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  2. Zappos - Wikipedia

    en.wikipedia.org/wiki/Zappos

    zappos.com. Zappos.com is an American online shoe and clothing retailer based in Las Vegas, Nevada, United States. [1] The company was founded in 1999 by Nick Swinmurn and launched under the domain name Shoesite.com. In July 2009, Amazon acquired Zappos in an all-stock deal worth around $1.2 billion at the time.

  3. Rebate (marketing) - Wikipedia

    en.wikipedia.org/wiki/Rebate_(marketing)

    Not all buyers remember to mail the coupons, a phenomenon known in the industry as breakage, or the shoebox effect. Though it can be used interchangeably with breakage , [20] slippage is the phenomenon when a consumer has his or her rebate fulfilled, but he or she loses or forgets to cash the check.

  4. Copper - Wikipedia

    en.wikipedia.org/wiki/Copper

    Copper alloys are widely used in the production of coinage; seen here are two examples - post-1964 American dimes, which are composed of the alloy cupronickel and a pre-1968 Canadian dime, which is composed of an alloy of 80 percent silver and 20 percent copper.

  5. JD.com - Wikipedia

    en.wikipedia.org/wiki/JD.com

    JD.com started the e-book selling business online on 20 February 2012, and provided customers with more than 80,000 electronic books. JD.com also offered discounts to the buyers, this situation was the unfoldment of a new round of price war. On 17 April 2013, most of the e-books on Dangdang's website were free for users to download.

  6. KGW - Wikipedia

    en.wikipedia.org/wiki/KGW

    KGW (channel 8) is a television station in Portland, Oregon, United States, affiliated with NBC and owned by Tegna Inc. The station's studios are located on Jefferson Street in southwestern Portland, and its transmitter is located in the city's Sylvan-Highlands section. KGW also served as the Portland bureau for co-owned regional news channel ...

  7. Surface runoff - Wikipedia

    en.wikipedia.org/wiki/Surface_runoff

    Surface runoff (also known as overland flow or terrestrial runoff) is the unconfined flow of water over the ground surface, in contrast to channel runoff (or stream flow).It occurs when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil.

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