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The Holocene thermal maximum, which occurred around 9,000 to 5,000 years ago, was mainly caused by changes in Earth's orbital parameters leading to an increase in summer insolation at high latitudes. This led to global warming during the early to mid-Holocene period. Additionally, factors such as greenhouse gas concentrations and feedback mechanisms may have contributed to this warming trend.

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What statement best describes the altithermal period?

The altithermal period, also known as the mid-Holocene thermal maximum, was a warm period that occurred around 7,000 to 5,000 years ago during the Holocene epoch. It was characterized by higher temperatures and changes in climate patterns, leading to shifts in ecosystems and human adaptations. This period played a role in shaping landscapes and influencing human societies.


What is the name given to the current geological epoch?

The current geological epoch is called the Holocene epoch. It began approximately 11,700 years ago and continues to the present day.


What is the opposite of the ice age?

The geo-historic opposite of the Ice Ages (maximum glaciation) would be the periods of higher temperatures such as the Cretaceous Thermal Maximum (65 to 100 million years ago) and the Paleocene-Eocene Thermal Maximum (peaking about 55 million years ago).


The current interglacial period is known as?

The current interglacial period is known as the Holocene epoch, which began about 11,700 years ago after the last major glacial period. It is characterized by relatively stable climate conditions compared to the glacial periods.


What eventually causes a thermal to dissipate?

Thermal dissipation occurs when the heat energy stored in an object (such as a heated material or component) is transferred to its surroundings, resulting in a decrease in temperature. This transfer of heat can happen through conduction, convection, or radiation, allowing the object to return to thermal equilibrium with its surroundings.