Chamberlin–Moulton planetesimal hypothesis
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. Though the Chamberlin–Moulton hypothesis is no longer accepted, the idea of planetesimals remains in modern theory.
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Chamberlin–Moulton planetesimal hypothesis
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. Though the Chamberlin–Moulton hypothesis is no longer accepted, the idea of planetesimals remains in modern theory.
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The Chamberlin–Moulton planete ...... mals remains in modern theory.
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張伯倫莫頓假說是地質學家和天文學家弗雷斯·雷·莫頓在1905 ...... 倫莫頓假說已經被摒棄,但微行星的想法依然留存在現在的理論中。
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The Chamberlin–Moulton planete ...... mals remains in modern theory.
@en
張伯倫莫頓假說是地質學家和天文學家弗雷斯·雷·莫頓在1905 ...... 倫莫頓假說已經被摒棄,但微行星的想法依然留存在現在的理論中。
@zh
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Chamberlin–Moulton planetesimal hypothesis
@en
張伯倫莫頓假說
@zh