Summary
of properties:
Hadean
worlds are relatively rare in planetary systems, they are generally of
terrestrial planet composition and because of the extreme amount of
energy in their systems they are in constant volcanic upheaval. Often
there surface is racked with lava, though plates may exist on the
surface they are relatively thin and short lived, and always undergoing
change from volcanoes punctuating there surfaces or from meteoric
collisions. Hadean worlds are in short the first chapter of every
terrestrial planets creation.
Detailed
description:
These
types of worlds are present generally only in the early stages of solar
system development, growing from planetesimal impacts these worlds are
constantly bombarded from collisions with small and occasionally large
celestial bodies. Though the violence from these events may be able to
eject some of the material from these early planet’s gravity well,
most of the material is recaptured and the planet slowly grows.
The
term micro-Hadean is used to describe a celestial object that is well on
the way to form a full sized terrestrial planet (roughly between 500km,
and 5000km), with further growth these small planets may grow on to more
interesting stages of development, if however the source of their growth
material disappears their path will change, lacking enough mass to
retain an atmosphere there once molten, out-gassing surface cools and
hardens, these airless bodies pass into a second category in planetary
description, Mercurian, named after the archetypal example Mercury.
Though Micro-Hadeans are the origins for most of these types of bodies,
most micro-Hadeans follow other evolutionary pathways.
In
the disorganized chaos in protoplanetary discs many of these young
bodies will be gobbled up by the sun or flung out of the solar system,
some however go on to gain more mass from the environment and become
fully fledged Hadeans. The important transition is when the planet has
enough mass to retain an atmosphere, the initial atmosphere may be very
unpleasant from a biological point of view being a brew of gases from
the molten rock of the planet’s composition, but this insulating layer
is enough for the planet to develop more interesting lifecycles.
If
the planet is close enough to the sun the combination of initial
atmosphere and huge amount of heat input form the sun maybe enough to
keep the planet molten well after the initial surface bombardment has
finished, these types of Hadeans are described as ‘perpetual’
Hadeans, though this name could not be further from the truth. Though
these planets may exist in this molten state for a long time, the
ferocity of the sun’s local presence may be enough to strip the
atmosphere from the planet over time, and expose the surface to cool,
and eventually turn such a planet into a Mercurian, or if the planet is
closer still to the sun, its extensive atmosphere may slow the planet in
its path and lead to orbital decay where it falls into the sun. Some
perpetual Hadeans around appropriate stars may also have a third option,
this is particularly true for low mass stars whose birth may be
spectacular and bright, but whose main existence will be dim and cool.
When the heating from the sun declines the long wracked Hadean will
slowly cool putting it back onto the pathway from which other planetary
types can evolve.
Though
Hadean planet may be still surfaced with seething lava, the planet’s
composition and location have in part decided its fate. A large Hadean,
large enough to maintain its atmosphere that is, basically has two
initial pathways, firstly to cool down and become proto-Gaian, or
secondly to generate thick greenhouse like atmosphere, and become
Venusian.
As
the energy from the planet’s initial formation is radiated away or
dissipated the planet will slowly move out it’s brief (in terms of
total lifecycle) Hadean phase into one of the paths available to it,
however though the Hadean phase is the start of every world, many worlds
end in the same manner as their sun expands and roasts them back to the
stage they started their lives, these final lava wracked planets are
called ‘end-stage’ Hadeans, and are usually brief as either the sun
consumes the inner terrestrial planets, or the sun dims and dies,
freezing the world now stripped of its atmosphere. |