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No beginning No End 

Like a circle 
 no beginning no end 
time is circular 
karma is what go goes around comes around 
love is start and has no end.
It just got origin the very minute
point encircling the whole life. #NojotoQuote

circle
#lovelife #Loads #circle #instago #Love #beginning #End #start #Origin

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Wiash You And Your Family A Bombastic Diwali Have loads of Fan And  Loads of Masti
Happy Diwali

 

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Wiash You And Your Family A Bombastic Diwali Have loads of Fan And  Loads of Masti
Happy Diwali

 

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Difference between Rock and Soil music:

Soil and rock are composed of similar materials, but differ in their structure.

Rock (in this instance massive bedrock or floating rock formations) has properties defined by the existing failure surfaces - i.e. cracks in the rock formation. Typical rock formations have one or more series of parallel cracks or fracture planes that define the capacity of the rock to support given loads.

Soils, on the other hand, consist of weathered rock particles. The difference between rock and soil will depend on the scope of your analysis. For example, a rock that has small particles in the cracks noted above may perform more like a soil, while a high gravel- or cobble-containing soil mass may perform more like rock that a soil.

Coherence between components is the main affair in this.area. rock is solid, coherent enough so you cannot break its components away without a hard enough tool. Soil is not coherent enough to resist lateral presure, or hiting parts of it without any tool, just a stone your shoes, or even your hands, ussually, aside some draught or pressure hardened soil classes.

The weathered rock particles can raise from cobble-sized (6+ inch particle size) to clay-sized (0.075 inch or smaller particle size). In a soil, the behavior of how the individual particles interact define the capacity of the soil to support loads. This includes friction angles and normal loads (granular soils - cobbles, gravels, and sands) or cohesion (bonding by particles in the presence of water - clay soils and to an extent, silt soils). The strength is defined by the INTERACTION, not the material, in a soil.

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