BENEATH THE MARTIAN SOIL.
black/silver
Silica itself is a mineral compound and is typically colorless or white. However, impurities can give silica various colors such as pink, green, or black.
silica
Quartz
A milky white mineral made up of silica is quartz. Quartz is the second most abundant mineral on the Earth's crust.
White chert is a microcrystalline sedimentary rock made up of silica. It forms in environments where silica-rich waters deposit material that solidifies into fine-grained, white-colored chert.
You can find sand without crystalline silica in locations such as non-beach environments like riverbeds, quarries, and desert regions where the sand has not undergone weathering processes that convert it into crystalline silica. Silica-free sands are used in industries that require non-silica materials, such as foundries and construction.
White sand, which is primarily composed of silica, is insoluble in hydrochloric acid. Silica is a very stable compound and does not react with hydrochloric acid under normal conditions.
Generally, igneous rocks with more silica are lighter in color.
The silica gel colour is blue, and after capturing the moisture the colour is become a pink colour.
The mineral you are referring to is likely known as "opal." Opal is a hydrated amorphous form of silica, characterized by its milky white appearance and iridescent colors when exposed to light. It is commonly used in jewelry due to its unique beauty and play of colors.
Silica in molten material tends to crystallise as quartz, which is white or mostly pale in colour. So felsic rocks (from silica-rich magma) tend to be pale, while mafic rocks (from silica-poor magma) tend to be dark in colour.