Q.An example of amorphous solid is

Crystalline and Amorphous Solids

Imagine you are in a school assembly. All students stand in neat rows and columns — every person knows exactly where to stand, and the pattern repeats across the entire ground. That is a crystalline solid. Now imagine a crowded market: people are packed together, but there is no fixed arrangement; everyone is just wherever they happen to be. That is an amorphous solid.

The difference is not about how tightly packed the particles are — both types can be dense. It is about order.

Crystalline Solids: The Ordered World

In a crystalline solid, atoms, ions, or molecules are arranged in a regular, repeating three-dimensional pattern that extends throughout the entire material. This pattern is called a crystal lattice. Because of this long-range order, every unit cell is identical to its neighbour, and the arrangement repeats for millions of atomic distances.

This order has two immediate consequences you can observe:

• Sharp melting point. When you heat a crystal, every bond is identical to every other bond. So all bonds break at exactly the same temperature — the solid turns into a liquid at one precise temperature, not over a range.
• Cleavage into smooth planes. If you break a crystal, it tends to split along flat surfaces because the planes of atoms are neatly stacked. Think of how a diamond (crystalline carbon) can be cut into facets.

Examples: sodium chloride (table salt), diamond, quartz, ice, and most metals.

Amorphous Solids: The Disordered World

An amorphous solid has no long-range order. The particles are arranged randomly, much like in a liquid. In fact, you can think of an amorphous solid as a supercooled liquid — a liquid that was cooled so quickly that its molecules did not get a chance to arrange themselves into a crystal before they froze.

Because there is no repeating pattern, the bonds between particles are not all identical. Some are stronger, some weaker. This leads to:

• No sharp melting point. As you heat an amorphous solid, the weaker bonds break first, then the stronger ones later. So the material softens gradually over a range of temperatures — it does not melt at one specific temperature. This is why glass can be blown and shaped while hot; it becomes soft and pliable over a range, not suddenly liquid.
• Irregular fracture. When broken, amorphous solids do not split along flat planes. Instead, they produce curved, shell-like surfaces (conchoidal fracture). Think of how a glass bottle breaks — it shatters into curved, jagged pieces, not flat cubes.

Examples: glass, rubber, plastic, wax, and amorphous silica.

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