Hypertherm

Hypertherm is a term used in history to describe a period when the Earth's temperature was higher than it is today. At that time, the climate was hotter and more humid, which contributed to the development of life on Earth.

Hyperthermia began about 350 million years ago and ended about 200 million years ago. During this period, many changes occurred on Earth that affected life and the environment. For example, the first plants and animals appeared, and the first oceans began to develop.

One of the main factors that led to hyperthermia was an increase in the amount of carbon dioxide in the atmosphere. This caused the Earth's temperature to rise and precipitation to increase. Climate change has also been associated with changes in the Earth's orbit around the Sun.

Overall, hyperthermia was an important period in Earth's history that led to the development of life and environmental changes. However, we are now living in a period where global warming is leading to even greater climate change, which could have serious consequences for our planet in the future.