According to Bowen's Reaction Series with decreasing temperature

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Multiple Choice

According to Bowen's Reaction Series with decreasing temperature

Explanation:
As magma cools, minerals crystallize in a specific order, with the highest-temperature stable minerals forming first. Olivine is stable at the highest temperatures among common rock-forming minerals, so it crystallizes early as the melt begins to cool. As olivine is removed from the melt, the remaining liquid evolves toward compositions that favor minerals that crystallize at lower temperatures. Quartz, potassium feldspar, and muscovite require further cooling and higher silica contents, so they appear later in the sequence. Therefore, olivine is the first mineral to crystallize as temperature decreases.

As magma cools, minerals crystallize in a specific order, with the highest-temperature stable minerals forming first. Olivine is stable at the highest temperatures among common rock-forming minerals, so it crystallizes early as the melt begins to cool. As olivine is removed from the melt, the remaining liquid evolves toward compositions that favor minerals that crystallize at lower temperatures. Quartz, potassium feldspar, and muscovite require further cooling and higher silica contents, so they appear later in the sequence. Therefore, olivine is the first mineral to crystallize as temperature decreases.

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