Answer:
Ferrous (Fe²⁺) and magnesium cation (Mg²⁺).
Explanation:
The olivine mineral is a type of orthosilicate, which is generally yellow to yellow-green in color. It is the main component of the upper mantle of the Earth, which can be found in igneous and metamorphic rocks.
The olivine mineral exists in the form of Mg₂SiO₄, Fe₂SiO₄, or (Mg,Fe)₂SiO₄.
<u>This silicate consists of two divalent cations, ferrous (Fe²⁺) and magnesium cation (Mg²⁺).</u>
<span>I would say
Government systems lack capacity.
and
Representative government is increasing.</span>
Answer:
all of them can be a factor for a landslide
Explanation:
yeah
A) some kind of subduction zone
Because parallel measures one degree north or south of the equator, with 90 degree north of the equator and 90 degree south of the equator.
