The boundary between the Earth's crust and mantle is the planet's equalisation shell — and from its radius come the fine structure constant, hydrogen's ruler, the year the stars mark, the sidereal day and a colour of light
The crust–mantle boundary sits at twenty thousand over π kilometres from the centre of the Earth, and so its circumference is forty thousand kilometres exactly. The Earth's dimensional mass, 1875/π, divided by 9375 is the same shell: the node reports its own radius.
Read in degrees, the Moho is the base unit of hydrogen's spectrum; doubled, it is α. Hydrogen's Balmer-α line run off the two faces of its constant returns the Moho's top and bottom: a seam one G-bond step thick.
The shell one helical turn above the Moho is 6396.0802 km. The 29.88 km gap between them is the year the stars mark, 365.2566126366; the radius as a mass is light on G2, and squared through the hours it is the sidereal day. The volume inside the Moho, through the veil, is the orange/red boundary of the spectrum, 619.2294611 nm.
The boundary between the Earth's crust and mantle. In the Universal Force of Time it is the Earth's equalisation shell, at 20000/π = 6366.1977 km.
Because its radius is 20000/π: carried once round the circle, the π cancels and leaves 40,000 km exactly.
The Moho read through the veil is 3600/π², the base unit of hydrogen's spectrum; doubled it is α, so 1/α = 137.0778389.
Nothing on this page was pulled, attracted or held down. There is one substance — time — flowing from the sparse toward the dense, and the radio whisper of cold hydrogen and the slow turning of Mercury are one thread of its pattern. If it stirred your curiosity, the whole weave is waiting: the planets, the atom, light, life and number, all carried by the same single force.
Read the whole theory of the Universal Force of Time →