By Ben Phillips

"It doesn't subject that you're grotesque and feature a small d!#k, you'll nonetheless have ladies throwing themselves at you! Won't you!"

Welcome to Uber using - and this hilarious and poignant account of riding Sydneysiders to and from destinations wild, recognized and notorious. Uber drivers get an intimate glimpse into people's lives - from their morning exercises to their melancholy after being ditched on the pub (see gruesome dick comments). They act as sounding forums, take the rap for loud tune, see humans at their best and weakest, and most significantly get to monitor a solid of completely amazing characters that make a massive city.

From Jacob the hire boy to Lydia the neglectful, the trendy Uber driving force sees all of it. And whilst humans ask our driving force why doesn't he get a true task, he thinks of the wonderful tales he will get on a daily basis, and says, "No thanks."

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The nucleation of one phase crystal growth rate vs. increasing superresults in rapid growth of a crescumulate layer saturation. The growth rate curve (so#d outwards into the supersaturated melt, and #ne) peaks at lower degrees of supersaturesults in the eventual buildup of rejected ration than does the nucleation curve components to the point where a second phase (dashed curve). In a crystal-free system, nucleates and forms a second layer (Figure 11). supersaturation will increase until suffiIn any mechanism dependent upon differcient nucleation occurs to allow crystal ences in nucleation rates to cause differences in growth to decrease the degree of supermodal abundances, layers with greater abunsaturation.

24 ! " ! ,, B t2 A B A Figure 13. (a). Initial crystallization across a zone with a temperature gradient results in 10% crystallization at the hot end and 50% crystallization at the cooler end for an initial uniform bulk composition at X denoted by the so#d vertical #ne. The composition of the interstitial #quid (denoted by open circles) will follow the liquidus curve, and the composition of the solid (denoted by filled circles) will be pure A. (b). Migration of component A down its compositional gradient towards the cooler end and component B down its compositional gradient toward the hot end will promote increased crystallization at the cooler end and dissolution at the hot end.

Taubeneck and Poldervaart (1960) and McBirney and Noyes (1979) proposed a mechanism involving diffusion of heat and chemical components in the boundary layer Figure 11. A plot of temperature vs. disat the margin of a magma chamber to form tance for a profile through a crystallization rhythmic layering. ~'ont in which the #quidus temperature in of a mineral nucleate and begin to grow, the the adjacent magma is depressed by the components that make up that mineral will addition of rejected components at the crysdiffuse towards the growing crystals forming tal-liquid interface.

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