Difference between revisions of "Planets"
m (Clarification) |
(Add images/icons and alpha-sort planet sections) |
||
Line 6: | Line 6: | ||
Planets are present in every solar system in EVE. The vast majority are uninhabited. Planetary Interaction introduced in the [http://www.eveonline.com/tyrannis/ Tyrannis] expansion allows players to utilize the planets in EVE to mine and produce goods in the first step in linking EVE with the upcoming DUST 514. Each planet type has 5 resources available to it to be mined via [[Planetary Interaction]]. Resources that only appear on one planet type appear in <font color=green>green</font>. | Planets are present in every solar system in EVE. The vast majority are uninhabited. Planetary Interaction introduced in the [http://www.eveonline.com/tyrannis/ Tyrannis] expansion allows players to utilize the planets in EVE to mine and produce goods in the first step in linking EVE with the upcoming DUST 514. Each planet type has 5 resources available to it to be mined via [[Planetary Interaction]]. Resources that only appear on one planet type appear in <font color=green>green</font>. | ||
− | =Types of planets= | + | = Types of planets = |
− | ==Gas== | + | |
+ | == Barren == | ||
+ | |||
+ | <table><tr><td> | ||
+ | Barren planets are archetypical "dead terrestrials": dry, rocky worlds with a minimal atmosphere and an unremarkable composition. They are commonly etched with flood channels, which are often broad enough to be visible from orbit; most such worlds have accumulated significant quantities of ice over their lifetimes, but cannot retain it on their surface. Generally surface liquid evaporates rapidly, contributing to the thin atmosphere, but occasionally it will seep back into the ground and refreeze, ready for another breakout in future when the local temperature rises. | ||
+ | |||
+ | '''Resources''' | ||
+ | *Aqueous Liquids | ||
+ | *Base Metals | ||
+ | *Carbon Compounds | ||
+ | *Micro Organisms | ||
+ | *Noble Metals | ||
+ | </td><td> | ||
+ | |||
+ | [[File:BarrenLarge.png]] | ||
+ | |||
+ | </td></tr></table> | ||
+ | |||
+ | |||
+ | == Gas == | ||
+ | |||
+ | <table><tr><td> | ||
Gas planets are characterized by a deep, opaque upper atmosphere, usually composed primarily of light elements such as hydrogen or helium. Simple chemicals can add a range of hues and shades in the visual spectrum, and the interaction between upwellings and rapidly circulating pressure bands result in a huge variety of visible surface structures. A similar level of diversity can be found beneath the cloud-tops: the inner composition of a given gas planet might belong to any one of a dozen broad groups, with no two planets entirely alike in this regard. | Gas planets are characterized by a deep, opaque upper atmosphere, usually composed primarily of light elements such as hydrogen or helium. Simple chemicals can add a range of hues and shades in the visual spectrum, and the interaction between upwellings and rapidly circulating pressure bands result in a huge variety of visible surface structures. A similar level of diversity can be found beneath the cloud-tops: the inner composition of a given gas planet might belong to any one of a dozen broad groups, with no two planets entirely alike in this regard. | ||
Line 20: | Line 41: | ||
Resources on a Gas planet will typically be found in narrow bands running east-west at various latitudes. Base metals are generally in bands around the equator, Aqueous Liquids and Ionic Solutions in mid-latitudes bands, with the Noble Gas near the poles. Reactive Gas will be found in small pockets at all latitudes. | Resources on a Gas planet will typically be found in narrow bands running east-west at various latitudes. Base metals are generally in bands around the equator, Aqueous Liquids and Ionic Solutions in mid-latitudes bands, with the Noble Gas near the poles. Reactive Gas will be found in small pockets at all latitudes. | ||
− | ==Ice== | + | </td><td> |
+ | |||
+ | [[File:GasLarge.png]] | ||
+ | |||
+ | </td></tr></table> | ||
+ | |||
+ | |||
+ | == Ice == | ||
+ | |||
+ | <table><tr><td> | ||
