| 
	
	
		|    J. Marvin 
		Herndon's Early Earth Formation as a Jupiter-like Gas Giant
 |  Various hypotheses about the origin of the Sun and planets, 
since the 18th Century, generally fall into one of two categories that involve 
either (1) condensation at high-pressures, hundreds to thousands of atmospheres; 
or (2) condensation at very low pressures, one ten-thousandth of an atmosphere. The presently popular idea that Earth formed from matter that 
condensed at low pressure, one ten-thousandth of an atmosphere began in 1963 as 
an assumption-based model [1] and was built-upon with other assumption-based 
models. Basically the idea is this: Dust would condense from the gas, form 
dust-balls, then grains, then rocks, then planetesimals, and finally planets. 
But it is not correct. Why? Because such condensation would lead highly oxidized 
matter which would form planets 
having insufficiently massive cores [14]. 
		  Thermodynamic 
considerations led Arnold Eucken [2], pictured at left, to conceive of Earth 
formation at high pressures and high temperatures from within a giant, gaseous 
protoplanet with molten-iron first raining out to form the core, then followed 
by the condensation of the silicate-rock mantle. Figure at right shows the phase 
		boundary between liquid iron and a gas of primordial composition in the 
		range considered by Eucken. 
		J. Marvin Herndon and Hans E. Suess verified those calculations and showed that similar 
circumstances would explain the oxygen-starved composition of enstatite 
chondrite meteorite minerals [3]. Herndon subsequently showed that the interior 
of Earth below a depth of 660 km resembles an enstatite chondrite [4-11]. Later, 
Herndon extended Eucken's idea to complete condensation of Earth as a 
Jupiter-like gas giant [12-16]. The discovery of close-to-star gas giant 
exo-planets lends support to Herndon's idea that Earth originated as as 
Jupiter-like gas giant. 
 Herndon's concept of Earth formation is illustrated at right. Image from 
left to right, 1) Earth rains out in the center of a giant 
gaseous protoplanet; 2) Fully formed Jupiter-like gas giant 
Earth; 3) As the thermonuclear reactions in the Sun ignite, 
violent super-intense T-Tauri phase solar winds strip away the gases, leaving;
4) Earth, compressed by about 300 Earth-masses of gas, will 
eventually decompress from 64% the diameter of; 5) present-day 
Earth; 6) Jupiter is shown for size-scale. 
 Envision 
pre-Hadien Earth, compressed to about 64% of its present radius by about 300 
Earth-masses of primordial gases and ices. At some point, after being stripped 
of its massive volatile envelope, presumably by the Sun's super-intense T-Tauri 
solar winds, internal pressures would build eventually cracking the rigid crust. 
Powered by the stored energy of protoplanetary compression, Earth's progressive 
decompression, illustrated by the image at left, is the principal engine that 
drives surface geology. J. Marvin Herndon's new geodynamic theory, called
whole-Earth decompression dynamics [17-19], explains 
the myriad measurements and observations whose descriptions are attributed to 
plate tectonics, but without requiring physically-impossible mantle convection 
[20, 21], and explains even more, such as the origin of mountains and the primary initiation of submarine 
canyons [22]. 
For a more detailed WebPage on Whole-Earth 
Decompression Dynamics  
click here. 
Return to Home Page NuclearPlanet.com 
	
		| References |  
		| 1. | Cameron, A. G. W., Formation of the solar nebula. Icarus, 1963,
		1, 339-342. |  
		| 2. | 
		Eucken, A., Physikalisch-chemische Betrachtungen ueber die frueheste 
Entwicklungsgeschichte der Erde. Nachr. Akad. Wiss. Goettingen, Math.-Kl., 
1944: p. 1-25. |  
		| 3. | Herndon, J. M. and Suess, H. E., Can enstatite chondrites form from a 
		nebula of solar composition. Geochimica et Cosmochimica Acta, 
		1976, 40, 395-399. |  
		| 4. | Herndon, J. M., The nickel silicide inner core of the Earth. 
		Proceedings of the Royal Society of London, 
		1979, 
		A368, 495-500. (click here for pdf) |  
		| 5. | Herndon, J. M., 
		 
