Final answer:
Extrusive rocks produced by an explosive volcano are generally expected to be light in color due to their rapid cooling and the presence of light-colored felsic minerals such as quartz and feldspar, which are typical in rocks like tuff and rhyolite.
"The correct option is approximately option 1"
Step-by-step explanation:
Based on the information provided about volcanic fragmental rocks and igneous rocks, we can determine the expected color of extrusive rocks produced by an explosive volcano. Explosive eruptions produce solid fragments and ash, often resulting in rocks such as tuff, which is described as light colored and sometimes contains glass and pumice fragments. Tuff may appear similar to rhyolite, which is a felsic extrusive igneous rock with a light gray to pinkish color.
Rhyolite is significant in this context due to its composition and formation process; it is very finely crystalline because it cools from a high-viscosity lava, which does not allow large crystals to form. With the rapid cooling rates of lava upon eruption, the resulting extrusive igneous rocks are fine-grained and often light in color due to the presence of minerals like quartz and feldspar, which are typically lighter in color than the mafic (dark-colored, iron and magnesium-rich) minerals.
Therefore, we would expect extrusive rocks produced by an explosive volcano to be generally light in color, as evidenced by rocks like tuff and rhyolite. Light coloration indicates a higher silica content, typical of felsic rocks, which are associated with more explosive volcanic activity.
This characteristic is opposed to the dark-colored basalts that tend to form from less explosive eruptions and have a higher content of mafic minerals.