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Inner core
Earth was discovered to have a solid inner core distinct from its liquid outer core in 1936, by the seismologist Inge Lehmann, who deduced its presence from observations of earthquake-generated seismi ...
category:    2014-7-12 22:00
Structure of the Earth
The force exerted by Earth's gravity can be used to calculate its mass, and by estimating the volume of the Earth, its average density can be calculated. Astronomers can also calculate Earth's mass fr ...
category:    2014-7-12 21:59
Arctic ice pack
Sea ice helps to constrain methane in permafrost and in clathrates. Arctic methane release triggered by a breakdown in sea ice could cause an abrupt climate change event, potentially similar in some w ...
category:    2014-7-12 21:57
Antarctic ice sheet
The icing of Antarctica began with ice-rafting from middle Eocene times about 45.5 million years ago and escalated inland widely during the Eocene–Oligocene extinction event about 34 million years ag ...
category:    2014-7-12 21:55
Geographical pole
A geographical pole (also known as a geographic pole) is either of the two points on a planet, moon or other relatively large rotating body where the body's axis of rotation meets its surface. As with ...
category:    2014-7-12 21:53
Geologic time scale
The largest defined unit of time is the supereon, composed of eons. Eons are divided into eras, which are in turn divided into periods, epochs and ages. The terms eonothem, erathem, system, series, an ...
category:    2014-7-12 21:51
Lithosphere
In the Earth, the lithosphere includes the crust and the uppermost mantle, which constitute the hard and rigid outer layer of the Earth. The lithosphere is underlain by the asthenosphere, the weaker, ...
category:    2014-7-12 21:50
Geological history of Earth
The Precambrian includes approximately 90% of geologic time. It extends from 4.6 billion years ago to the beginning of the Cambrian Period (about 541 Ma). It includes three eons, the Hadean, Archean, ...
category:    2014-7-12 21:48
Gravity of Earth
The gravitational pull of the Moon and Sun give rise to two high tides and two low tides every lunar day, or every 24 hours and 50 minutes. Therefore, there is a gap of 12 hours and 25 minutes between ...
category:    2014-7-12 21:45
Super-Earths in the habitable zone.
The 2007 discovery of Gliese 581 c, the first super-Earth in the circumstellar habitable zone, created significant interest in the system by the scientific community, although the planet was later fou ...
category:    2014-7-12 21:43
Circumstellar habitable zone
The concept of a Circumstellar Habitable Zone was first introduced in 1953 by Hubertus Strughold, who in his treatise The Green and the Red Planet: A Physiological Study of the Possibility of Life on ...
category:    2014-7-12 21:42
Sunlight
Sunlight may be recorded using a sunshine recorder, pyranometer, or pyrheliometer.Sunlight takes about 8.3 minutes to reach the Earth from the surface of the Sun. A photon starting at the centre of th ...
category:    2014-7-12 21:40
Dynamo theory
The Earth's magnetic field is believed to be generated by electric currents in the conductive material of its core, created by convection currents due to heat escaping from the core. However the proce ...
category:    2014-7-12 21:38
Earth's magnetic field
Earth's magnetic field serves to deflect most of the solar wind, whose charged particles would otherwise strip away the ozone layer that protects the Earth from harmful ultraviolet radiation. One stri ...
category:    2014-7-12 21:36
Ozone layer
The photochemical mechanisms that give rise to the ozone layer were discovered by the British physicist Sydney Chapman in 1930. Ozone in the Earth's stratosphere is created by ultraviolet light striki ...
category:    2014-7-12 21:35

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