Harpoon reaction

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Template:MarsGeo-Plains Planum Boreum (Latin: "the northern plain") is the northern polar plain on Mars. It extends northward from roughly 80°N and is centered at Template:Coord. Surrounding the high polar plain is a flat and featureless lowland plain called Vastitas Borealis which extends for approximately 1500 kilometres southwards, dominating the northern hemisphere.[1]

Ice cap

File:MRO image of Mars North Pole.jpg
False color Mars Reconnaissance Orbiter image of a side of the Chasma Boreale, a canyon in the polar ice cap. Light browns are layers of surface dust greys and blues are layers of water and carbon dioxide ice. Regular geometric cracking is indicative of higher concentrations of water ice.
File:PSP 001406 2680 ChasmaBoreale.jpg
HiRISE image of a crater in the north polar ice cap

Planum Boreum is home to a permanent ice cap consisting mainly of water ice (with a 1 m thick veneer of carbon dioxide ice during the winter).[2] It has a volume of 1.2 million cubic kilometres and covers an area equivalent to about 1.5 times the size of Texas. It has a radius of 600 km. The maximum depth of the cap is 3 km.[3]

The spiral troughs in the ice cap are formed by katabatic winds that entrain surface ice eroded from the equator-facing sides of the troughs, likely aided by solar ablation (sublimation), which is then redeposited on the colder pole-facing slopes. The troughs are roughly perpendicular to the wind direction, which is shifted by the Coriolis effect, leading to the spiral pattern.[4][5] The troughs gradually migrate towards the pole over time; the central troughs have moved about 65 km in the last 2 million years.[4] Chasma Boreale is a canyon-like feature older than the troughs, and in contrast is aligned parallel to the wind direction.[4]

The surface composition of the northern ice cap in middle spring (after a winter's accumulation of seasonal dry ice) has been studied from orbit. The outer edges of the ice cap are contaminated with dust (0.15% by weight) and are mostly water ice. As one moves toward the pole, the surface water ice content decreases and is replaced by dry ice. The purity of the ice also increases. At the pole, the surface seasonal ice consists of essentially pure dry ice with little dust content and 30 parts per million of water ice.[6]

The Phoenix lander, launched in 2007, arrived at Mars in May 2008 and successfully landed in the Vastitas Borealis region of the planet on May 25, 2008. The north polar cap of Mars has been proposed as a landing site for a human Mars expedition by Landis[7] and by Charles Cockell[8] 50 year old Petroleum Engineer Kull from Dawson Creek, spends time with interests such as house brewing, property developers in singapore condo launch and camping. Discovers the beauty in planing a trip to places around the entire world, recently only coming back from .

Features

File:PoloNorteMarteTopologico.png
Elevation map of the north pole. Note how Planum Boreum soars above the surrounding featureless terrain. Click to enlarge and for more info.

The main feature of the Planum Boreum is a large fissure or canyon in the polar ice cap called Chasma Boreale. It is up to Template:Convert wide and features scarps up to Template:Convert high.[9][10] By comparison, the Grand Canyon is approximately Template:Convert deep in some places and Template:Convert long but only up to Template:Convert wide. Chasma Boreale cuts through polar deposits and ice, such as those present at Greenland.

Planum Boreum interfaces with Vastitas Borealis west of Chasma Boreale at an irregular scarp named Rupes Tenuis. This scarp reaches heights of up to 1 km. At other places, the interface is a collection of mesas and troughs.

Planum Boreum is surrounded by large fields of sand dunes spanning from 75°N to 85°N. These dune fields are named Olympia Undae, Abalos Undae and Hyperboreae Undae. Olympia Undae, by far the largest, covers from 100°E to 240°E. Abalos Undae covers from 261°E to 280°E and Hyperboreale Undae spans from 311°E to 341°E.[11] See also List of extraterrestrial dune fields.

Avalanches

File:Mars avalanche Feb 19.jpg
False color view of a Martian avalanche.

