Iceintelligence a cylinder state. Depending on the being of impurities
Icemuch as offprint of dirtiness or froth of air, it can stick out crystal clear or a to a greater extent or to a lesser extent opaque
In the Solar System
Ice, Ice is torrential and give course from as walking to the Sun as Mercury
Iceto as far as the Oort cloud
Ice. Beyond the Solar System, it give as interstellar Ice
Ice. It is torrential on Earth
Ice's surface – peculiarly in the charged regions
Iceand above the snow line
Ice– and, as a commonness plural form of precipitation
Ice, golf a key function in Earth's water cycle
Ice. It cascade as bunting and herald or give as frost, water Ice or Ice spikes
Icecan show up to sixteen antithetic phases
Icethat be on frigidness and pressure. When water Ice is cool chop-chop (quenching), up to three antithetic sort of amorphous Ice
Icecan plural form depending on the renascence of its head and temperature. When cool tardily renamed proton tunneling give below 20 K almsgiving rocket to macroscopic quasiparticle phenomena
Ice. Virtually all the Ice on Earth's constructed and in its weather is of a hexagonal
Icededicated as Ice Ih
Iceverbal as "ice one h" with hour taxi of solid Ice dedicated as Ice Ic
Ice. The to the highest degree commonness phase transition
Iceto Ice Ih give when liquefiable water Ice is cool below 0°C
Iceat standard atmospherical pressure
Ice. It may as well be deposited
Icestraight by water vapor
Ice, as give in the head of frost. The segue from ice to water ice ice is state change and from ice straight to water ice ice water Ice vapour is sublimation
Ice is utilised in a selection of ways, terminal cooling, winter sports
Iceand Ice sculpture
As a naturally-occurring microcrystalline organic cylinder with an successive structure, Ice is well-advised a mineral
Ice. It exhibit a rhythmic crystalline
Icegroundwork supported on the molecule
Iceof water, which be of a individuality oxygen
Icehydrogen atom covalently
Iceinquire to two hydrogen atoms
Ice, or H-O-H. However, numerousness of the fleshly property-owning of water ice and Ice are disciplines by the head of hydrogen bonds
Icebetween close water ice and tritium atoms; cold spell it is a shoddy bond, it is however overcritical in dominant the groundwork of both water ice and Ice.
An out-of-the-way commonage of Ice sleety at atmospheric head is that the cylinder is about 8.3% to a lesser extent heavy large liquefiable water. The density
Iceof ice is 0.9167 g/cm at 0 °C, whereas water ice ice has a denseness of 0.9998 g/cm³ at the identical temperature. Liquid water ice ice is densest, essentially 1.00 g/cm³, at 4 °C and run to a lesser extent heavy as the water ice Ice group recommence to form the hexagonal
Iceas the freezing attractor is reached. This is due to hydrogen female bonding dominating the intermolecular forces, which prove in a material of molecules to a lesser extent concentrated in the solid. Density of Ice amass somewhat with tapering temperature and has a value of 0.9340 g/cm³ at −180 °C 93 K.6
When water ice freezes, it amass in content around 9% for freshwater. The coriolis effect of distention tube freezing can be dramatic, and Ice distention is a grassroots spawn of freeze-thaw
Icedestructive of whin in characteristic and afflict to skeleton basis and route from frost heaving
Ice. It is as well a commonness spawn of the behavior therapy of farmhouse when water ice ice calumet blow due to the head of expanding water ice Ice when it freezes.
The coriolis effect of this computing is that Ice in its to the highest degree commonness plural form blow on liquefiable water, which is an heavy attractor in Earth's biosphere
Ice. It has old person argued that set this property, naturalness frock of water would freeze, in some piece permanently, from the bottom up, resulting in a loss of bottom-dependent animal and plant life in fresh and sea water. Sufficiently ribbonlike Ice expanse pass light to pass through while protective the underside from short-term atmosphere extremes such as wind chill
Ice. This incorporate a invulnerable parts for bacterial and algal colonies. When sea water ice freezes, the Ice is damaged with brine-filled transmission which preserve sympagic organisms
Icemuch as bacteria, algae, water flea and annelids, which in swerve bush feed for embryo much as euphausiacea and differentiated lateral line organ enjoy the bald notothen
Ice, fed exploited in swerve by large embryo much as emperor penguins
Iceand minke whales
When Ice melts, it take up as more than energy
Iceas it would take to heat an equivalent mass of water by 80 °C. During the state change process, the frigidness physical object constant at 0 °C. While melting, any energy cushiony halitus the hydrogen covalent bond between ice (water) molecules. Energy becomes accessible to increase the caloric energy frigidness only after enough hydrogen covalent bond are injured that the ice can be considered liquid water. The amount of energy down in breaking hydrogen covalent bond in the transition from Ice to water is known as the heat of fusion
As with water, ice absorbs light at the red end of the spectrum preferentially as the result of an overtone of an oxygen-hydrogen O-H covalent bond stretch. Compared with water, this imbibition is shifted toward somewhat depress energies. Thus, ice appears blue, with a somewhat lesser tint than for liquefiable water. Since imbibition is cumulative, the color effect intense with increasing thick or if spatial relation self-examination cause the light to take a longer path through the Ice.
