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1		-XWiki.terraindex
	1	+XWiki.RoelofZwaan

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23	23	The secondary fraction lies between 5 and 50 % of the same material. At 5% > 20% of the same material one can speak of a weak presence of the material. At 20%>50% of the same material one can speak of a strong presence of the material. There is a possibility to add a second secondary component, but that is also the maximum of secondary components that can be present.
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25		-== [[Gradation>>doc:Eigenschappen.Soil boundaries.WebHome]] ==
	25	+== [[Gradation>>doc:Characteristics .Soil boundaries.WebHome]] ==
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27	27	When the material has abrupt transition into the primary or tertiary fraction the gradation is called weak. With a strong gradation the border between materials is less clear and the clast size changes gradually.
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174	174	Detritus is particles of rock derived from pre-existing rock through processes of weathering and erosion. Detritus can also be dead organic material.
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176		-== [[Dolerite>>doc:Rock types.Igneous rocks.Extrusive igneous rocks.Dolerite.WebHome]] ==
	176	+== [[Dolerite>>doc:Rock types.Igneous rocks.Extrusief stollingsgesteente.Dolerite.WebHome]] ==
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178	178	Dolerite is an igneous rock with a silica amount of 48 till 52%. The minerals present in dolerite are: olivine, plagioclase, biotite, amphiboles and pyroxenes.
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