Scientific
Notation: 1.4959789 x 108 km (1.000 A.U.)
Perihelion
(closest)
Metric:
147,100,000 km
English:
91,400,000 miles
Scientific
Notation: 1.471 x 108 km (0.983 A.U.)
Aphelion
(farthest)
Metric:
152,100,000 km
English:
94,500,000 miles
Scientific
Notation: 1.521 x 108 km (1.017 A.U.)
Equatorial
Radius
Metric:
6,378.14 km
English:
3,963.19 miles
Scientific
Notation: 6.37814 x 103 km
By Comparison:
1 x Earth's
Equatorial
Circumference
Metric:
40,075 km
English:
24,901 miles
Scientific
Notation: 4.0075 x 104 km
Volume
Metric:
1,083,200,000,000 km3
English:
259,900,000 mi3
Scientific
Notation: 1.0832 x 1012 km3
By Comparison:
1 x Earth's
Mass
Metric:
5,973,700,000,000,000,000,000,000 kg
Scientific
Notation: 5.9737 x 1024 kg
Density
Metric:
5.515 g/cm3
Surface
Area
Metric:
510,065,700 km2
English:
196,937,500 square miles
Scientific
Notation: 5.100657 x 108 km2
Equatorial
Surface Gravity
Metric:
9.766 m/s2
English:
32.041 ft/s2
Escape
Velocity
Metric:
40,248 km/h
English:
25,009 mph
Scientific
Notation: 11,180 m/s
Sidereal
Rotation Period (Length of Day)
0.99726968 Earth
days
23.934 hours
Sidereal
Orbit Period (Length of Year)
1.0000174 Earth
years
365.24 Earth days
Mean
Orbit Velocity
Metric:
107,229 km/h
English:
66,629 mph
Scientific
Notation: 29,785.9 m/s
Orbital
Eccentricity
0.01671022
Orbital
Inclination to Ecliptic
0.00005 degrees
Equatorial
Inclination to Orbit
23.45 degrees
Orbital
Circumference
Metric:
924,375,700 km
English:
574,380,400 miles
Scientific
Notation: 9.243757 x 108 km
Minimum/Maximum
Surface Temperature
Metric:
-88/58 (min/max) °C
English:
-126/136 (min/max) °F
Scientific
Notation: 185/331 (min/max) K
Atmospheric
Constituents
Nitrogen, Oxygen
Scientific
Notation: N2, O2
By Comparison:
N2 is 80% of Earth's air and is a crucial
element in DNA.
NASA:
Destination Earth Video
Earth is the third planet from
the Sun and the fifth largest in the solar system.
Earth's diameter is just a
few hundred kilometers larger than that of Venus. The four seasons are a result
of Earth's axis of rotation being tilted more than 23 degrees.
Visible Planet
Orbits
This diagram shows the relative size of the orbits of the seven planets visible
to the naked eye. All the orbits are nearly circular (but slightly elliptical)
and nearly in the same plane as Earth's orbit (called the ecliptic).
The diagram is from a view out of the ecliptic plane and away from the
perpendicular axis that goes through the Sun.
Image Credit: Lunar and Planetary Institute
Oceans at least 4 km deep cover
nearly 70 percent of Earth's surface. Fresh water exists in the liquid phase
only within a narrow temperature span (0 degrees to 100 degrees Celsius). This
temperature span is especially narrow when contrasted with the full range of
temperatures found within the solar system. The presence and distribution of
water vapor in the atmosphere is responsible for much of Earth's weather.
Near the surface, an ocean of air
that consists of 78 percent nitrogen, 21 percent oxygen, and 1 percent other
ingredients envelops us. This atmosphere affects Earth's long-term climate and
short-term local weather; shields us from nearly all harmful radiation coming
from the Sun; and protects us from meteors as well - most of which burn up
before they can strike the surface. Satellites have revealed that the upper
atmosphere actually swells by day and contracts by night due to solar activity.
Our planet's rapid spin and
molten nickel-iron core give rise to a magnetic field, which the solar wind
distorts into a teardrop shape. The solar wind is a stream of charged particles
continuously ejected from the Sun. The magnetic field does not fade off into
space, but has defi- nite boundaries. When charged particles from the solar wind
become trapped in Earth's magnetic field, they collide with air molecules above
our planet's magnetic poles. These air molecules then begin to glow and are
known as the aurorae, or the Northern and Southern Lights.
Credit:ESA
Earth's
land surfaces are also in motion. For example, the North American continent
continues to move west over the Pacific Ocean basin. Earthquakes result when plates grind past one
another, ride up over one another, collide to make mountains, or split and
separate. These movements are known as plate tectonics.
NASA
Image
Earth is the only planet
whose English name does not derive from Greek/Roman mythology. The name derives
from Old English and Germanic.
Earth's
Moon
NASA
Image
Earth has only one natural satellite, the Moon,
which is 384,000 km (211,265 miles) away.
Earth
has a modest magnetic field produced by electric currents in the outer core. The
Earth's magnetic field and its interaction with the solar wind also produce the
Van Allen radiation belts, a pair of doughnut shaped rings of ionized gas (or
plasma) trapped in orbit around the Earth.