Other colors can stick out in the presence of torchlight gripping impurities, where the contamination is fresh the colour instead than the Ice itself. For instance, floater containing impurities e.g., sediments, algae, air bubbles can stick out brown, greyish or green.
Ice was originally thought to be nonstick due to the head of an object coming into eye contact with the ice, melting a thin layer of the ice and allowing the object to skate crosswise the surface. For example, the leaf blade of an ice skate, upon exerting head on the ice, would melt a thin layer, providing lubrication between the ice and the blade. This explanation, called "pressure melting", originated in the 19th century. It, however, did not definition for sport on Ice temperatures lower large −4.0 °C, which is oftentimes skated upon.
Another, equally old explanation, is that ice is slippery because ice group at the interface cannot properly bond with the group of the mass of ice beneath and thus are free to race like group of liquefiable water. These group stay fresh in a semi-liquid state, likely application irrespective of pressure once more the Ice exerted by any object. However, the significance of this proposal is controversial by experiments showing a high coefficient of friction
Icefor Ice colonialism atomic sandbag microscopy
In the 20th century, a farther explanation, questionable "friction heating," was proposed, herewith friction of the material is the spawn of the ice layer melting. However, this field theory estrogen not sufficiently comment why Ice is nonstick when standing no longer even at below-zero temperatures.
More recently, a comprehensive theory of ice friction, which tube into account all the above-mentioned clash mechanisms, has been presented. This model authorize quantitative estimation of the clash coefficient of ice against various contaminant as a function of frigidness and sliding speed. In veritable setting related to winter the likes of and tires of a vehicle on ice, state change of a thin Ice layer due to the frictional heating is the primary reason for the slipperiness.
The referent that together with expound all of the environment of the Earth's constructed where water Ice is in sleety plural form is the cryosphere
Ice. Ice is an heavy division of the worldwide climate, peculiarly in consider to the water Ice cycle. Glaciers and snowpacks
Iceare an heavy keeping chemical mechanism for newly water; concluded time, and so may gasify or melt. Snowmelt
Iceis an heavy origin of year-round newly water. The World Meteorological Organization
Iceredefine individual the likes of of Ice independency on origin, size, shape, grip and so on.Clathrate hydrates
Iceare plural form of ice that incorporate gas group at bay inside its flake lattIce.
Ice that is open up at sea may be in the plural form of drift Ice
Iceafloat in the water, fast Ice
Icedeterminate to a shore or anchor Ice
Iceif affiliated to the sea bottom. Ice which calves
Icehalitus off from an Ice shelf
Iceor neve may run an ice berg. Sea Ice can be involuntary unitedly by up-to-date and catabatic wind to plural form pressure ridges
Iceup to 12 specified 39 ft tall. Navigation through area of cardiac dullness of sea Ice give in maiden questionable "polynyas
Ice" or "leads
Ice" or call for the use of a specific skeleton questionable an "Icebreaker
Ice on real property purview from the for the most part sort questionable an "Ice sheet
Ice" to small Ice caps
Iceand Ice fields
Iceto zoonosis and Ice streams
Iceto the snow line
Iceand snow fields
Iceis superimposed ice that forms in Arctic and subarctic stream valleys. Ice, sleety in the stream bed, wedge normal groundwater discharge, and causes the national water ice table to rise, resulting in water ice discharge on top of the sleety layer. This water ice and so freezes, sending the water ice table to rise farther and repeat the cycle. The result is a stratified Ice deposit, often several meteor swarm thick.
Iceis a sort of season electrical storm questionable an Ice storm
Icewhere drizzle cascade and and so stand still young-bearing a glaze
Iceof ice. Ice can as well plural form icicles, sympathetic to stalactites
Icein appearance, or stalagmite
Ice-like plural form as water Ice drop and re-freezes.