The majority of icy planets went through a period of being barren terrestrials, before being surfaced with ice over the course of many millennia. The exact process for this varies from case to case, but the end result is both common and visually uniform - a bright, reflective planet scored by countless fractures and crevasses. A few icy planets are hypothesized to have been warmer, liquid-bearing planets in the past that have subsequently frozen, as a result of either stellar cooling or failed terraforming projects. | The majority of icy planets went through a period of being barren terrestrials, before being surfaced with ice over the course of many millennia. The exact process for this varies from case to case, but the end result is both common and visually uniform - a bright, reflective planet scored by countless fractures and crevasses. A few icy planets are hypothesized to have been warmer, liquid-bearing planets in the past that have subsequently frozen, as a result of either stellar cooling or failed terraforming projects. | ||
Line 32: | Line 62: | ||
Ice planets typically have high amounts of Heavy Metals and Aqueous Liquids available. Micro Organisms and Noble Gas are less abundant, with Planktic Colonies being somewhat thin. Aqueous Liquids tends to be found more in the polar regions of Ice planets, Planktic Colonies in the temperate latitudes and Micro Organisms in the equatorial regions. Noble Gas and Heavy Metals are more randomly distributed with Heavy Metals more towards the equator and Noble Gas more towards the poles but with large areas of overlap and intermingling. | Ice planets typically have high amounts of Heavy Metals and Aqueous Liquids available. Micro Organisms and Noble Gas are less abundant, with Planktic Colonies being somewhat thin. Aqueous Liquids tends to be found more in the polar regions of Ice planets, Planktic Colonies in the temperate latitudes and Micro Organisms in the equatorial regions. Noble Gas and Heavy Metals are more randomly distributed with Heavy Metals more towards the equator and Noble Gas more towards the poles but with large areas of overlap and intermingling. | ||
− | + | </td><td> | |
− | |||
− | + | [[File:IceLarge.png]] | |
− | |||
− | |||
− | |||
− | |||
− | |||
− | + | </td></tr></table> | |
− | |||
− | |||
− | + | == Lava == | |
− | |||
− | |||
− | |||
− | |||
− | |||
− | + | <table><tr><td> | |
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
− | |||
So-called "lava planets" (properly "magmatic planets") fall into one of three groups: solar magmatics, which orbit sufficiently close to their star that the surface never cools enough to solidify; gravitational magmatics, which experience gravitational shifts sufficiently strong to regularly and significantly fracture cooling crusts; and magmatoids, which are for largely-unexplained reasons simply incapable of cooling and forming a persistent crust. All three types generally exhibit the same external phenomena - huge red-orange lava fields being a defining feature - but the latter two types are sometimes capable of briefly solidifying for a period measured in years or perhaps decades. | So-called "lava planets" (properly "magmatic planets") fall into one of three groups: solar magmatics, which orbit sufficiently close to their star that the surface never cools enough to solidify; gravitational magmatics, which experience gravitational shifts sufficiently strong to regularly and significantly fracture cooling crusts; and magmatoids, which are for largely-unexplained reasons simply incapable of cooling and forming a persistent crust. All three types generally exhibit the same external phenomena - huge red-orange lava fields being a defining feature - but the latter two types are sometimes capable of briefly solidifying for a period measured in years or perhaps decades. | ||
Line 76: | Line 83: | ||
*Consumer Electronics | *Consumer Electronics | ||
− | ==Oceanic== | + | </td><td> |
+ | |||
+ | [[File:LavaLarge.png]] | ||
+ | |||
+ | </td></tr></table> | ||
+ | |||
+ | |||
+ | == Oceanic == | ||
+ | |||
+ | <table><tr><td> | ||
Oceanic worlds are a class of terrestrial world covered entirely by liquids, usually in the form of mundane water. While the liquid surface is exceptionally smooth, the ocean floor on most worlds of this type exhibits significant topographic variety. It is this subsurface irregularity which causes the formation of complex weather systems, which would otherwise revert to more uniform patterns. | Oceanic worlds are a class of terrestrial world covered entirely by liquids, usually in the form of mundane water. While the liquid surface is exceptionally smooth, the ocean floor on most worlds of this type exhibits significant topographic variety. It is this subsurface irregularity which causes the formation of complex weather systems, which would otherwise revert to more uniform patterns. | ||
Line 86: | Line 102: | ||
*Planktic Colonies | *Planktic Colonies | ||
− | ==Plasma== | + | </td><td> |
+ | |||
+ | [[File:OceanicLarge.png]] | ||
+ | |||
+ | </td></tr></table> | ||
+ | |||
+ | |||
+ | == Plasma == | ||
+ | |||
+ | <table><tr><td> | ||
The aptly-named "plasma planets" have captured the imagination of countless artists and inspired innumerable works, yet the physics behind them are surprisingly mundane by cosmological standards. A rocky terrestrial with the right kind of atmosphere and magnetic field will, when bombarded with solar radiation, generate sprawling plasma storms as specific atmospheric elements are stripped of their electrons. Over time these storms will generally scorch the surface rock black, adding to the visual impact. | The aptly-named "plasma planets" have captured the imagination of countless artists and inspired innumerable works, yet the physics behind them are surprisingly mundane by cosmological standards. A rocky terrestrial with the right kind of atmosphere and magnetic field will, when bombarded with solar radiation, generate sprawling plasma storms as specific atmospheric elements are stripped of their electrons. Over time these storms will generally scorch the surface rock black, adding to the visual impact. | ||
Line 98: | Line 123: | ||
Compared to some other planet types, the resources on Plasma planets tend to be somewhat anemic but evenly distributed across all five types. Unlike Gas planets, there are few guidelines on where you will find concentrations of resources. Distribution of resources is very chaotic. | Compared to some other planet types, the resources on Plasma planets tend to be somewhat anemic but evenly distributed across all five types. Unlike Gas planets, there are few guidelines on where you will find concentrations of resources. Distribution of resources is very chaotic. | ||
− | ==Shattered== | + | </td><td> |
+ | |||
+ | [[File:PlasmaLarge.png]] | ||
+ | |||
+ | </td></tr></table> | ||
+ | |||
+ | |||
+ | == Storm == | ||
+ | |||
+ | <table><tr><td> | ||
+ | Storm worlds are usually considered terrestrial planets, although to a casual eye they may appear more similar to gas planets, given their opaque, high-pressure atmospheres. Geomorphically, however, the distinctions are clear: compared to a gas world, the atmosphere of a storm world is usually considerably shallower, and generally composed primarily of more complex chemicals, while the majority of the planet's mass is a rocky terrestrial ball. Their name is derived from the continent-scale electrical storms that invariably flash through their upper atmospheres. | ||
+ | |||
+ | '''Resources''' | ||
+ | *Aqueous Liquids | ||
+ | *Base Metals | ||
+ | *Ionic Solutions | ||
+ | *Noble Gas | ||
+ | *Suspended Plasma | ||
+ | |||
+ | Storm planets tend to have equal amounts of Aqueous Liquids, Base Metals and Suspended Plasma in decent amounts, with Noble Gas running a close 4th and Ionic Solutions as a distant 5th and somewhat sparse. Ionic Solutions tend to be distributed in the middle latitudes, Noble Gas anywhere but the equator and Suspended Plasma tending towards the equatorial regions. Aqueous Liquids and Base Metals will appear on broad swaths across all latitudes in giant swirling patterns. | ||
+ | |||
+ | </td><td> | ||
+ | |||
+ | [[File:StormLarge.png]] | ||
+ | |||
+ | </td></tr></table> | ||
+ | |||
+ | |||
+ | == Temperate == | ||
+ | |||
+ | <table><tr><td> | ||
+ | Life-bearing worlds are often referred to as "temperate", as their mild temperatures are one of their defining features. Planets with existing, stable ecosystems are prime targets for colonization efforts as they are generally easier to make fully habitable; as a result, the majority of highly populated worlds are of this type. Indeed, it is not altogether uncommon for detailed surveys to reveal signs of previous settlements from various stages of [[New_Eden|New Eden]]'s history. | ||
+ | |||
+ | '''Resources''' | ||
+ | *Aqueous Liquids | ||
+ | *<font color=green>Autotrophs</font> (unique) | ||
+ | *Carbon Compounds | ||
+ | *Complex Organisms | ||
+ | *Micro Organisms | ||
+ | |||
+ | </td><td> | ||
+ | |||
+ | [[File:TemperateLarge.png]] | ||
+ | |||
+ | </td></tr></table> | ||
+ | |||
+ | |||
+ | == Shattered == | ||
+ | |||
Shattered worlds were once terrestrial planets, torn asunder by some immense cataclysm. All such worlds in the [[New_Eden|New Eden]] cluster are products of the disastrous stellar events that occurred during the "Seyllin Incident". However, reports continue to circulate of similar planets discovered in the unmapped systems reached exclusively through unstable [[Wormholes|wormholes]]. How these met their fate, if indeed they exist at all, is unknown. | Shattered worlds were once terrestrial planets, torn asunder by some immense cataclysm. All such worlds in the [[New_Eden|New Eden]] cluster are products of the disastrous stellar events that occurred during the "Seyllin Incident". However, reports continue to circulate of similar planets discovered in the unmapped systems reached exclusively through unstable [[Wormholes|wormholes]]. How these met their fate, if indeed they exist at all, is unknown. | ||
'''Resources''' | '''Resources''' | ||
*None | *None | ||
+ | |||
=Resource Distribution by Planet Type= | =Resource Distribution by Planet Type= | ||
Line 125: | Line 199: | ||
| <br /> Suspended<br />Plasma | | <br /> Suspended<br />Plasma | ||
|- valign="top" | |- valign="top" | ||
− | | width="72" | Gas | + | | width="72" | [[File:GasIcon.png]] Gas |
| width="16" bgcolor="#c0c0c0" | <br /> | | width="16" bgcolor="#c0c0c0" | <br /> | ||
| width="100" | <br /> | | width="100" | <br /> | ||
Line 142: | Line 216: | ||
| <br /> | | <br /> | ||
|- valign="top" | |- valign="top" | ||
− | | width="72" | Ice | + | | width="72" | [[File:IceIcon.png]] Ice |
| width="16" bgcolor="#c0c0c0" | <br /> | | width="16" bgcolor="#c0c0c0" | <br /> | ||
| width="100" | <br /> | | width="100" | <br /> | ||
Line 159: | Line 233: | ||
| <br /> | | <br /> | ||
|- valign="top" | |- valign="top" | ||
− | | width="72" | Storm | + | | width="72" | [[File:StormIcon.png]] Storm |
| width="16" bgcolor="#c0c0c0" | <br /> | | width="16" bgcolor="#c0c0c0" | <br /> | ||
| width="100" | <br /> | | width="100" | <br /> | ||
Line 176: | Line 250: | ||
| bgcolor="#c0c0c0" | <br /> | | bgcolor="#c0c0c0" | <br /> | ||
|- valign="top" | |- valign="top" | ||
− | | width="72" | Barren | + | | width="72" | [[File:BarrenIcon.png]] Barren |
| width="16" bgcolor="#c0c0c0" | <br /> | | width="16" bgcolor="#c0c0c0" | <br /> | ||
| width="100" | <br /> | | width="100" | <br /> | ||
Line 193: | Line 267: | ||
| <br /> | | <br /> | ||
|- valign="top" | |- valign="top" | ||
− | | width="72" | Temperate | + | | width="72" | [[File:TemperateIcon.png]] Temperate |
| width="16" bgcolor="#c0c0c0" | <br /> | | width="16" bgcolor="#c0c0c0" | <br /> | ||
| width="100" bgcolor="green" | <br /> | | width="100" bgcolor="green" | <br /> | ||
Line 210: | Line 284: | ||
| <br /> | | <br /> | ||
|- valign="top" | |- valign="top" | ||
− | | width="72" | Lava | + | | width="72" | [[File:LavaIcon.png]] Lava |
| width="16" | <br /> | | width="16" | <br /> | ||
| width="100" | <br /> | | width="100" | <br /> | ||
Line 227: | Line 301: | ||
| bgcolor="#c0c0c0" | <br /> | | bgcolor="#c0c0c0" | <br /> | ||
|- valign="top" | |- valign="top" | ||
− | | width="72" | Oceanic<br /> | + | | width="72" | [[File:OceanicIcon.png]] Oceanic<br /> |
| width="16" bgcolor="#c0c0c0" | <br /> | | width="16" bgcolor="#c0c0c0" | <br /> | ||
| width="100" | <br /> | | width="100" | <br /> | ||
Line 244: | Line 318: | ||
| <br /> | | <br /> | ||
|- valign="top" | |- valign="top" | ||
− | | width="72" | Plasma<br /> | + | | width="72" | [[File:PlasmaIcon.png]] Plasma<br /> |
| width="16" | <br /> | | width="16" | <br /> | ||
| width="100" | <br /> | | width="100" | <br /> | ||
Line 279: | Line 353: | ||
|} | |} | ||
− | =Distribution of planet types= | + | |
+ | = Distribution of planet types = | ||
+ | |||
{| border="1" cellpadding="1" cellspacing="1" align="center" | {| border="1" cellpadding="1" cellspacing="1" align="center" | ||
! Type | ! Type | ||
Line 288: | Line 364: | ||
![[W-Space|W-Space]] | ![[W-Space|W-Space]] | ||
|- | |- | ||
− | |Gas | + | |[[File:GasIcon.png]] Gas |
|align="right"| 23754 | |align="right"| 23754 | ||
|align="right"| 3140 | |align="right"| 3140 | ||
Line 295: | Line 371: | ||
|align="right"| 7545 | |align="right"| 7545 | ||
|- | |- | ||
− | |Ice | + | |[[File:IceIcon.png]] Ice |
|align="right"| 11251 | |align="right"| 11251 | ||
|align="right"| 1589 | |align="right"| 1589 | ||
Line 302: | Line 378: | ||
|align="right"| 3502 | |align="right"| 3502 | ||
|- | |- | ||
− | |Storm | + | |[[File:StormIcon.png]] Storm |
|align="right"| 8592 | |align="right"| 8592 | ||
|align="right"| 1407 | |align="right"| 1407 | ||
Line 309: | Line 385: | ||
|align="right"| 2674 | |align="right"| 2674 | ||
|- | |- | ||
− | |Barren | + | |[[File:BarrenIcon.png]] Barren |
|align="right"| 8036 | |align="right"| 8036 | ||
|align="right"| 1064 | |align="right"| 1064 | ||
Line 316: | Line 392: | ||
|align="right"| 2597 | |align="right"| 2597 | ||
|- | |- | ||
− | |Temperate | + | |[[File:TemperateIcon.png]] Temperate |
|align="right"| 6939 | |align="right"| 6939 | ||
|align="right"| 1062 | |align="right"| 1062 | ||
Line 323: | Line 399: | ||
|align="right"| 2054 | |align="right"| 2054 | ||
|- | |- | ||
− | |Lava | + | |[[File:LavaIcon.png]] Lava |
|align="right"| 6473 | |align="right"| 6473 | ||
|align="right"| 795 | |align="right"| 795 | ||
Line 330: | Line 406: | ||
|align="right"| 2002 | |align="right"| 2002 | ||
|- | |- | ||
− | |Oceanic | + | |[[File:OceanicIcon.png]] Oceanic |
|align="right"| 1256 | |align="right"| 1256 | ||
|align="right"| 171 | |align="right"| 171 | ||
Line 337: | Line 413: | ||
|align="right"| 406 | |align="right"| 406 | ||
|- | |- | ||
− | |Plasma | + | |[[File:PlasmaIcon.png]] Plasma |
|align="right"| 943 | |align="right"| 943 | ||
|align="right"| 127 | |align="right"| 127 | ||
Line 354: | Line 430: | ||
Note: The distribution of planets on the test server, Sisi, was changed on April 27, 2010. So take this information as tentative until it is confirmed when the expansion goes live. | Note: The distribution of planets on the test server, Sisi, was changed on April 27, 2010. So take this information as tentative until it is confirmed when the expansion goes live. | ||
+ | |||
= Planets near Aldrat = | = Planets near Aldrat = | ||
Line 359: | Line 436: | ||
Handy reference material for interesting planets near Aldrat. If you'd like to help build constellation lists, then simply pick a constellation, post it here, review which planet types exist in the system in-game, and make a table here. Easy! | Handy reference material for interesting planets near Aldrat. If you'd like to help build constellation lists, then simply pick a constellation, post it here, review which planet types exist in the system in-game, and make a table here. Easy! | ||
− | As for the rarest (useful) planet type, the Plasma planet, the closest to Aldrat go as follows: | + | As for the rarest (useful) planet type, the [[File:PlasmaIcon.png]] Plasma planet, the closest to Aldrat go as follows: |
Hisec | Hisec | ||
Line 388: | Line 465: | ||
! Urnhard | ! Urnhard | ||
|- | |- | ||
− | |<font color=green>Gas</font> | + | |[[File:GasIcon.png]] <font color=green>Gas</font> |
|align="right"| <font color=green>3</font> | |align="right"| <font color=green>3</font> | ||
|align="right"| 0 | |align="right"| 0 | ||
Line 396: | Line 473: | ||
|align="right"| <font color=green>3</font> | |align="right"| <font color=green>3</font> | ||
|- | |- | ||
− | |Ice | + | |[[File:IceIcon.png]] Ice |
|align="right"| 0 | |align="right"| 0 | ||
|align="right"| 0 | |align="right"| 0 | ||
Line 404: | Line 481: | ||
|align="right"| 0 | |align="right"| 0 | ||
|- | |- | ||
− | |Storm | + | |[[File:StormIcon.png]] Storm |
|align="right"| 0 | |align="right"| 0 | ||
|align="right"| 1 | |align="right"| 1 | ||
Line 412: | Line 489: | ||
|align="right"| 1 | |align="right"| 1 | ||
|- | |- | ||
− | |Barren | + | |[[File:BarrenIcon.png]] Barren |
|align="right"| 5 | |align="right"| 5 | ||
|align="right"| 3 | |align="right"| 3 | ||
Line 420: | Line 497: | ||
|align="right"| 2 | |align="right"| 2 | ||
|- | |- | ||
− | |<font color=green>Temperate</font> | + | |[[File:TemperateIcon.png]] <font color=green>Temperate</font> |
|align="right"| 0 | |align="right"| 0 | ||
|align="right"| <font color=green>1</font> | |align="right"| <font color=green>1</font> | ||
Line 428: | Line 505: | ||
|align="right"| 0 | |align="right"| 0 | ||
|- | |- | ||
− | |<font color=green>Lava</font> | + | |[[File:LavaIcon.png]] <font color=green>Lava</font> |
|align="right"| <font color=green>1</font> | |align="right"| <font color=green>1</font> | ||
|align="right"| 0 | |align="right"| 0 | ||
Line 436: | Line 513: | ||
|align="right"| <font color=green>1</font> | |align="right"| <font color=green>1</font> | ||
|- | |- | ||
− | |Oceanic | + | |[[File:OceanicIcon.png]] Oceanic |
|align="right"| 0 | |align="right"| 0 | ||
|align="right"| 0 | |align="right"| 0 | ||
Line 444: | Line 521: | ||
|align="right"| 0 | |align="right"| 0 | ||
|- | |- | ||
− | |Plasma | + | |[[File:PlasmaIcon.png]] Plasma |
|align="right"| 0 | |align="right"| 0 | ||
|align="right"| 0 | |align="right"| 0 | ||
Line 475: | Line 552: | ||
! Vilur | ! Vilur | ||
|- | |- | ||
− | |<font color=green>Gas</font> | + | |[[File:GasIcon.png]] <font color=green>Gas</font> |
|align="right"| <font color=green>5</font> | |align="right"| <font color=green>5</font> | ||
|align="right"| <font color=green>3</font> | |align="right"| <font color=green>3</font> | ||
Line 484: | Line 561: | ||
|align="right"| <font color=green>1</font> | |align="right"| <font color=green>1</font> | ||
|- | |- | ||
− | |Ice | + | |[[File:IceIcon.png]] Ice |
|align="right"| 0 | |align="right"| 0 | ||
|align="right"| 0 | |align="right"| 0 | ||
Line 493: | Line 570: | ||
|align="right"| 0 | |align="right"| 0 | ||
|- | |- | ||
− | |Storm | + | |[[File:StormIcon.png]] Storm |
|align="right"| 0 | |align="right"| 0 | ||
|align="right"| 1 | |align="right"| 1 | ||
Line 502: | Line 579: | ||
|align="right"| 0 | |align="right"| 0 | ||
|- | |- | ||
− | |Barren | + | |[[File:BarrenIcon.png]] Barren |
|align="right"| 6 | |align="right"| 6 | ||
|align="right"| 4 | |align="right"| 4 | ||
Line 511: | Line 588: | ||
|align="right"| 6 | |align="right"| 6 | ||
|- | |- | ||
− | |<font color=green>Temperate</font> | + | |[[File:TemperateIcon.png]] <font color=green>Temperate</font> |
|align="right"| <font color=green>2</font> | |align="right"| <font color=green>2</font> | ||
|align="right"| 0 | |align="right"| 0 | ||
Line 520: | Line 597: | ||
|align="right"| 0 | |align="right"| 0 | ||
|- | |- | ||
− | |<font color=green>Lava</font> | + | |[[File:LavaIcon.png]] <font color=green>Lava</font> |
|align="right"| <font color=green>1</font> | |align="right"| <font color=green>1</font> | ||
|align="right"| <font color=green>1</font> | |align="right"| <font color=green>1</font> | ||
Line 529: | Line 606: | ||
|align="right"| <font color=green>1</font> | |align="right"| <font color=green>1</font> | ||
|- | |- | ||
− | |Oceanic | + | |[[File:OceanicIcon.png]] Oceanic |
|align="right"| 0 | |align="right"| 0 | ||
|align="right"| 0 | |align="right"| 0 | ||
Line 538: | Line 615: | ||
|align="right"| 0 | |align="right"| 0 | ||
|- | |- | ||
− | |Plasma | + | |[[File:PlasmaIcon.png]] Plasma |
|align="right"| 0 | |align="right"| 0 | ||
|align="right"| 0 | |align="right"| 0 |
Revision as of 02:11, 9 May 2010
Edit note: Need to add a bullet list to each planet showing what can be made from the resources on that planet without having to ship resources/products in from other planets. Such as Lava being able to make Consumer Electronics
Planets are present in every solar system in EVE. The vast majority are uninhabited. Planetary Interaction introduced in the Tyrannis expansion allows players to utilize the planets in EVE to mine and produce goods in the first step in linking EVE with the upcoming DUST 514. Each planet type has 5 resources available to it to be mined via Planetary Interaction. Resources that only appear on one planet type appear in green.
Types of planets
Barren
Barren planets are archetypical "dead terrestrials": dry, rocky worlds with a minimal atmosphere and an unremarkable composition. They are commonly etched with flood channels, which are often broad enough to be visible from orbit; most such worlds have accumulated significant quantities of ice over their lifetimes, but cannot retain it on their surface. Generally surface liquid evaporates rapidly, contributing to the thin atmosphere, but occasionally it will seep back into the ground and refreeze, ready for another breakout in future when the local temperature rises. Resources
|
Gas
Gas planets are characterized by a deep, opaque upper atmosphere, usually composed primarily of light elements such as hydrogen or helium. Simple chemicals can add a range of hues and shades in the visual spectrum, and the interaction between upwellings and rapidly circulating pressure bands result in a huge variety of visible surface structures. A similar level of diversity can be found beneath the cloud-tops: the inner composition of a given gas planet might belong to any one of a dozen broad groups, with no two planets entirely alike in this regard. Resources
Resources on a Gas planet will typically be found in narrow bands running east-west at various latitudes. Base metals are generally in bands around the equator, Aqueous Liquids and Ionic Solutions in mid-latitudes bands, with the Noble Gas near the poles. Reactive Gas will be found in small pockets at all latitudes. |
Ice
The majority of icy planets went through a period of being barren terrestrials, before being surfaced with ice over the course of many millennia. The exact process for this varies from case to case, but the end result is both common and visually uniform - a bright, reflective planet scored by countless fractures and crevasses. A few icy planets are hypothesized to have been warmer, liquid-bearing planets in the past that have subsequently frozen, as a result of either stellar cooling or failed terraforming projects. Resources
Ice planets typically have high amounts of Heavy Metals and Aqueous Liquids available. Micro Organisms and Noble Gas are less abundant, with Planktic Colonies being somewhat thin. Aqueous Liquids tends to be found more in the polar regions of Ice planets, Planktic Colonies in the temperate latitudes and Micro Organisms in the equatorial regions. Noble Gas and Heavy Metals are more randomly distributed with Heavy Metals more towards the equator and Noble Gas more towards the poles but with large areas of overlap and intermingling. |
Lava
So-called "lava planets" (properly "magmatic planets") fall into one of three groups: solar magmatics, which orbit sufficiently close to their star that the surface never cools enough to solidify; gravitational magmatics, which experience gravitational shifts sufficiently strong to regularly and significantly fracture cooling crusts; and magmatoids, which are for largely-unexplained reasons simply incapable of cooling and forming a persistent crust. All three types generally exhibit the same external phenomena - huge red-orange lava fields being a defining feature - but the latter two types are sometimes capable of briefly solidifying for a period measured in years or perhaps decades. Resources
Single-Planet Products
|
Oceanic
Oceanic worlds are a class of terrestrial world covered entirely by liquids, usually in the form of mundane water. While the liquid surface is exceptionally smooth, the ocean floor on most worlds of this type exhibits significant topographic variety. It is this subsurface irregularity which causes the formation of complex weather systems, which would otherwise revert to more uniform patterns. Resources
|
Plasma
