A timeline of Earth's average temperature since the last Ice Age glaciation

Since the last ice age glaciation, which ended around 11,700 years ago, Earth's average temperature has undergone significant fluctuations.

During the early Holocene, temperatures rose rapidly, leading to the establishment of a warmer climate than today's. This period, known as the Holocene Climate Optimum, peaked around 6,000 to 9,000 years ago, with global temperatures possibly 1-2 degrees Celsius warmer than pre-industrial levels.

Following the Holocene Climate Optimum, temperatures gradually declined due to natural factors such as changes in Earth's orbit and solar output. This cooling trend culminated in the Little Ice Age, a period of colder-than-average temperatures that lasted from roughly the 14th to the mid-19th century. During this time, glaciers advanced in many parts of the world, and colder conditions prevailed.

A timeline of Earth's average temperature since the last Ice Age glaciation

Since the end of the Little Ice Age, Earth's average temperature has been increasing, a trend that has accelerated since the late 19th century due to human activities, particularly the burning of fossil fuels and deforestation. This period of rapid warming, often referred to as anthropogenic or human-induced global warming, has led to a significant increase in global average temperatures compared to pre-industrial levels. The past few decades have seen some of the warmest years on record, with impacts on ecosystems, weather patterns, and sea levels, highlighting the importance of addressing climate change through mitigation and adaptation measures.

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Find cities with similar climate

This map has been created using The Global environmental stratification. The Global environmental stratification (GEnS), based on statistical clustering of bioclimate data (WorldClim). GEnS, consists of 125 strata, which have been aggregated into 18 global environmental zones (labeled A to R) based on the dendrogram. Interactive map >> Via www.vividmaps.com Related posts: - Find cities with similar climate 2050 - How global warming will impact 6000+ cities around the world?

The Appalachian Mountains, the Scottish Highlands, and the Atlas Mounts in Africa were the same mountain range

The Central Pangean Mountains was a prominent mountain ridge in the central part of the supercontinent Pangaea that extends across the continent from northeast to southwest through the Carboniferous , Permian Triassic periods. The mountains were formed due to a collision within the supercontinents Gondwana and Laurussia during the creation of Pangaea. It was comparable to the present Himalayas at its highest peak during the start of the Permian period. It isn’t easy to assume now that once upon a time that the Scottish Highlands, The Appalachian Mountains, the Ouachita Mountain Range, and the Atlas Mountains in northwestern Africa are the same mountains , once connected as the Central Pangean Mountains.

Human Emotions Visualized

Despite significant diversity in the culture around the globe, humanity's DNA is 99.9 percent alike. There are some characteristics more primary and typical to the human experience than our emotions. Of course, the large spectrum of emotions we can feel can be challenging to verbalize. That's where this splendid visualization by the Junto Institute comes in. This visualization is the newest in an ongoing attempt to categorize the full range of emotions logically. Our knowledge has come a long route since William James suggested 4 primary emotions: fear, grief, love, and rage. These kernel emotions yet form much of the basis for current frameworks. The Junto Institute's visualization above classifies 6 basic emotions: fear, anger, sadness, surprise, joy, love More nuanced descriptions begin from these 6 primary emotions, such as jealousy as a subset of anger and awe-struck as a subset of surprise. As a result, there are 102 second-and third-order emotions placed on this emo

Ecoclimax

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