We are currently in the cenozoic period.
A period of one hundred thousand years is called a "hectocentury." In geological and paleoclimatic contexts, this timescale is often relevant for studying climate cycles and major geological events.
The current geological epoch is called the Holocene epoch. It began approximately 11,700 years ago and continues to the present day.
The current period is the Quaternary. It began 2.588 million years ago. The Quaternary is the third geological period in the Cenozoic era.
The Holocene period began approximately 11,700 years ago and continues to the present day. It is the current geological epoch and follows the Pleistocene epoch.
The geological time scale organizes a long period of time.
Its called, as it says in latin, "modernictus", though for us it is modernism
The time period between ice ages is called an interglacial period. This is a geological term referring to the warmer periods between glaciations when ice sheets retreat and temperatures are generally warmer.
Its called, as it says in latin, "modernictus", though for us it is modernism
The geological process that transforms mountains that were once trees into their current form is called tectonic uplift. This process involves the movement of Earth's crust, which can push up and reshape the landscape over millions of years.
IT encompasses all of the geological time period that have happened since the begin of time
period costs
Its called, as it says in latin, "modernictus", though for us it is modernism