		
The chemical 
		composition of the interior shells of the Earth.
		Proceedings of the Royal Society of London, 
		1980, 
		A372, 149-154. (click here for pdf) |  
		| 6. | Herndon, J. M., The object at the centre of the Earth. 
		Naturwissenschaften, 
		1982, 
		69, 34-37. |  
		| 7. | Herndon, J. M.,  
		 
		Feasibility of a 
		nuclear fission reactor at the center of the Earth as the energy source 
		for the geomagnetic field. Journal of Geomagnetism and Geoelectricity, 
		1993, 45, 423-437.  
		(click here for pdf) |  
		| 8. | Herndon, J. M., Sub-structure of the inner core of the Earth. 
		Proceedings of the National Academy of Sciences USA, 
		1996,  
		93, 646-648. 
		 (click here for pdf) |  
		| 9. | Herndon, J. M.,   
		 Composition of 
		the deep interior of the Earth: Divergent geophysical development with 
		fundamentally different geophysical implications.
		 
		 Physics of the 
		Earth and Planetary Interiors, 
		1998, 
		105, 1-4. |  
		| 10. | Herndon, J. M., 
		 
		
Scientific 
		basis of knowledge on Earth's composition.
		Current Science, 
		2004, 
		88, 1034-1037. 
		(click here for pdf) |  
		| 11. | Herndon, J. M., Chemical basis of deep-Earth physics: Emphasis on the 
		core-mantle boundary D''. 2011, arXiv: 1101.5085
		(click here for pdf) |  
		| 12. | 
		Herndon, J. M., Solar System formation deduced from observations of 
matter. arXiv:astro-ph/0408151  9 Aug 2004.
		(click here for pdf) |  
		| 13. | 
		Herndon, J. M., Protoplanetary Earth formation: further evidence and 
geophysical implications. arXiv:astro-ph/0408539  30 Aug 2004, 2004.
		(click here for pdf) |  
		| 14. | 
		Herndon, J. M., Solar System processes underlying planetary formation, 
geodynamics, and the georeactor. Earth, Moon and Planets, 2006, 
		99, 53-99. (click here for pdf) |  
		| 15. | 
		Herndon, J. M., Maverick's Earth and Universe. 2008, Vancouver: 
Trafford Publishing, ISBN 978-1-4251-4132-5. |  
		| 16. | 
Herndon, J. M., 
		Nature of planetary matter and magnetic field generation in the Solar 
		System. Current Science, 2009, 
		96, 1033-1039. (click here for pdf) |  
		| 17. | Herndon, J. M., Whole-Earth decompression dynamics. 
		Current 
 Science, 2005. 89(10), 1937-1941. 
		 
 (click here for pdf) |  
		| 18. | 
		Herndon, J. M., Energy for geodynamics: Mantle decompression thermal 
tsunami. Current Science, 2006, 
		90, 1605-1606.
		(click here for pdf) |  
		| 19. | Herndon, J. M., Impact of recent discoveries on petroleum and natural 
		gas explaration: Emphasis on India. Current Science, 2010,
		98, 772-779. (click here for pdf) |  
		| 20. | Herndon, J. M., 
		Uniqueness of 
		Herndon's georeactor: Energy source and production mechanism for Earth's 
		magnetic field. 2009, arXiv:0901.4509 (click here for pdf) |  
		| 21. | Herndon, J. M., Geodynamic basis of heat transport in the Earth.
 Current Science, 2011, 
		101, 1440-1450.
		(click here for pdf) |  
		| 22. | Herndon, J. M., Origin of mountains and primary initiation of submarine canyons: 
		Consequences of Earth's early formation as a Jupiter-like gas giant. Current Science, 
		2012, 102, 1370-1372. (click here for pdf) |  |