Before I comment on this, let me get you straight:
In your mind, emissions from an explosion equals chaos? Is that what you're saying?
You asked for an observable chaotic event. An observed supernova qualifies. Other qualifiers are what we already know has happened, example...impact craters. While we didn't technically see the meteor strike we have the evidence left behind which suggest it was quite a chaotic event. Compare nuclear blast craters to meteor craters and you quickly get some what of an understanding. Some what because some nuclear test blast did not yield as much power or damage as some meteors did in our past. Chaotic (what we classify as chaotic) are present throughout our solar system and our galaxy. At any given point "chaotic" events happen throughout our universe.
Atoms:
Why the names to its parts and functions?
I'm not sure what you mean can you clarify? Are you asking for the etymology of the names of the parts?
Do you? Really?
Let's see:
By what process was the difference between this one
and this one, accomplished?
Since you know EXACTLY how they were formed, that should be easy.
The link was given.
Snowflake - Wikipedia, the free encyclopedia
Snowflakes are conglomerations of frozen ice crystals which fall through the Earth's atmosphere. They begin as snow crystals which develop when microscopic supercooled cloud droplets freeze. Snowflakes come in a variety of sizes and shapes. Complex shapes emerge as the flake moves through differing temperature and humidity regimes. Individual snowflakes are nearly unique in structure. Types which fall in the form of a ball due to melting and refreezing, rather than a flake, are known as graupel, with ice pellets and snow grains as examples of graupel.
Snow crystals form when tiny supercooled cloud droplets (about 10 μm in diameter) freeze. These droplets are able to remain liquid at temperatures lower than −18 °C (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; then the droplet freezes around this "nucleus." Experiments show that this "homogeneous" nucleation of cloud droplets only occurs at temperatures lower than −35 °C (−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. The particles that make ice nuclei are very rare compared to nuclei upon which liquid cloud droplets form, however it is not understood what makes them efficient. Clays, desert dust and biological particles may be effective, although to what extent is unclear. Artificial nuclei include particles of silver iodide and dry ice, and these are used to stimulate precipitation in cloud seeding.
Once a droplet has frozen, it grows in the supersaturated environment, which is one where air is saturated with respect to ice when the temperature is below the freezing point. The droplet then grows by deposition of water molecules in the air (vapor) onto the ice crystal surface where they are collected. Because water droplets are so much more numerous than the ice crystals due to their sheer abundance, the crystals are able to grow to hundreds of micrometers or millimeters in size at the expense of the water droplets. This process is known as the Wegner-Bergeron-Findeison process. The corresponding depletion of water vapor causes the droplets to evaporate, meaning that the ice crystals grow at the droplets' expense. These large crystals are an efficient source of precipitation, since they fall through the atmosphere due to their mass, and may collide and stick together in clusters, or aggregates. These aggregates are snowflakes, and are usually the type of ice particle that falls to the ground. Guinness World Records list the world’s largest snowflakes as those of January 1887 at Fort Keogh, Montana; allegedly one measured 38 cm (15 inches) wide. The exact details of the sticking mechanism remain controversial. Possibilities include mechanical interlocking, sintering, electrostatic attraction as well as the existence of a "sticky" liquid-like layer on the crystal surface. The individual ice crystals often have hexagonal symmetry. Although the ice is clear, scattering of light by the crystal facets and hollows/imperfections mean that the crystals often appear white in color due to diffuse reflection of the whole spectrum of light by the small ice particles
A non-aggregated snowflake often exhibits six-fold "radial" symmetry. The initial symmetry occurs because the crystalline structure of ice is six-fold. The six "arms" of the snowflake then grow independently, and each side of each arm grows independently. Most snowflakes are not completely symmetric. The micro-environment in which the snowflake grows changes dynamically as the snowflake falls through the cloud, and tiny changes in temperature and humidity affect the way in which water molecules attach to the snowflake. Since the micro-environment (and its changes) are very nearly identical around the snowflake, each arm grows in nearly the same way. Since the micro-environment of one snowflake is not the same as the micro-environment of a different snowflake, it is very unlikely that two snowflakes will be identical.
So yes, we know the mechanisms and the processes as to how they form and what they look like after formation. Nothing in it denotes design even though we perceive each one as a complex structure. While all of this, again, is high school textbook information....it (the notion of design) has pretty much nothing to do with the fossil record.
Thanks for the link. :jiggy:
