John Dalton was an English scientist born in 1766 who is considered the founder of modern atomic theory. He proposed that all matter is composed of small indivisible particles called atoms and that different atoms have different weights. His atomic theory included the ideas that atoms of a given element are all identical, atoms cannot be created, destroyed, or divided, and atoms combine in simple whole number ratios to form chemical compounds. Dalton's atomic theory was groundbreaking and laid the foundation for modern chemistry, though some of his specific assumptions, like his rule of simplest composition, were later found to be incorrect. He made many contributions in the fields of mathematics, meteorology, and gas behavior.