They are arranged differently.
Graphite forms in thin layers. Imagine a stack of thin papers. Every time you press down on a pencil, a few layers rub off onto the surface you are writing on and stay there.
Diamonds, on the other hand, form in much stronger and complex forms, which are almost impossible to break. This makes it one of the strongest substances on Earth.
similarities -- all are forms of carbon differences -- because of the structures of the bonds of the carbon atoms, they have different properties
This explanation is not correct.
Diamonds and graphite are both allotropes of carbon.
composition
composition
because they are of allotropes of carbon.
Everything has 'properties' used to identify the object/ item/ mineral/ material.
Graphite has a layered structure: the bonds between carbon atoms are covalent and the bonds between layers are weak van der Waals bonds.Diamonds have a face centered cubic diamond lattice which is very rigid.Differences in structure explain differences of physical properties.
No. Both graphite and diamond are allotropes of carbon. They have different molecular structures.
Diamonds, coke, coal, graphite, fullerenes
similarities -- all are forms of carbon differences -- because of the structures of the bonds of the carbon atoms, they have different properties
This explanation is not correct.
No. Graphite and diamond are both allotropes of carbon, each with a different and distinct molecular structure.
Diamonds and graphite are both allotropes of carbon.
No. They are actually a type of graphite. Diamonds are made of carbon.
Both graphite and diamond are composed of the element carbon, but have different crystalline structures.
Graphite and diamonds are both network covalent carbon chains. The only difference is the structure of each. Graphite is very soft and is used as a lubricant, due to the fact that its carbon atoms are bonded together in layers which slide apart easily. Diamond, however, is very abrasive, because its carbons are all bonded to each other in a very rigid fashion.