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  2. Edmund Lowe - Wikipedia

    en.wikipedia.org/wiki/Edmund_Lowe

    In fact, Lowe's career was stalling as early as 1938, when the actor was too mature to play most romantic leads. His last such role was in 1937's Every Day's a Holiday, in which the 48-year-old Lowe played opposite the 44-year-old Mae West. Lowe shifted gears and began playing strong supporting roles in major films and leads in minor films.

  3. Quartzite - Wikipedia

    en.wikipedia.org/wiki/Quartzite

    Quartzite is a very hard rock composed predominantly of an interlocking mosaic of quartz crystals. The grainy, sandpaper-like surface is glassy in appearance. Minor amounts of former cementing materials, iron oxide, silica, carbonate and clay, often migrate during recrystallization, causing streaks and lenses to form within the quartzite. [1 ...

  4. East Side Story (Squeeze album) - Wikipedia

    en.wikipedia.org/wiki/East_Side_Story_(Squeeze...

    East Side Story is the fourth studio album by new wave group Squeeze.The album peaked at number 19 in the UK Albums Chart, spending 26 weeks in the listing. [4]The album marked a shift from the new wave sound of their earlier work, as it contained songs influenced by rockabilly, R&B, blue-eyed soul, Merseybeat, and psychedelia among other genres.

  5. A partial lunar eclipse occurs when Earth moves between the sun and the full moon without being perfectly aligned. The celestial event appeared over Europe and much of Asia, Africa, North America ...

  6. Placer deposit - Wikipedia

    en.wikipedia.org/wiki/Placer_deposit

    Heavy minerals (black) forming placers along ripple marks. In geology, a placer deposit or placer is an accumulation of valuable minerals formed by gravity separation from a specific source rock during sedimentary processes. [1] The name is from the Spanish word placer, meaning " alluvial sand". Placer mining is an important source of gold, and ...

  7. Amethyst - Wikipedia

    en.wikipedia.org/wiki/Amethyst

    Amethyst is a purple variety of quartz (SiO. 2) and owes its violet color to irradiation, impurities of iron (Fe3+. ) and in some cases other transition metals, and the presence of other trace elements, which result in complex crystal lattice substitutions. [2][3][4] The irradiation causes the iron Fe3+.

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