Changes

604 bytes added ,  02:36, 13 December 2020
m
Text replacement - "http://" to "https://"
Line 2: Line 2:     
==Etymology==
 
==Etymology==
[http://nordan.daynal.org/wiki/index.php?title=English#ca._1100-1500_.09THE_MIDDLE_ENGLISH_PERIOD Middle English], from Anglo-French, soil, piece of land, from Vulgar Latin *solium, alteration of [[Latin]] solea sole, sandal, [[foundation]] timber
+
[https://nordan.daynal.org/wiki/index.php?title=English#ca._1100-1500_.09THE_MIDDLE_ENGLISH_PERIOD Middle English], from Anglo-French, soil, piece of land, from Vulgar Latin *solium, alteration of [[Latin]] solea sole, sandal, [[foundation]] timber
   −
*Date: [http://www.wikipedia.org/wiki/14th_Century 14th century]
+
*Date: [https://www.wikipedia.org/wiki/14th_Century 14th century]
 
==Definitions==
 
==Definitions==
 
*1 : firm land : [[earth]]
 
*1 : firm land : [[earth]]
Line 13: Line 13:  
*5 : a [[medium]] in which something takes hold and [[develops]]
 
*5 : a [[medium]] in which something takes hold and [[develops]]
 
==Description==
 
==Description==
'''Soil''' is a [[natural]] [[body]] consisting of layers (soil horizons) of mineral [[constituents]] of variable thicknesses, which differ from the [[parent]] [[materials]] in their [http://en.wikipedia.org/wiki/Geomorphology morphological], [[physical]], [[chemical]], and [http://en.wikipedia.org/wiki/Mineralogical mineralogical] characteristics.
+
'''Soil''' is a [[natural]] [[body]] consisting of layers (soil horizons) of mineral [[constituents]] of variable thicknesses, which differ from the [[parent]] [[materials]] in their [https://en.wikipedia.org/wiki/Geomorphology morphological], [[physical]], [[chemical]], and [https://en.wikipedia.org/wiki/Mineralogical mineralogical] characteristics.
   −
It is [[composed]] of [[particles]] of broken rock that have been altered by [[chemical]] and [[environmental]] [[processes]] that include weathering and erosion. Soil [[differs]] from its [[parent]] rock due to [[interactions]] between the [http://en.wikipedia.org/wiki/Lithosphere lithosphere], [http://en.wikipedia.org/wiki/Hydrosphere hydrosphere], [[atmosphere]], and the [http://en.wikipedia.org/wiki/Biosphere biosphere].
+
It is [[composed]] of [[particles]] of broken rock that have been altered by [[chemical]] and [[environmental]] [[processes]] that include weathering and erosion. Soil [[differs]] from its [[parent]] rock due to [[interactions]] between the [https://en.wikipedia.org/wiki/Lithosphere lithosphere], [https://en.wikipedia.org/wiki/Hydrosphere hydrosphere], [[atmosphere]], and the [https://en.wikipedia.org/wiki/Biosphere biosphere].
    
It [[supports]] a [[complex]] [[ecosystem]], which supports the plants on the [[surface]] and creates new soil by breaking down rocks and sand. This microscopic ecosystem has co-evolved with the plants to [[collect]] and store [[water]] and [[nutrients]] in a [[form]] usable by plants.
 
It [[supports]] a [[complex]] [[ecosystem]], which supports the plants on the [[surface]] and creates new soil by breaking down rocks and sand. This microscopic ecosystem has co-evolved with the plants to [[collect]] and store [[water]] and [[nutrients]] in a [[form]] usable by plants.
   −
Soil particles pack loosely, forming a soil [[structure]] filled with pore spaces. These pores contain soil [http://en.wikipedia.org/wiki/Solution solution] (liquid) and air ([[gas]]). Accordingly, soils are often treated as a [[three]] [[state]]-[[system]]. Most soils have a [[density]] between 1 and 2 g/cm³. Soil is also known as [[earth]]: it is the substance from which our [[planet]] takes its name. Little of the soil [[composition]] of planet [[Earth]] is older than the [http://en.wikipedia.org/wiki/Tertiary Tertiary] and most no older than the [http://en.wikipedia.org/wiki/Pleistocene Pleistocene]. In engineering, soil is referred to as regolith, or loose rock [[material]].
+
Soil particles pack loosely, forming a soil [[structure]] filled with pore spaces. These pores contain soil [https://en.wikipedia.org/wiki/Solution solution] (liquid) and air ([[gas]]). Accordingly, soils are often treated as a [[three]] [[state]]-[[system]]. Most soils have a [[density]] between 1 and 2 g/cm³. Soil is also known as [[earth]]: it is the substance from which our [[planet]] takes its name. Little of the soil [[composition]] of planet [[Earth]] is older than the [https://en.wikipedia.org/wiki/Tertiary Tertiary] and most no older than the [https://en.wikipedia.org/wiki/Pleistocene Pleistocene]. In engineering, soil is referred to as regolith, or loose rock [[material]].
 
==See also==
 
==See also==
*'''''[[Sky]]'''''
+
*'''''[[Clouds]]'''''
 +
 
 +
==Quote==
 +
For only when you [[experience]] the [[stillness]] are you in complete [[knowledge]] of His [[presence]] and only as you carry your [[understanding]] of [[grace]] with you into your arena are you capable of maintaining that [[quality]] which allows you to prevail with men in such a way as to [[maintain]] your own sense of [[balance]] and [[solidarity]] -- that is to say: your head in the [[clouds]] and your feet on the [[ground]] -- and this condition is [[evidence]] of a well-unified [[personality]] operating in the fullest [[capacity]] known to him at that time. - Tomas
 +
 
 
[[Category: Earth Science]]
 
[[Category: Earth Science]]