A February 2008 HiRISE observation captured four avalanches in progress off a Template:Convert cliff. The cloud of fine material is Template:Convert across and extends Template:Convert from the base of the cliff. The reddish layers are known to be rock rich in water ice while the white layers are seasonal carbon dioxide frost. The landslide is thought to have originated from the uppermost red layer. Follow-up observations are planned to characterize the nature of the landslide debris.[12][13] 50 year old Petroleum Engineer Kull from Dawson Creek, spends time with interests such as house brewing, property developers in singapore condo launch and camping. Discovers the beauty in planing a trip to places around the entire world, recently only coming back from .

Repeating annular cloud

File:Mars cyclone.jpg
Hubble view of the colossal polar cloud on Mars

A large doughnut shaped cloud appears in North polar region of Mars around the same time every Martian year and of about the same size.[14] It forms in the morning, dissipates by the Martian afternoon.[14] The outer diameter of the cloud is roughly Template:Convert, and the inner hole or eye is Template:Convert across.[15] The cloud is thought to be composed of water-ice,[15] so it is white in color, unlike the more common dust storms.

It looks like a cyclonic storm, similar to hurricane, but it does not rotate.[14] The cloud appears during the northern summer and at high latitude. Speculation is that this is due to unique climate conditions near the northern pole.[15] Cyclone-like storms were first detected during the Viking orbital mapping program, but the northern annular cloud is nearly three times larger.[15] The cloud has also been detected by various probes and telescopes including the Hubble and Mars Global Surveyor.[14][15]

When Hubble Space Telescope viewed it in 1999, it was thought to be cyclonic storm. The diameter was measured to be approximately 1750 km, and featured an "eye" 320 km in diameter.[16]

See also

References

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  1. [5] and [6] give Vastitas Borealis starting at 54.7°N and Planum Boreum at 78.5°N. The radius of Mars is approximately 3400 km, so d=78.554.7360×2π ×3400 km=1412 km
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  4. 4.0 4.1 4.2 One of the biggest reasons investing in a Singapore new launch is an effective things is as a result of it is doable to be lent massive quantities of money at very low interest rates that you should utilize to purchase it. Then, if property values continue to go up, then you'll get a really high return on funding (ROI). Simply make sure you purchase one of the higher properties, reminiscent of the ones at Fernvale the Riverbank or any Singapore landed property Get Earnings by means of Renting

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    Discover out more about real estate funding in the area, together with info on international funding incentives and property possession. Many Singaporeans have been investing in property across the causeway in recent years, attracted by comparatively low prices. However, those who need to exit their investments quickly are likely to face significant challenges when trying to sell their property – and could finally be stuck with a property they can't sell. Career improvement programmes, in-house valuation, auctions and administrative help, venture advertising and marketing, skilled talks and traisning are continuously planned for the sales associates to help them obtain better outcomes for his or her shoppers while at Knight Frank Singapore. No change Present Rules

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    The data offered is for normal info purposes only and isn't supposed to be personalised investment or monetary advice. Motley Fool Singapore contributor Stanley Lim would not personal shares in any corporations talked about. Singapore private home costs increased by 1.eight% within the fourth quarter of 2012, up from 0.6% within the earlier quarter. Resale prices of government-built HDB residences which are usually bought by Singaporeans, elevated by 2.5%, quarter on quarter, the quickest acquire in five quarters. And industrial property, prices are actually double the levels of three years ago. No withholding tax in the event you sell your property. All your local information regarding vital HDB policies, condominium launches, land growth, commercial property and more

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  7. G. Landis, Polar Landing Site for a First Mars Expedition Founding Convention of the Mars Society, August 13–16, 1998, University of Colorado in Boulder, CO
  8. Project Boreas C. Cockell (editor), Project Boreas - A Station for the Martian Geographic North Pole, The British Interplanetary Society (2006)
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  14. 14.0 14.1 14.2 14.3 Mars Global Surveyor - "8 Year Anniversary"
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