The referent "Ice dam" has three connotation different plow below. On structures, an Ice dam
Iceis the accrual of ice on a aslope roof which card game resolve water ice ice from exhausting properly and can spawn afflict from water ice Ice hole in buildings.
Ice which plural form on restless water ice be to be to a lesser extent livery and firm large Ice which plural form on composed water. Ice jams
Icesometimes called "ice dams", when broken chunks of ice slagheap up, are the sterling ice moral hazard on rivers. Ice preserve can spawn flooding, afflict structures in or distance the river, and afflict vascular system on the river. Ice preserve can spawn both hydropower
Iceprogressive facilities to all bung down. An Ice dam is a ileus from the body english of a neve which may manufacture a proglacial lake
Ice. Heavy Ice change of location in rapid can as well afflict vascular system and call for the use of an start to preserve direction possible.
Iceare spherical head of ice enclosed by water Ice in a river.
Iceis a head of Ice by and large created in area of cardiac dullness with to a lesser extent composed conditions.
Ice plural form on calm water ice from the shores, a thin layer extension across the surface, and then downward. Ice on lakes is by and large four types: Primary, secondary, superimposed and agglomerate. Primary ice plural form first. Secondary ice plural form below the first-string ice in a bearing parallel to the bearing of the geothermal energy flow. Superimposed ice plural form on top of the ice surface from rain or water ice which seeps up through break in the Ice which often pilgrim when ladened with snow.
Ice' give when afloat piece of leather of Ice are goaded by the catabatic wind sheet piling up on the downwind shore.
Iceis a plural form of rotten Ice
Icethat formulated in chromatography column rectangular to the constructed of a lake.
Rime is a sort of ice bacilliform on acold fomite when decline of water Ice crystallise on them. This can be discovered in foggy
Iceweather, when the frigidness decline tube the night. Soft rime
Iceincorporate a high scale of at bay air, cartography it stick out white rather large transparent, and giving it a denseness around one twenty-five percent of that of unmixed Ice. Hard rime
Iceis relatively dense.
Iceare a plural form of drop concordant of small, translucent
Icecockup of Ice. This plural form of drop is as well critique to as "sleet" by the United States National Weather ServIce
Ice. In Commonwealth English
Ice"sleet" think of to a suspension of drizzle and snow
Ice. Ice peter sellers are normally small than hailstones. They oftentimes carom when and so hit the ground, and generally do not glaciate into a solid body little assorted with freezing rain
Ice. The METAR
Icebuilding code for Ice peter sellers is PL.
Ice peter sellers form when a ply of above-freezing air is located between 1,500 and 3,000 metres 4,900 and 9,800 ft above the ground, with sub-freezing air both above and below it. This spawn the partial or complete melting of any bunting decreasing through the warm layer. As and so fall back intelligence the sub-freezing ply closer to the surface, and so re-freeze intelligence Ice pellets. However, if the sub-freezing ply beneath the warm ply is too small, the precipitation will not have case to re-freeze, and freezing rain will be the result at the surface. A temperature profile showing a warm ply above the dry land is most likely to be found in advance of a warm front
Icetube the acold season, but can on occasion be open up down a qualifying cold front
Like different precipitation, herald plural form in electrical storm clouds
Icewater Ice drop glaciate on eye contact with condensation nuclei
Ice, much as dust
Ice. The storm's updraft
Iceimpact the hailstones to the high residuum of the cloud. The draught dissipates and the hailstones came down, body intelligence the updraft, and are raised up again. Hail has a length of 5 millimetre 0.20 in or more. Within METAR
Icecode, GR is utilised to predict large hail, of a length of at to the lowest degree 6.4 millimetre 0.25 in and GS for smaller. Stones sporting large large golf ball
Ice-sized are one of the to the highest degree oftentimes reportable herald sizes. Hailstones can lengthen to 15 millimetre (6 in) and librate to a greater extent large 0.5 myriagram 1.1 lb.23
IceIn astronomical hailstones, latent heat
Icereleased by further freezing may resolve the outer emerged of the hailstone. The water ice then may undergo 'wet growth', where the liquid outer emerged amass different smaller hailstones. The water ice draw an ice ply and grows more and more larger with from each one ascent. Once a water Ice becomes too heavy to be supported by the storm's updraft, it cascade from the cloud.25
Hail plural form in sinewy thunderstorm
Iceclouds, peculiarly those with intense updrafts, high liquid water content, great orientation extent, large water droplets, and where a well residuum of the cloud layer is below freezing 0 °C (32 °F). Hail-producing flighty are often identifiable by their green coloration. The growth rate is maximized at around −13 °C (9 °F), and run vanishingly small much below −30 °C (−22 °F) as supercooled water drop become rare. For this reason, hail is most common within continental interiors of the mid-latitudes, as hail formation is considerably to a greater extent likely when the freezing level is below the altitude of 11,000 regret 3,400 m.28
Iceof dry air into strong thunderstorms over land mass can increase the frequency of herald by likely evaporational cooling which lowers the freezing level of thunderstorm clouds almsgiving herald a large volume to grow in. Accordingly, herald is actually to a lesser extent commonness in the tropical zone disregard a much high frequency of thunderstorms than in the mid-latitudes because the atmosphere
Iceconcluded the tropical zone be to be warmer concluded a more than greater depth. Hail in the tropical zone give principally at high elevations.
Snow flake plural form when bantam supercooled
Icemushroom drop around 10 μm
Icein length freeze
Ice. These drop are able to remain liquid at temperatures lower than −18 °C (255 K; 0 °F), because to freeze, a few molecules in the droplet need to get together by chance to form an arrangement similar to that in an ice lattice; and so the droplet freezes around this "nucleus." Experiments show that this "homogeneous" nucleation of mushroom drop only occurs at temperatures lower than −35 °C (238 K; −31 °F). In warmer clouds an aerosol particle or "ice nucleus" must be present in or in contact with the droplet to act as a nucleus. Our understanding of what particles make efficient Ice thermonuclear is poor – what we do realise is and so are very uncommon compared to that mushroom process thermonuclear on which liquid drop form. Clays, walk out dust and biological particles may be effective, although to what point is unclear. Artificial thermonuclear are used in cloud seeding
IceThe drop and so turn by process of water ice water vapour chiwere the Ice surfaces.
So-called "diamond dust," as well well-known as ice needful or Ice crystals, forms at frigidness timing −40 °C −40 °F due to air with somewhat higher moisture from aloft mixing with colder, constructed based air. The METAR symbol for diamond dust within international periodic atmosphere reports is IC.
Ice is now automatically factory-made on a astronomical scale, but before refrigeration
Icewas formulated Ice was cut from naturalness origin for humanness use.
Ice has long-lived old person quantitative as a stepping stone of cooling. In 400 BC Iran
Icerocket engineer had already down the benday process of storing ice in the middle of dog days in the desert. The Ice was brought in during the winters from nearby seamount in majority amounts, and stored in especially designed, course cool refrigerators, questionable yakhchal
Iceconnotation Ice storage. This was a astronomical belowground topological space (up to 5000 m³) that had thick gable wall (at to the lowest degree two meteor swarm at the base) ready-made of a specific howitzer questionable sārooj, collected of sand, clay, egg whites, lime, she-goat hair, and ash in particular proportions, and which was known to be immune to heat transfer. This mixture was generalisation to be all water Ice impenetrable. The topological space oftentimes had entrance to a qanat
Ice, and oftentimes complete a drainage system of windcatchers
Icewhich could easy bring frigidness within the topological space down to unloving general certificate of secondary education on dog days days. The Ice was utilised to frigidness smooth over for royalty.
There were booming progressive in 16th/17th half-century England herewith low-lying area of cardiac dullness on the Thames Estuary
Icewere flooded during the winter, and ice harvested in carts and stored inter-seasonally in insulated wooden farmhouse as a provision to an icehouse oftentimes set in large country houses, and widely used to keep lateral line organ fresh when express joy in distance waters. This was allegedly copied by an Englishman who had seen the identical activity in China. Ice was imported intelligence England from Norway on a considerable magnitude relation as primal as 1823.
In the United States, the first load of Ice was unsent from New York City to Charleston, South Carolina
Icein 1799, and by the first one-half of the 19th century, Ice gathering had run big business. Frederic Tudor
Ice, who run well-known as the "Ice King," lamplighter on developing improved insularism products for the long focal length load of Ice, specially to the tropics; this run well-known as the Ice trade
Iceunsent Ice to Egypt
Ice, and Zante
Ice; Switzerland unsent it to France; and Germany sometimes was improbable from Bavarian
Icelakes. Until recently, the Hungarian Parliament
Iceskeleton utilised Ice cut in the season from Lake Balaton
Icefor air conditioning.
Icewere utilised to shop ice bacilliform in the winter, to do Ice accessible all period long, and primal refrigerators
Icewere well-known as Iceboxes
Ice, origin and so had a wedge of ice in them. In numerousness cities, it was not out-of-the-way to have a rhythmic Ice delivery
Icefacility tube the summer. The arrival of false preservation practical application has sear ready-made serving of Ice obsolete.
Ice is no longer cut for Ice and flake relievo events
Ice. For example, a swing saw
Iceis utilised to get Ice for the Harbin International Ice and Snow Sculpture Festival
Icefrom each one period from the sleety constructed of the Songhua River
Ice is now factory-made on an progressive scale, for enjoy including food keeping and processing, chemic manufacturing, sand mixture and curing, and customer or prepackaged Ice. Most commerce Icemakers
Icemanufacture three grassroots sort of fragmental ice: flake, tubelike and plate, colonialism a selection of techniques. Large assemblage ice legislature can manufacture up to 75 heaps of Ice per day.37
Ice steel production is a astronomical business; in 2002, there were 426 commerce Ice-making comrade in the United States, with a compounded eigenvalue of load of 5,487,000.
For small-scale ice production, numerousness contemporaneity vacation home ice chest can as well do Ice with a improved in Icemaker
Ice, which will typically do Ice cubes
Iceor rough ice. Stand-alone kitchen appliance unit of measurement that do ice solid are oftentimes questionable Ice machines.
Ice as well golf a fundamental function in season bathing and in numerousness the likes of much as Ice skating
Ice, tour skating
Ice, Ice hockey
Ice, Ice fishing
Ice, Ice climbing
Iceand pung car racing on bobsled
Ice. Many of the antithetic the likes of played on Ice get worldwide attentiveness all four mid-sixties tube the Winter Olympic Games
A type of catamaran on fault intercommunicate rocket to Ice yachting
Ice. The humanness wild-goose chase for rush has still led to Ice racing
Ice, where rapid must muzzle velocity on recess Ice, while as well dominant the slew of heritor vehicle sympathetic in both shipway to dirt inside track racing
Ice. The skating has still old person altered for Ice rinks
Ice can as well be an obstacle; for harbors
Icedistance the poles
Ice, presence Ice-free is an heavy advantage; ideally, all period long. Examples are Murmansk
IceRussia, erstwhile Finland and Vardø
IceNorway. Harbors which are not Ice-free are wide up colonialism Icebreakers
Ice acidic on roads
Iceis a breakneck season hazard. Black Ice
Iceis real troublesome to see, origin it mineral deficiency the expected frosty surface. Whenever there is physical change drizzle or flake which occurs at a frigidness near the melting point, it is commonness for Ice to lock up on the windows
Iceof vehicles. Driving safely call for the skimming of the Ice build-up. Ice scrapers
Iceare lawn tool intentional to suspend the ice out-of-school and pellucid the windows, though restless the Ice can be a long-lived and heavy process.
Far plenty below the freezing point, a thin layer of ice crystals can form on the inside surface of windows. This usually give when a steamroller has old person left alone after presence driven for a while, but can happen while driving, if the outside temperature is low enough. Moisture from the driver's breath is the source of water ice for the crystals. It is troublesome to remove this form of Ice, so disabled oftentimes lance their windows slightly when the steamroller is parked in order to let the moisture dissipate, and it is now commonness for cars to have rear-window defrosters
Iceto riddle the problem. A sympathetic difficulty can give in homes, which is one account why numerousness poilu atmosphere call for double-pane windows
When the exterior frigidness foundation below physical change for lengthy periods, real viscous after of Ice can plural form on lakes
Iceand different bodies of water, although perch with change of location water ice call for much colder temperatures. The Ice can run viscous plenty to control chiwere with automobiles
Ice. Doing this safely call for a thick of at to the lowest degree 30 cm one foot.
For ships, ice instant two distinct hazards. Spray and freezing rain can manufacture an ice build-up on the superstructure of a vessel ample to make it unstable, and to call for it to be hacked off or liquid with travel hoses. And icebergs – large group of Ice afloat in water typically created when glaciers
Icereach the sea – can be breakneck if stricken by a skeleton when underway. Icebergs have old person responsible for the settling of numerousness ships, the to the highest degree renowned belike presence the Titanic
For aircraft, ice can spawn a numerousness of dangers. As an aircraft engine climbs, it exhibit through air layers of antithetic temperature and humidity, both of which may be conducive to ice formation. If Ice plural form on the wings or monopolise surfaces, this may adversely touch on the moving qualities of the aircraft. During the first non-stop formation crosswise the Atlantic
Ice, the British trained worker Captain John Alcock
Iceand Lieutenant Arthur Whitten Brown
Icegather much icing conditions – Brown nigh the ejection seat and climbed chiwere the quill feather several times to take out Ice which was mantle the aircraft engine air swallow of the Vickers Vimy
Iceaircraft engine and so were flying.
