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John Dalton lived between September 6,1766 and July 27,1844

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What period of time did john Dalton live?

18th century


How old is John Dalton?

John Dalton was born on September 6, 1766 and died on July 27, 1844. John Dalton would have been 77 years old at the time of death or 248 years old today.


Did john wesley live during the Renaissance?

Yes, John Wesley was alive during the Renaissance time period.


How did John Dalton investigate atomic theory?

Experiments in the atomic structure were not possible in the time of Dalton. Intuition played an important role.


Who is Harvard all time leading rusher?

Kevin Faulk. Dalton Hilliard is second.


Why was John Dalton's model accepted?

John Dalton's atomic theory was accepted because it provided a simple and elegant explanation for chemical reactions and the law of definite proportions, which were consistent with experimental observations at the time. Additionally, Dalton's theory was supported by quantitative evidence, such as his work on combining gas volumes in reactions.


What approximate time in history was John Dalton in?

18th century. To be exact September 6, 1766


John Dalton used a scanning tunneling microscope to observe individual atoms?

This statement is incorrect. John Dalton was a British scientist known for developing the atomic theory in the early 19th century. The scanning tunneling microscope was invented much later, in 1981 by Gerd Binnig and Heinrich Rohrer.


What time period did the Bachipods live in?

Ordovician Period


What time period did iguanodon live in?

Cretaceous period,


What time period did ankylosaurs live?

Cretaceous period


What time period were Dalton theories made?

John Dalton's atomic theories were primarily developed in the early 19th century, with his seminal work published in 1803. His ideas laid the groundwork for modern chemistry by proposing that matter is composed of indivisible atoms and that these atoms combine in specific ratios to form compounds. Dalton's theories significantly advanced scientific understanding of atomic structure and chemical reactions during the early 1800s.