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  2. Planetesimal - Wikipedia

    en.wikipedia.org/wiki/Planetesimal

    The dividing line between a planetesimal and protoplanet is typically framed in terms of the size and the stages of development that the potential planet has already gone through: planetesimals combine to form a protoplanet, and protoplanets continue to grow (faster than planetesimals). [13] [14] [15]

  3. Protoplanet - Wikipedia

    en.wikipedia.org/wiki/Protoplanet

    A protoplanet is a large planetary embryo that originated within a protoplanetary disk and has undergone internal melting to produce a differentiated interior. Protoplanets are thought to form out of kilometer-sized planetesimals that gravitationally perturb each other's orbits and collide, gradually coalescing into the dominant planets .

  4. List of planet types - Wikipedia

    en.wikipedia.org/wiki/List_of_planet_types

    Protoplanet: A large planetary embryo that originates within protoplanetary discs and has undergone internal melting to produce differentiated interiors. Protoplanets are believed to form out of kilometer-sized planetesimals that attract each other gravitationally and collide. PDS 70 b and c, AB Aurigae b: Puffy planet

  5. Accretion (astrophysics) - Wikipedia

    en.wikipedia.org/wiki/Accretion_(astrophysics)

    [5] [6] Since then, the model has been further developed using intensive numerical simulations to study planetesimal accumulation. It is now accepted that stars form by the gravitational collapse of interstellar gas. Prior to collapse, this gas is mostly in the form of molecular clouds, such as the Orion Nebula.

  6. Pebble accretion - Wikipedia

    en.wikipedia.org/wiki/Pebble_accretion

    Nonetheless, formation via planetesimal collisions can be accomplished within the typical lifetime of a protoplanetary disc. [ 14 ] [ 15 ] The largest planetesimals can grow much faster via pebble accretion, [ 10 ] but if the formation or delivery of pebbles is rapid numerous Earth-mass planets form instead of a few giant planet cores. [ 16 ]

  7. Moon's giant crater created by huge protoplanet collision

    www.aol.com/news/2016-07-21-moons-giant-crater...

    The huge indent, called the 'imbrue basin,' stretches across 750 miles.

  8. History of Solar System formation and evolution hypotheses

    en.wikipedia.org/wiki/History_of_Solar_System...

    In 1944, German chemist and physicist Arnold Eucken considered the thermodynamics of Earth condensing and raining-out within a giant protoplanet at pressures of 100–1000 atm. In the 1950s and early 1960s, discussion of planetary formation at such pressures took place, but Cameron's 1963 low-pressure (c. 4–10 atm.) model largely supplanted ...

  9. Protoplanetary disk - Wikipedia

    en.wikipedia.org/wiki/Protoplanetary_disk

    Protoplanetary disk. Simulated spiral arm vs observational data. [9] Protoplanetary disks around T Tauri stars differ from the disks surrounding the primary components of close binary systems with respect to their size and temperature. Protoplanetary disks have radii up to 1000 AU, and only their innermost parts reach temperatures above 1000 K.