Alternating planetary phase layers

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  • Thread starter Thread starter Loren Booda
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SUMMARY

Terrestrial planets typically consist of solid layers with a liquid core, while gaseous planets are predominantly liquid with a solid core. The discussion explores the possibility of planetoids exhibiting alternating layers of solid and liquid materials, referencing moons such as Europa, Ganymede, and Callisto as potential examples. The Earth itself is structured in four distinct layers: the crust, mantle, outer core, and inner core, each with varying states of matter due to temperature and pressure. The conversation emphasizes the importance of understanding phase diagrams and geophysical equations to predict the composition and state of matter in planetary bodies.

PREREQUISITES
  • Understanding of planetary geology and structure
  • Familiarity with phase diagrams and their applications
  • Knowledge of geophysical equations related to equilibrium conditions
  • Basic chemistry principles relevant to planetary composition
NEXT STEPS
  • Research the geological structures of Europa and Ganymede
  • Study phase diagrams for various compounds under different temperature and pressure conditions
  • Explore geophysical equations used in planetary science
  • Investigate the chemistry of planetary materials and their implications for planetary formation
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Astronomers, planetary scientists, geologists, and anyone interested in the composition and structure of celestial bodies.

Loren Booda
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Terrestrial planets in general are solid, or solid with a liquid core. Gaseous planets in general are liquid, or liquid with a solid core.

Can there be planetoids with substantial alternating layers of solid - liquid - solid, or liquid - solid - liquid? (I do not consider Earth's hydrosphere as substantial in this regard.) I believe there are some known moons which qualify.
 
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As I understand it, the Earth has a gaseous atmosphere, over much of its expanse, a liquid ocean, a solid crust, liquid rock pockets, a solid layer, a liquid layer, and a solid metal core.

The Earth is made of four layers. We live on the earth’s crust made of rocks broken into small pieces. The continents, ocean floors, mountains, and valleys of the earth’s surface are in the earth’s crust. Below the crust there are pockets of melted rock. Under the melted rock is the mantle. The mantle is made of solid hot rock with temperatures from 900 to 3000 degrees Celsius. The outer core is the third layer. It is liquid metal melted from temperatures between 3000 and 4000 degrees Celsius. The inner core at the center of the Earth is solid metal and the temperature is between 3000 and 6500 degrees Celsius.


http://volcano.und.nodak.edu/vwdocs/kids/volcano_project/volcanoes.html

I see no reason why this couldn't happen elsewhere.
 
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Europa (certainly), Ganymede (almost certainly), and Callisto (maybe) are all at least solid-liquid-solid.

The state which matter is in depends (at least) on its composition (mix of compounds), temperature, and pressure; with a huge set of inputs of the physical properties (e.g. phase diagrams) of a great many compounds, the appropriate geophysical equations (for determining equilibrium conditions), and a lot of patience you could have a lot of fun making all kinds of strange planets! Oh, and making sure you get all the chemistry right too will earn you extra gold stars!
 

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