Answer: Hello some parts of your question is missing attached below is the missing detail
answer :
1) attached below
2) Non-conformity
Explanation:
1) Line along the boundary between Vishnu schist and relatively horizontal sedimentary rocks
attached below
2) The type of unconformity traced above is called Non - Conformity
i.e. when a sedimentary rock lies above an igneous rock or a metamorphic rock it is called Non-conformity
Answer:
Feldspar-clay
Quartz- No chemical change
Olivine- Limonite
Explanation:
When chemically weathered, some of the original minerals of granite change into different minerals.
Feldspar, for example, tends to hydrate and transform into a clay mineral.
Iron-rich minerals, like olivine, turn into limonite by chemical weathering. Quartz is considerably resistant to chemical weathering, so it´s the least susceptible to the chemical change.
Answer:
The Mediterranean area is the lightest green color towards the bottom left (southeast portion) of the map.
The Mediterranean region has been characterized with: rainy winters and dry summers; grow native fruits of figs, grapes, and olives; and include the native species of turtles, seals, deer, badgers, and toads.
Explanation: