Quote from: challengerX on January 15, 2015, 07:18:58 AM

Quote from: Madman Mordo on January 15, 2015, 06:35:12 AM

Quote from: Lemy the Lizerd on January 14, 2015, 10:41:05 PM

nigga muslims are not an ethnic group

Religion falls under the official definition of Ethnic Cleansing even though they aren't actually an ethnicity.

You actually shouldn't use the term "ethnic cleansing". It's as if there's something that's "dirty" or wrong being cleansed. There isn't.

We as a society shouldn't adopt the terms of mass murderers.

Does it really matter what we call it? It's already been adopted and it's stuck, sorta like homophobia. We don't use it to describe people who fear gay people, but that's what we call them anyway.

It's just that it's a word used to make light of genocide, so to speak.

Quote from: challengerX on January 15, 2015, 08:08:14 AM

Quote from: Icy on January 15, 2015, 08:06:39 AM

Quote from: challengerX on January 15, 2015, 08:05:21 AM

Quote from: Icy on January 15, 2015, 08:04:12 AM

Quote from: challengerX on January 15, 2015, 08:03:31 AM

I'm just sitting here laughing at all the people who respect this guy because of his publicity stunts.

I respect him more for his work with the poor before (and still during) being named Pope.

You know, actually helping.

It's all bullshit. When the Vatican gives away all their millions to the poor I'll respect them. When they stop oppressing and raping kids I'll respect them.

Not even going to start down that, because this thread will be derailed by Page 2

Religious leaders are almost always garbage.

I'd amend that to say most World leaders.

But I'm talking about religion specifically.

In fact, there have been more good world leaders than there has been religious leaders.

Quote from: challengerX on January 15, 2015, 08:03:31 AM

I'm just sitting here laughing at all the people who respect this guy because of his publicity stunts.

I respect him more for his work with the poor before (and still during) being named Pope.

You know, actually helping.

It's all bullshit. When the Vatican gives away all their millions to the poor I'll respect them. When they stop oppressing and raping kids I'll respect them.

Quote from: challengerX on January 15, 2015, 07:45:36 AM

Quote from: Dustin xLilD on January 15, 2015, 07:44:12 AM

Quote from: BerzerkCommando on January 15, 2015, 07:41:48 AM

Quote from: challengerX on January 15, 2015, 07:37:00 AM

Quote from: Dustin xLilD on January 15, 2015, 07:35:11 AM

http://www.bungie.net/en/Forum/Post/91439352/0/0

The obsession is real.

Should we call him "Methew" now? Also does that guy still post on Bnet?

Maybe autistic isn't the word to describe that thread. Politically brainwashed may suit better IMO.

Politically brainwashed by a party I don't vote for or even fully support.

#DustbinPosting

"I don't support everything this party says, therefore I'm not brainwashed."

Being brainwashed by the definition of the word would mean I'd support them completely.

When are you going to start learning the definitions of the words you use so you stop embarrassing yourself like this?

Icy was pretty clear. Posts have been pruned and the next person to continue fighting gets hit.

Icy's post wasn't even in the thread when I replied. 

http://www.bungie.net/en/Forum/Post/91439352/0/0

The obsession is real.

Quote from: challengerX on January 15, 2015, 07:24:43 AM

but seeing how I'm not wrong

2+2=5 mentality

"I'M NOT WRONG, I'M NOT WRONG, I'M NOT WRONG"

Seeing how I have tons of discussions in Serious, no I'm not wrong.

What is your obsession with me anyway? Out of the blue you just randomly started talking shit about me all the time. What exactly are you so butthurt about?

Quote from: challengerX on January 15, 2015, 07:06:45 AM

Quote from: Flee on January 15, 2015, 07:03:29 AM

Quote from: challengerX on January 15, 2015, 07:00:53 AM

Quote from: Flee on January 15, 2015, 07:00:00 AM

Quote from: challengerX on January 15, 2015, 06:57:56 AM

Quote from: Flee on January 15, 2015, 06:56:47 AM

Quote from: challengerX on January 15, 2015, 06:55:32 AM

Quote from: Flee on January 15, 2015, 06:54:53 AM

Should I have waffles, french fries (with mayo of course) or chocolate? All with beer, of course.

#BelgianAsFuck

Just have all of them.

I'll probably just have ramen in a cup.

You know I've never had Ramen.

Wut. I still have two empty cups sitting on my desk.

I probably just never had them because I'm not Belgian so I have good taste.

But I've seen plenty of Americans eat them too.

Liar.

This is at Walmart.

Dude I was kidding.

Ramen is a cliche college kid food in America.

Looks ugly, fragile, and useless.

Quote from: Lemy the Lizerd on January 14, 2015, 10:41:05 PM

nigga muslims are not an ethnic group

Religion falls under the official definition of Ethnic Cleansing even though they aren't actually an ethnicity.

You actually shouldn't use the term "ethnic cleansing". It's as if there's something that's "dirty" or wrong being cleansed. There isn't.

We as a society shouldn't adopt the terms of mass murderers.

Ocean
From Wikipedia, the free encyclopedia
For other uses, see Ocean (disambiguation).
Further information: Seawater

Surface of the Atlantic Ocean meeting the Earth's planetary boundary layer and troposphere.
View of the Earth where all five oceans visible
Earth's oceans
Arctic
Pacific
Atlantic
Indian
Southern
World Ocean
v t e
An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity[1]) is a body of saline water that composes much of a planet's hydrosphere.[2] On Earth, an ocean is one of the major conventional divisions of the World Ocean, which occupies two-thirds of the planet's surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans.[3][4] The word sea is often used interchangeably with "ocean" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land.[5]
Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of the Earth's surface.[6] The ocean contains 97% of the Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored.[6] The total volume is approximately 1.3 billion cubic kilometers (310 million cu mi)[7] with an average depth of 3,682 meters (12,080 ft).[8]
Because it is the principal component of Earth's hydrosphere, the world ocean is integral to all known life, forms part of the carbon cycle, and influences climate and weather patterns. It is the habitat of 230,000 known species, although much of the oceans depths remain unexplored, and over two million marine species are estimated to exist.[9] The origin of Earth's oceans remains unknown; oceans are believed to have formed in the Hadean period and may have been the impetus for the emergence of life.
Extra-terrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for the existence of oceans elsewhere in the Solar System. Early in their geologic histories, Mars and Venus are theorized to have had large water oceans. The Mars ocean hypothesis suggests that nearly a third of the surface of Mars was once covered by water, and a runaway greenhouse effect may have boiled away the global ocean of Venus. Compounds such as salts and ammonia dissolved in water lower its freezing point, so that water might exist in large quantities in extraterrestrial environments as brine or convecting ice. Unconfirmed oceans are speculated beneath the surface of many dwarf planets and natural satellites; notably, the ocean of Europa is believed to have over twice the water volume of Earth. The Solar System's gas giant planets are also believed to possess liquid atmospheric layers of yet to be confirmed compositions. Oceans may also exist on exoplanets and exomoons, including surface oceans of liquid water within a circumstellar habitable zone. Ocean planets are a hypothetical type of planet with a surface completely covered with liquid.[10][11]
Contents  [hide]
1 Earth's global ocean
1.1 Global divisions
1.2 Physical properties
1.3 Zones with depth
1.4 Exploration
1.5 Climate
1.6 Biology
1.7 Gases
1.8 Ocean Surface
1.9 Mixing Time
1.10 Salinity
1.11 Absorption of light
1.12 Economic value
1.13 Waves
2 Extraterrestrial oceans
2.1 Planets
2.2 Natural satellites
2.3 Dwarf planets and trans-Neptunian objects
2.4 Extrasolar
2.5 Non-water surface liquids
3 See also
4 References
5 Further reading
6 External links
Earth's global ocean[edit]
Global divisions[edit]
Further information: Borders of the oceans
Rotating series of maps showing alternate divisions of the oceans
Various ways to divide the World Ocean
Though generally described as several separate oceans, these waters comprise one global, interconnected body of salt water sometimes referred to as the World Ocean or global ocean.[12][13] This concept of a continuous body of water with relatively free interchange among its parts is of fundamental importance to oceanography.[14]
The major oceanic divisions are defined in part by the continents, various archipelagos, and other criteria. See the table below for more information; note that the table is in descending order in terms of size.[11][15]
Rank   Ocean   Notes
1   Pacific   The peaceful sea west of the Magellan Strait,[16] officially separated into the North and South Pacific (divided by the Equator[17] and containing the waters between the southernmost points of Tasmania and Terra del Fuego (and including the waters of the Magellan Strait) but limited by the borders of the Tasman, Coral, Solomon, and Bismark Seas, the East Indian Archipelago, the Philippine, Japan, Okhotsk, and Bering Seas, the Gulf of Alaska, the coastal waters of southeast Alaska and British Columbia, and the Gulf of California.[18]
2   Atlantic   The sea beyond the Atlas Mountains,[19][20] officially separated into the North and South Atlantic (divided by the Equator) and containing the waters between the southernmost points of Tierra del Fuego and Africa but limited by the borders of the Rio de la Plata, the Caribbean Sea, the Gulf of Mexico, the Bay of Fundy, the Gulf of St. Lawrence, the Davis Strait, the Greenland, Norwegian, North, Scottish, and Irish Seas, the Bristol and English Channels, the Bay of Biscay, the Mediterranean Sea, and the Gulf of Guinea,[18] although now often considered to end north of the Antarctic Convergence.
3   Indian   The sea south of India, officially containing the waters between the southernmost points of Africa and Tasmania, bounded on the north by the Arabian and Laccadive Seas, the Bay of Bengal, the East Indian Archipelago, and the Great Australian Bight and on the south by Antarctica,[18] although now often considered to end north of the Antarctic Convergence.
4   Southern
or
Antarctic   Still officially considered an extension of the Pacific, Atlantic and Indian Oceans by the IHO,[11][18] it is distinguished by the convergence which encircles Antarctica.
5   Arctic   The sea around the North Pole, officially containing the waters north of the Greenland Sea, then a line east along 80°N to the Barentsz, Kara, Laptev, East Siberian, Chuckchi, and Beaufort Seas.[18] Sometimes[when?] itself considered[by whom?] a sea of the Atlantic.
These adjacent regions—whether seas, gulfs, bays, bights, or straits—are very often included as part of the nearest ocean.
Physical properties[edit]
Further information: Seawater
The total mass of the hydrosphere is about 1,400,000,000,000,000,000 metric tons (1.5×1018 short tons) or 1.4×1021 kg, which is about 0.023 percent of the Earth's total mass. Less than 3 percent is freshwater; the rest is saltwater, mostly in the ocean. The area of the World Ocean is 361 million square kilometers (139 million square miles),[21] and its volume is approximately 1.3 billion cubic kilometers (310 million cu mi).[7] This can be thought of as a cube of water with an edge length of 1,111 kilometers (690 mi). Its average depth is 3,790 meters (12,430 ft), and its maximum depth is 10,923 meters (6.787 mi).[21] Nearly half of the world's marine waters are over 3,000 meters (9,800 ft) deep.[13] The vast expanses of deep ocean (anything below 200 meters (660 ft)) cover about 66% of the Earth's surface.[22] This does not include seas not connected to the World Ocean, such as the Caspian Sea.
The bluish color of water is a composite of several contributing agents. Prominent contributors include dissolved organic matter and chlorophyll.[23]
Sailors and other mariners have reported that the ocean often emits a visible glow, or luminescence, which extends for miles at night. In 2005, scientists announced that for the first time, they had obtained photographic evidence of this glow.[24] It is most likely caused by bioluminescence.[25][26][27]
Zones with depth[edit]
Drawing showing divisions according to depth and distance from shore
The major oceanic divisions
Oceanographers divide the ocean into different zones by physical and biological conditions. The pelagic zone includes all open ocean regions, and can be divided into further regions categorized by depth and light abundance. The photic zone includes the oceans from the surface to a depth of 200 m; it is the region where photosynthesis can occur and is, therefore, the most biodiverse. Since plants require photosynthesis, life found deeper than the photic zone must either rely on material sinking from above (see marine snow) or find another energy source. Hydrothermal vents are the primary source of energy in what is known as the aphotic zone (depths exceeding 200 m). The pelagic part of the photic zone is known as the epipelagic.
The pelagic part of the aphotic zone can be further divided into vertical regions according to temperature. The mesopelagic is the uppermost region. Its lowermost boundary is at a thermocline of 12 °C (54 °F), which, in the tropics generally lies at 700–1,000 meters (2,300–3,300 ft). Next is the bathypelagic lying between 10 and 4 °C (50 and 39 °F), typically between 700–1,000 meters (2,300–3,300 ft) and 2,000–4,000 meters (6,600–13,100 ft) Lying along the top of the abyssal plain is the abyssopelagic, whose lower boundary lies at about 6,000 meters (20,000 ft). The last zone includes the deep oceanic trench, and is known as the hadalpelagic. This lies between 6,000–11,000 meters (20,000–36,000 ft) and is the deepest oceanic zone.
The benthic zones are aphotic and correspond to the three deepest zones of the deep-sea. The bathyal zone covers the continental slope down to about 4,000 meters (13,000 ft). The abyssal zone covers the abyssal plains between 4,000 and 6,000 m. Lastly, the hadal zone corresponds to the hadalpelagic zone, which is found in oceanic trenches.
The pelagic zone can be further subdivided into two subregions: the neritic zone and the oceanic zone. The neritic zone encompasses the water mass directly above the continental shelves whereas the oceanic zone includes all the completely open water.
In contrast, the littoral zone covers the region between low and high tide and represents the transitional area between marine and terrestrial conditions. It is also known as the intertidal zone because it is the area where tide level affects the conditions of the region.
The ocean can be divided into three density zones: the surface zone, the pycnocline, and the deep zone. The surface zone, also called the mixed layer, refers to the uppermost density zone of the ocean. Temperature and salinity are relatively constant with depth in this zone due to currents and wave action. The surface zone contains ocean water that is in contact with the atmosphere and within the photic zone. The surface zone has the ocean's least dense water and represents approximately 2% of the total volume of ocean water. The surface zone usually ranges between depths of 500 feet to 3,300 feet below ocean surface, but this can vary a great deal. In some cases, the surface zone can be entirely non-existent. The surface zone is typically thicker in the tropics than in regions of higher latitude. The transition to colder, denser water is more abrupt in the tropics than in regions of higher latitudes. The pycnocline refers to a zone wherein density substantially increases with depth due primarily to decreases in temperature. The pycnocline effectively separates the lower-density surface zone above from the higher-density deep zone below. The pycnocline represents approximately 18% of the total volume of ocean water. The deep zone refers to the lowermost density zone of the ocean. The deep zone usually begins at depths below 3,300 feet in mid-latitudes. The deep zone undergoes negligible changes in water density with depth. The deep zone represents approximately 80% of the total volume of ocean water. The deep zone contains relatively colder and stable water.
If a zone undergoes dramatic changes in temperature with depth, it contains a thermocline. The tropical thermocline is typically deeper than the thermocline at higher latitudes. Polar waters, which receive relatively little solar energy, are not stratified by temperature and generally lack a thermocline since surface water at polar latitudes are nearly as cold as water at greater depths. Below the thermocline, water is very cold, ranging from −1 °C to 3 °C. Since this deep and cold layer contains the bulk of ocean water, the average temperature of the world ocean is 3.9 °C If a zone undergoes dramatic changes in salinity with depth, it contains a halocline. If a zone undergoes a strong, vertical chemistry gradient with depth, it contains a chemocline.
The halocline often coincides with the thermocline, and the combination produces a pronounced pycnocline.
Exploration[edit]
False color photo
Map of large underwater features (1995, NOAA)
Ocean travel by boat dates back to prehistoric times, but only in modern times has extensive underwater travel become possible.
The deepest point in the ocean is the Mariana Trench, located in the Pacific Ocean near the Northern Mariana Islands. Its maximum depth has been estimated to be 10,971 meters (35,994 ft) (plus or minus 11 meters; see the Mariana Trench article for discussion of the various estimates of the maximum depth.) The British naval vessel, Challenger II surveyed the trench in 1951 and named the deepest part of the trench, the "Challenger Deep". In 1960, the Trieste successfully reached the bottom of the trench, manned by a crew of two men.
Climate[edit]
World map with colored, directed lines showing how water moves through the oceans. Cold deep water rises and warms in the central Pacific and in the Indian, while warm water sinks and cools near Greenland in the North Atlantic and near Antarctica in the South Atlantic.
A map of the global thermohaline circulation; blue represent deep-water currents, while red represent surface currents
Ocean currents greatly affect the Earth's climate by transferring heat from the tropics to the polar regions. Transferring warm or cold air and precipitation to coastal regions, where winds may carry them inland. Surface heat and freshwater fluxes create global density gradients that drive the thermohaline circulation part of large-scale ocean circulation. It plays an important role in supplying heat to the polar regions, and thus in sea ice regulation. Changes in the thermohaline circulation are thought to have significant impacts on the Earth's radiation budget. In so far as the thermohaline circulation governs the rate at which deep waters reach the surface, it may also significantly influence atmospheric carbon dioxide concentrations.
For a discussion of the possibilities of changes to the thermohaline circulation under global warming, see shutdown of thermohaline circulation.
It is often stated that the thermohaline circulation is the primary reason that the climate of Western Europe is so temperate. An alternate hypothesis claims that this is largely incorrect, and that Europe is warm mostly because it lies downwind of an ocean basin, and because atmospheric waves bring warm air north from the subtropics.[28][29]
The Antarctic Circumpolar Current encircles that continent, influencing the area's climate and connecting currents in several oceans.
One of the most dramatic forms of weather occurs over the oceans: tropical cyclones (also called "typhoons" and "hurricanes" depending upon where the system forms).
Biology[edit]
Further information: Marine biology
The ocean has a significant effect on the biosphere. Oceanic evaporation, as a phase of the water cycle, is the source of most rainfall, and ocean temperatures determine climate and wind patterns that affect life on land. Life within the ocean evolved 3 billion years prior to life on land. Both the depth and the distance from shore strongly influence the biodiversity of the plants and animals present in each region.[30]
Lifeforms native to the ocean include:
Fish;
Radiata, such as jellyfish (Cnidaria);
Cetacea, such as whales, dolphins, and porpoises;
Cephalopods, such as octopus and squid;
Crustaceans, such as lobsters, clams, shrimp, and krill;
Marine worms;
Plankton; and
Echinoderms, such as brittle stars, starfish, sea cucumbers, and sand dollars.
In addition, many land animals have adapted to living a major part of their life on the oceans. For instance, seabirds are a diverse group of birds that have adapted to a life mainly on the oceans. They feed on marine animals and spend most of their lifetime on water, many only going on land for breeding. Other birds that have adapted to oceans as their living space are penguins, seagulls and pelicans. Seven species of turtles, the sea turtles, also spend most of their time in the oceans.
Gases[edit]
Characteristics of Oceanic Gases [31][32][33]
Gas   Concentration of Seawater, by Mass (in parts per million), for whole Ocean    % Dissolved Gas, by Volume, in Seawater at Ocean Surface
Carbon dioxide (CO2)   64 to 107   15%
Nitrogen (N2)   10 to 18   48%
Oxygen (O2)   0 to 13   36%
Solubility of Oceanic Gases (in terms of mL/L) with Temperature at salinity of 33‰ and atmospheric pressure[34]
Temperature   O2   CO2   N2
0 °C   8.14   8,700   14.47
10 °C   6.42   8,030   11.59
20 °C   5.26   7,350   9.65
30 °C   4.41   6,600   8.26
Ocean Surface[edit]
Generalized Characteristics of Ocean Surface by Latitude [35][36][37][38][39][40][41]
Characteristic   Oceanic Waters in Polar regions   Oceanic Waters in Temperate regions   Oceanic Waters in Tropical regions
Precipitation vs. evaporation   P > E   P > E   E > P
Sea Surface Temperature in Winter   −2 °C   5 to 20 °C   20 to 25 °C
Average Salinity   28‰ to 32‰   35‰   35‰ to 37‰
Annual Variation of Air Temperature   ≤ 40ªC   10 °C   < 5 °C
Annual Variation of Water Temperature   < 5ªC   10 °C   < 5 °C
Mixing Time[edit]
Residence Time=The amount of the element in the ocean ÷ The rate at which that element is added to (or removed from) the ocean
The mean oceanic mixing time (residence time) is thought to be approximately 1,600 years. If a given element in the ocean stays in the ocean, on average, longer than the oceanic mixing time, then that element is assumed to be homogeneously spread throughout the ocean. As a result, since the major salts have a residence time that is longer than 1,600 years, the ratio of major salts is thought to be unchanging across the ocean. This constant ratio is often referred to as Forchhammer's principle or the principle of constant proportions.
Mean Oceanic Residence Times for specific Constituents [42][43]
Constituent   Residence Time (in years)
Iron (Fe)   200
Aluminum (Al)   600
Manganese (Mn)   1,300
Water (H2O)   4,100
Silicon (Si)   20,000
Carbonate (CO32-)   110,000
Calcium (Ca2+)   1,000,000
Sulfate (SO42-)   11,000,000
Potassium (K+)   12,000,000
Magnesium (Mg2+)   13,000,000
Sodium (Na+)   68,000,000
Chloride (Cl-)   100,000,000
Salinity[edit]
A zone of rapid salinity increase with depth is called a halocline. The temperature of maximum density of seawater decreases as its salt content increases. Freezing temperature of water decreases with salinity, and boiling temperature of water increases with salinity. Typical seawater freezes at around −1.9 °C at atmospheric pressure. If precipitation exceeds evaporation, as is the case in polar and temperate regions, salinity will be lower. If evaporation exceeds precipitation, as is the case in tropical regions, salinity will be higher. Thus, oceanic waters in polar regions have lower salinity content than oceanic waters in temperate and tropical regions.[44]
Salinity can be calculated using the chlorinity, which is a measure of the total mass of halogen ions (includes fluorine, chlorine, bromine, and iodine) in seawater. By international agreement, the following formula is used to determine salinity:
Salinity (in ‰)=1.80655 x Chlorinity (in ‰)

The average chlorinity is about 19.2‰, and, thus, the average salinity is around 34.7‰ [44]
Absorption of light[edit]
Absorption of Light in Different Wavelengths by Ocean [44]
Color: Wavelength (nm)   Depth wherein 99 percent of wavelength is absorbed (in meters)   Percent absorbed in 1 meter of water
Ultraviolet (UV): 310   31   14.0
Violet (V): 400   107   4.2
Blue (B): 475   254   1.8
Green (G): 525   113   4.0
Yellow (Y): 575   51   8.7
Orange (O): 600   25   16.7
Red (R): 725   4   71.0
Infrared (IR): 800   3   82.0
Economic value[edit]
The oceans are essential to transportation. This is because most of the world's goods move by ship between the world's seaports. Oceans are also the major supply source for the fishing industry. Some of the more major ones are shrimp, fish, crabs, and lobster.[6]
Waves[edit]
Further information: Wind wave
The motions of the ocean surface, known as undulations or waves, are the partial and alternate rising and falling of the ocean surface.

Quote from: challengerX on January 15, 2015, 07:00:53 AM

Quote from: Flee on January 15, 2015, 07:00:00 AM

Quote from: challengerX on January 15, 2015, 06:57:56 AM

Quote from: Flee on January 15, 2015, 06:56:47 AM

Quote from: challengerX on January 15, 2015, 06:55:32 AM

Quote from: Flee on January 15, 2015, 06:54:53 AM

Should I have waffles, french fries (with mayo of course) or chocolate? All with beer, of course.

#BelgianAsFuck

Just have all of them.

I'll probably just have ramen in a cup.

You know I've never had Ramen.

Wut. I still have two empty cups sitting on my desk.

I probably just never had them because I'm not Belgian so I have good taste.

But I've seen plenty of Americans eat them too.

Liar.

i just get a bunch of people raising their arms

You're not patriotic enough.

Quote from: challengerX on January 15, 2015, 06:55:32 AM

Quote from: Flee on January 15, 2015, 06:54:53 AM

Should I have waffles, french fries (with mayo of course) or chocolate? All with beer, of course.

#BelgianAsFuck

Just have all of them.

I'll probably just have ramen in a cup.

You know I've never had Ramen.

Should I have waffles, french fries (with mayo of course) or chocolate? All with beer, of course.

#BelgianAsFuck

Just have all of them.