The aptly-named "plasma planets" have captured the imagination of countless artists and inspired innumerable works, yet the physics behind them are surprisingly mundane by cosmological standards. A rocky terrestrial with the right kind of atmosphere and magnetic field will, when bombarded with solar radiation, generate sprawling plasma storms as specific atmospheric elements are stripped of their electrons. Over time these storms will generally scorch the surface rock black, adding to the visual impact. Resources
Compared to some other planet types, the resources on Plasma planets tend to be somewhat anemic but evenly distributed across all five types. Unlike Gas planets, there are few guidelines on where you will find concentrations of resources. Distribution of resources is very chaotic. |
Storm
Storm worlds are usually considered terrestrial planets, although to a casual eye they may appear more similar to gas planets, given their opaque, high-pressure atmospheres. Geomorphically, however, the distinctions are clear: compared to a gas world, the atmosphere of a storm world is usually considerably shallower, and generally composed primarily of more complex chemicals, while the majority of the planet's mass is a rocky terrestrial ball. Their name is derived from the continent-scale electrical storms that invariably flash through their upper atmospheres. Resources
Storm planets tend to have equal amounts of Aqueous Liquids, Base Metals and Suspended Plasma in decent amounts, with Noble Gas running a close 4th and Ionic Solutions as a distant 5th and somewhat sparse. Ionic Solutions tend to be distributed in the middle latitudes, Noble Gas anywhere but the equator and Suspended Plasma tending towards the equatorial regions. Aqueous Liquids and Base Metals will appear on broad swaths across all latitudes in giant swirling patterns. |
Temperate
Life-bearing worlds are often referred to as "temperate", as their mild temperatures are one of their defining features. Planets with existing, stable ecosystems are prime targets for colonization efforts as they are generally easier to make fully habitable; as a result, the majority of highly populated worlds are of this type. Indeed, it is not altogether uncommon for detailed surveys to reveal signs of previous settlements from various stages of New Eden's history. Resources
|
Shattered
Shattered worlds were once terrestrial planets, torn asunder by some immense cataclysm. All such worlds in the New Eden cluster are products of the disastrous stellar events that occurred during the "Seyllin Incident". However, reports continue to circulate of similar planets discovered in the unmapped systems reached exclusively through unstable wormholes. How these met their fate, if indeed they exist at all, is unknown.
Resources
- None
Resource Distribution by Planet Type
Distribution of planet types
Type | All | HiSec | LoSec | NullSec | W-Space |
---|---|---|---|---|---|
Gas | 23754 | 3140 | 3199 | 9870 | 7545 |
Ice | 11251 | 1589 | 1470 | 4690 | 3502 |
Storm | 8592 | 1407 | 1116 | 3395 | 2674 |
Barren | 8036 | 1064 | 1032 | 3343 | 2597 |
Temperate | 6939 | 1062 | 912 | 2911 | 2054 |
Lava | 6473 | 795 | 872 | 2804 | 2002 |
Oceanic | 1256 | 171 | 168 | 511 | 406 |
Plasma | 943 | 127 | 131 | 386 | 299 |
Shattered | 9 | 0 | 1 | 6 | 2 |
Note: The distribution of planets on the test server, Sisi, was changed on April 27, 2010. So take this information as tentative until it is confirmed when the expansion goes live.
Planets near Aldrat
Handy reference material for interesting planets near Aldrat. If you'd like to help build constellation lists, then simply pick a constellation, post it here, review which planet types exist in the system in-game, and make a table here. Easy!
As for the rarest (useful) planet type, the Plasma planet, the closest to Aldrat go as follows:
Hisec
- 3 jumps - 0.9 sec rating - Olbra I
- 7 jumps - 0.6 sec rating - Traun II
- 8 jumps - 0.8 sec rating - Eiluvodi II
- 8 jumps - 0.8 sec rating - Frarn II
Lowsec
- 8 jumps - 0.4 sec rating - Rancer I
- 9 jumps - 0.2 sec rating - Fuskunen II
- 9 jumps - 0.4 sec rating - Atlar I
For finding other planets please refer to http://evemaps.dotlan.net/region/Metropolis/planets. Only shows tranquility data.
Constellation: Aptetter