The
outer belt stretches from 19,000 km in altitude to 41,000 km; the inner belt
lies between 13,000 km and 7,600 km in altitude.
The
magnetosphere is that area of space, around the Earth, that is controlled by the
Earth's magnetic field.The magnetosphere extends into the vacuum of space from
approximately 80 to 60,000 kilometers (50 to 37,280 miles) on the side toward
the Sun, and trails out more than 300,000 kilometers (186,500 miles) away from
the Sun.
Credit
UCAR
A
magnetosphere has many parts, such as the bow shock, magnetosheath, magnetotail,
plasmasheet, lobes, plasmasphere, radiation belts and many electric currents. It
is composed of charged particles and magnetic flux. These particles are
responsible for many wonderful natural phenomena such as the aurora and natural
radio emissions such as lion roars and whistler waves. The particles move and
circulate about the magnetosphere and even generate storms. The magnetosphere
changes constantly, even flipping its orientation every few thousand years.
Temperature
Records
Highest
Temperature: 136°F in
El Azizia, Libya on September 13, 1922
Lowest
Temperature: -129°F in
Vostok, Antarctica on July 21, 1983
Precipitation
Records
Greatest
12-Month: 1,042 inches
in Cherrapungi, India on August 1, 1860 - July 31, 1861
Lowest
Average Annual: 0.03
inches in Arica, Chile
Wettest
Location
467.4
inches per year in Mawsynram, India
463.4
inches per year in Tutunendo, Colombia
460
inches per year in Mount Waialeale, Kauai, Hawaii
Driest
Location
Arica,
Chile receives only 0.03 inches of rain annually
NASA
TERRA Satellite Global Vegetation Image
The Earth is 4.5 billion years old It is the home
of 6 Billion human beings and millions of species. Its is at least 4 1/2 billion
years old. It weighs 6.6 sextillion tons-6,000,000,000,000,000,000,000,000
(6E+24) kilograms.
Earth's
Layers
The
earth is divided into four main layers: the inner core, outer core, mantle, and
crust
0-
40 Crust
40-
400 Upper mantle
400-
650 Transition region
650-2700
Lower mantle
2700-2890
D'' layer
2890-5150
Outer core
5150-6378
Inner core
Earth's
crust is divided into several separate solid plates which float around
independently on top of the hot mantle below. The theory that describes this is
known as plate tectonics. In geologic terms, a plate is a large, rigid slab of
solid rock. The word tectonics comes from the Greek root "to build."
Putting these two words together, we get the
term plate tectonics, which refers
to how the Earth's surface is built of plates. The theory of plate tectonics
states that the Earth's outermost layer is fragmented into a dozen or more large
and small plates that are moving relative to one another as they ride atop
hotter, more mobile material. It is characterized by two major processes:
spreading and subduction. Spreading occurs when two plates move away from each
other and new crust is created by upwelling magma from below. Subduction occurs
when two plates collide and the edge of one dives beneath the other and
ends up
being destroyed in the mantle. There is also transverse motion at some plate
boundaries (i.e. the San Andreas Fault in California) and collisions between
continental plates (i.e. India/Eurasia).
There are eight major plates:
North American Plate - North
America, western North Atlantic and Greenland
South American Plate - South
America and western South Atlantic
Antarctic Plate - Antarctica
and the "Southern Ocean"
Eurasian Plate - eastern North
Atlantic, Europe and Asia except for India
African Plate - Africa,
eastern South Atlantic and western Indian Ocean
Indian-Australian Plate -
India, Australia, New Zealand and most of Indian Ocean
Nazca Plate - eastern Pacific
Ocean adjacent to South America
Pacific Plate - most of the
Pacific Ocean (and the southern coast of California)
NASA
TERRA Satellite North America Vegetation and Sea Surface Temperature Image
Tallest
Mountains
Mount
Everest 8850m (29035ft) Asia
Aconcagua
6959m (22831ft) S. America
Mount
McKinley 6194m (20320ft) N. America
Mount
Kilimanjaro 5963m (19563ft) Africa
Mount
Elbrus 5633m (18481ft) Europe
Puncak
Jaya 4884m (16023ft) Oceania
Vinson
Massif 4897m (16066ft) Antarctica
The Amazon
Rainforest is vanishing at 3 times the rate it
was in 1994.
About
20% of the Amazon
Rainforest is already obliterated
Global
emissions of carbon dioxide are expected to double or triple by the year 2030
The
U.S. wastes more energy yearly than is consumed by 2/3 of the World
In the World there are 70 million barrels of oil consumed daily of that 20
million are consumed by the United States
The
World's supply of oil will run out in about 80 years
40%
of the World's population has no access to electricity
The production of electricity is the number one source of air pollution
Credit:
NASA, EPA, USGS,University Corporation for Atmospheric Research
Data
compiled from The British Antarctic Study, NASA, Environment Canada,
UNEP, EPA and
other sources as stated and credited Researched by Charles
Welch-Updated dailyThis
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