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After an introduction, possibly explaining how to identify the first nagu, the next seven nagu are each introduced by the clause "To the n-th region [nagu], where you travel 7 leagues" (the distance of 7 leagues seems to indicate the width of the Ocean, rather than the distance between subsequent nagu).
Badenhorst was born in Pietermaritzburg in the then Natal Province on 6 December 1967. He was one of four children. Badenhorst completed high school at Hoërskool Waterkloof, Pretoria, in 1985 and subsequently went to work for the South African Government Printing Works.
Thus if N = 300,000,000 (90% of the US population, with 10% of population being too young to participate) and K = 30 then Degrees of Separation = APL = 19.5 / 3.4 = 5.7 and if N = 7,200,000,000 (90% of the world population, with 10% of population being too young to participate) and K = 30 then Degrees of Separation = APL = 22.7 / 3.4 = 6.7.
Only takes 3 or 5, depending on direction. George W. Bush → MIT is 3 or 2. smurrayinchester , 16:16, 5 March 2006 (UTC) Aliens to Vimes There is, according to kate's tool, no path under 10 steps between these articles, however the return path, Vimes to Aliens is only 4 degrees - none of which are date related. Chrisboote
There is no clear relationship between the size of soil mineral components and their mineralogical nature: sand and silt particles can be calcareous as well as siliceous, [18] while textural clay (0.002 mm (7.9 × 10 −5 in)) can be made of very fine quartz particles as well as of multi-layered secondary minerals. [19]
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These terms refer to the quality that the permeability value in question is an intensive property of the medium, not a spatial average of a heterogeneous block of material equation 2.28 [clarification needed] [further explanation needed]; and that it is a function of the material structure only (and not of the fluid).
A sample of a material is called dilative if its volume increases with increasing shear and contractive if the volume decreases with increasing shear. [7] [8] Dilatancy is a common feature of soils and sands. Its effect can be seen when the wet sand around the foot of a person walking on beach appears to dry up.