CHAMBETLIN MOULTEN
THEORY?????
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The Chamberlin–Moulton planetesimal hypothesis was proposed in 1905 by geologist Thomas Chrowder Chamberlin and astronomer Forest Ray Moulton to describe the formation of the Solar System. It was proposed as a replacement for the Laplacian version of the nebular hypothesis that had prevailed since the 19th century.
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A widely accepted theory of planet formation, the so-called planetesimal hypotheses, the Chamberlin–Moulton planetesimal hypothesis and that of Viktor Safronov, states that planets form from cosmic dust grains that collide and stick to form ever-larger bodies.
Thomas Chrowder Chamberlin, (born Sept. 25, 1843, Mattoon, Ill., U.S.—died Nov. 15, 1928, Chicago), U.S. geologist and educator who proposed the planetesimal hypothesis, which held that a star once passed near the Sun, pulling away from it matter that later condensed and formed the planets.
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