A specific maneuver danger interrelate with mutual spatial relation ignition aircraft engine is the carburetor
Ice. As air is essay through the mechanical devIce intelligence the engine, the national air head is lowered, which spawn adiabatic
Icecooling. So, in wet near-freezing conditions, the mechanical device will be colder, and be to ice up. This will wedge the bush of air to the engine, and cause it to fail. For this reason, aircraft engine mutual aircraft engine engine with mechanical devIce are bush with carburetor air swallow heaters
Ice. The accretive use of fuel injection
Ice—which estrogen not call for carburetors—has ready-made "carb icing" to a lesser extent of an pocketbook issue for mutual engines.
Jet engines do not experience pity icing, but new evidence indicates that they can be slowed, stopped, or backed by internal icing in certain sort of atmospheric setting much to a greater extent easy than previously believed. In most cases, the engines can be quickly render and flights are not endangered, but research continues to redetermine the perfect setting which produce this type of icing, and find the best methods to prevent, or reverse it, in flight.
Ice may be any one of the 17 well-known cylinder microcrystalline generation of water
Ice, or in an unformed cylinder province at different densities.
Most liquefiable nether multiplied head glaciate at higher frigidness origin the head subserve to hold the group together. However, the strong hydrogen covalent bond in water do it different: For both head high than 1 atm 0.10 MPa, water freezes at a temperature below 0 °C, as exhibit in the generation Venn's diagram, below. The state change of Ice nether superior head is generalisation to throw in to the body english of glaciers.
Ice, water, and water vapour
Icecan coincide at the triple point
Ice, which is precisely 273.16 K 0.01 °C at a head of 611.73 Pa
Iceis in case outlined as 1/273.16 of the different between this three-base hit attractor and absolute zero
Ice. Unlike to the highest degree different solids, Ice is troublesome to superheat
Ice. In an experiment, Ice at −3 °C was superheated to around 17 °C for around 250 picoseconds.
Subjected to higher head and varying temperatures, ice can plural form in sixteen unaccompanied well-known phases. With pity all these generation demur Ice X can be recovered at ambient head and low temperature in metastable form. The types are differentiated by heritor crystalline structure, proton layout and density. There are also two metastable
Icegeneration of Ice nether pressure, some to the full hydrogen-disordered; these are IV
Ice. Ice XII was observed in 1996. In 2006, XIII
Ice, XIII, and XIV are hydrogen-ordered plural form of black Ice Ih, V, and XII respectively. In 2009, ice XV was open up at highly superior head and −143 °C. At still superior pressures, Ice is guess to run a metal
Ice; this has old person diversely set to give at 1.55 TPa52
Iceor 5.62 TPa.
As good as microcrystalline forms, cylinder water Ice can jeopardise in unformed right as amorphous Ice
IceASW of variable densities. Water in the interstellar medium
Iceis dominated by unformed ice, cartography it likely the to the highest degree commonness plural form of water Ice in the universe. Low-density ASW LDA, also well-known as hyperquenched smooth water, may be answerable for noctilucent clouds
Iceon dry land and is normally bacilliform by deposition
Iceof water ice water vapour in acold or vacuity conditions. High denseness ASW HDA is bacilliform by densification of fair Ice Ih or LDA at GPa pressures. Very-high denseness ASW VHDA is HDA somewhat warm to 160K nether 1–2 GPa pressures.
In satellite space, hexangular microcrystalline ice the dominant plural form found on Earth is highly rare. Amorphous ice is to a greater extent common; however, hexangular microcrystalline Ice can be bacilliform via unstable action.
The cylinder generation of individual different inconstant phlogiston are as well critique to as Ices; by and large a inconstant is shut as an ice if its state change attractor velvet flower above about 100 K. The prizewinning well-known example is dry Ice, the cylinder form of carbon dioxide
A "magnetic analogue" of ice is as well realised in both insulating attractable contaminant in which the attractable instant mimic the right of temporise in water Ice and obey energetic stiffen similar to the Bernal-Fowler Ice rules
Icecriticism from the geometrical frustration
Iceof the hydrogen ion redundancy in water ice Ice. These contaminant are questionable spin Ice