Rocks are broken down into smaller pieces by the process of weathering and erosion.
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Answer:
See it in the explanation
Explanation:
1) Carbon moves from atmosphere to hydrosphere and biosphere in the process of photosynthesis and to lithosphere by deposition of dead bodies while from hydrosphere and biosphere, carbon can be move in the process of respiration by animals.
2) During respiration process which takes place in plants in which carbondioxide is released and by eating carbon containing food by animals. By decomposing the food, carbon is releases in the form of carbondioxide.
3) Carbon can be used by the marine plants in the process of photosynthesis and during the process of diffusion, carbon is also dissolve in water bodies.
4) When the plants and animals die, the carbon which is present inside their body is buried in the soil present at the bottom of the ocean and the shells and corels of some animals also contain carbon which is soon be the part of the lithosphere when they die.
5) After the decomposition of seashell, carbondioxide is produced because shells are made up of calcium carbonate.
Convection currents occur in the MANTLE. The mantle is the second layer of the earth after the crust. The mantle is approximately 2900 km thick. Convection currents are triggered or fueled by the heat from the Earth's core.
The part of the mantle closest to the core gets heated. It then becomes less dense than the layers above so it rises. When this rising plume interacts with the crust it cools and becomes more dense than the layers below and so it sinks and this circular motion continues to form convection currents.
