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Snowball Earth or Icehouse Earth refers to times when the Earth's surface was nearly or entirely frozen. The occurrence of Snowball (or Slushball) Earths... |
there many times the Earth was covered in ice sheets. (For example, the Cryogenian). This is called the Snowball Earth theory. Earth is rocky. It is the... |
cooling of the global climate around 700 million years ago (the so-called Snowball Earth of the Cryogenian period) and the rapid evolution of primitive life... |
severe and longest ice ages in geologic history. It was similar to the Snowball Earth ice ages that happened later, in the Neoproterozoic era. The glaciations... |
Rodinia and at the end of a global ice age (Snowball Earth). Throughout the early Palaeozoic, the Earth's landmass was broken up into a substantial number... |
the Earth had two great ice ages, the Sturtian and Marinoan glaciations. These ice ages were so severe they are sometimes called Snowball Earth. In the... |
The well-identified events were: Several glaciations, including the Snowball Earth during the Cryogenian period in the late Neoproterozoic. Rapid crustal... |
mya These two snowball earth events were previously put together as the Varangian glaciation. They covered much, possibly all, the Earth with ice. The... |
longer period: it included the whole of the Marinoan glaciation, of Snowball Earth fame. In other words, the Vendian included the last part of the Cryogenian... |
Kirschvink, Isaac A. Hilburn, and Cody Z. Nash (2005). "The Paleoproterozoic snowball Earth: A climate disaster triggered by the evolution of oxygenic photosynthesis"... |
methane, and caused the Huronian glaciation. This was perhaps the longest snowball Earth episode ever. Free oxygen has been an important part of the atmosphere... |
Ono, 2006 https://www.jstor.org/stable/20209693 The Palaeoproterozoic Snowball Earth: A climate disaster triggered by the evolution of oxygenic photosynthesis... |
glaciation (~2400 mya Earth completely covered in ice probably due to Great Oxygenation Event) Later Neoproterozoic Snowball Earth (~600 mya, precursor... |
populations crashed during the Cryogenian period 860 million years ago (the Snowball Earth episodes). They proliferated in the Cambrian explosion and reached their... |
this has partly been responsible for the present temperature rise. Snowball Earth Ice core Milankovitch cycle Orbital forcing Pleistocene Glaciation Global... |
Climate change (section Hot Earth) another one start?". Robert E. Kopp; et al. (2005). "The Paleoproterozoic snowball Earth: a climate disaster triggered by the evolution of oxygenic photosynthesis"... |
and the tail formed. These observations supported Fred Whipple's "dirty snowball" model. This correctly predicted that Halley would be composed of a mixture... |
animal fossils 580 million years - time since the end of a possible Snowball Earth ice age 703.8 million years - half-life of uranium-235 750 million years... |
that moves around in outer space. Comets are often described as "dirty snowballs". They are very different from asteroids. The orbital inclinations of... |
such as Earth, and streams of debris from a comet. Comets are dirty snowballs, made up of rock embedded in ice, orbiting the Sun. Each time a comet... |