Yes it combines with many nonmetals such as halogens, oxygen, sulfur etc. Generally form covalent bonds with these elements.
no none can
In combination with oxygen, silicon appears in large number of molecules. These include metal silicates in rocks such as feldspar and mica, and as silicon dioxide (silica) in sand, quartz, flint, and the gemstones amethyst and opal.
Oxygen and Silicon are elements in their own right. They do NOT contain aanything else. However, Silicon and Oxygen can combine to form the molecule 'Silicon Dioxide' ( SiO2 ), of which is sand on the beach is an impure form, mixed with oxides of other elements.
Carbon, Geranium, Tin, and Silicon. The reason for this is because all of these elements including Lead, have four valence electrons.
In addition to silicon and oxygen, silicate minerals usually contain other elements such as aluminum, magnesium, iron, or calcium. These elements combine with silicon and oxygen to form various types of silicate structures, giving rise to a wide range of silicate minerals in nature.
One is silicon, but I don't know the other:(oxygen
carbon is one of them, they are in the same column
Other elements
Various elements can combine with oxygen to form compounds, such as metals (e.g., iron, copper), nonmetals (e.g., sulfur, phosphorus), and metalloids (e.g., silicon). These elements can form oxides, peroxides, or other oxygen-containing compounds depending on their reactivity and valence states.
Oxygen is the element that can combine with almost all other elements.
Uranium combine with the majority of other elements; also uranium has alloys with the majority of metals.
The two most abundant elements in the Earth's crust are oxygen and silicon. When you combine them, you get silicon dioxide; which depending on the exact form it takes is glass or quartz or sand.They tend to combine further with other elements to produce silicate rocks.The two most abundant elements in Earth as a whole are iron and oxygen. When you combine them, you get iron oxide (rust, hematite, magnetite). The reason iron isn't more common in the crust than it is is that it's heavy and has been concentrated in the Earth's core.