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		<title>Whatever The Brand You Choose</title>
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		<summary type="html">&lt;p&gt;YolandaHupp3: ページの作成:「&amp;lt;br&amp;gt;Shears is a kind of scissors that can be used in a variety of different purposes. They even have medical and tactical uses and could be a perfect selection to feature…」&lt;/p&gt;
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At a time earlier than television, radio and even footage painted on canvas, stained glass home windows wer­e in all probability one of the dramatic, instructive and essential works of art most individuals had been uncovered to. Changes in taste and innovations in glassmaking hav­e made working with stained glass simpler than ever earlier than.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Because coloured glass is now cheaper and good designs and tutorials are simple to search out, the pastime is steadily gaining in popularity. With some follow, endurance and a few important tools, creating artwork with coloured glass is a hobby that is available to almost everybody. In the following part, we'll focus on the turbulent history of stained glass. Stained glass home windows in churches across Europe got larger, extra complex and extra majestic within the mid to late Middle Ages. Changes in political and religious beliefs had a profound impression on the development of stained glass, as well as on the survival of the stained glass artwork in churches across Europe. The­ Protestant Reformation in early 16th-century Europe, the rise of Oliver Cromwell in England  [http://39.108.174.133:1004/dustyuqx927276/wood-ranger-shears2005/wiki/Deco+Chef+16+Piece+Kitchen+Knife+Set+with+Wedge+Handles%252C+Shears%252C+Block%252C+And+Cutting+Board Wood Ranger Power Shears] and the French Revolution all introduced upheavals that resulted within the wanton destruction of religious art, including many irreplaceable stained glass home windows. After these episodes of unrest, glass artisans sought less controversial, more lucrative work with wealthy patrons, and ultimately began utilizing more nonreligious subjects, like nature or heraldic themes in privately commissioned tasks.&amp;lt;br&amp;gt;&lt;/div&gt;</summary>
		<author><name>YolandaHupp3</name></author>
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		<id>https://plamosoku.com/enjyo/index.php?title=Central_African_Shear_Zone&amp;diff=1828467</id>
		<title>Central African Shear Zone</title>
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		<updated>2025-10-20T13:43:36Z</updated>

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&lt;div&gt;&amp;lt;br&amp;gt;The Central African Shear Zone (CASZ) (or Shear System) is a wrench fault system extending in an ENE path from the Gulf of Guinea by Cameroon into Sudan. The structure is not properly understood. The shear zone dates to at the very least 640 Ma (million years ago). Motion occurred along the zone in the course of the break-up of Gondwanaland within the Jurassic and Cretaceous periods. A number of the faults within the zone were rejuvenated greater than once before and during the opening of the South Atlantic within the Cretaceous period. It has been proposed that the Pernambuco fault in Brazil is a continuation of the shear zone to the west. In Cameroon, the CASZ cuts across the Adamawa uplift, a post-Cretaeous formation. The Benue Trough lies to the north, and the Foumban Shear Zone to the south. Volcanic exercise has occurred alongside most of the size of the Cameroon line from 130 Ma to the current, and may be associated to re-activation of the CASZ.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The lithosphere beneath the CASZ in this space is thinned in a comparatively slim belt, with the asthenosphere upwelling from a depth of about 190 km to about 120 km. The Mesozoic and Tertiary movements have produced elongated rift basins in central Cameroon, northern Central African Republic and southern Chad. The CASZ was formerly thought to extend eastward solely to the Darfur region of western Sudan. It is now interpreted to extend into central and eastern Sudan, with a complete length of 4,000 km. Within the Sudan, the shear zone could have acted as a structural barrier to improvement of deep Cretaceous-Tertiary sedimentary basins in the north of the realm. Objections to this theory are that the Bahr el Arab and Blue Nile rifts lengthen northwest past one proposed line for the shear zone. However, the alignment of the northwestern ends of the rifts on this areas helps the speculation. Ibrahim, Ebinger &amp;amp; Fairhead 1996, pp.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Dorbath et al. 1986, pp. Schlüter &amp;amp; Trauth 2008, pp. Foulger &amp;amp; Jurdy 2007, pp. Plomerova et al. 1993, pp. Bowen &amp;amp; Jux 1987, pp. Bowen, Robert; Jux, Ulrich (1987). Afro-Arabian geology: a kinematic view. Dorbath, C.; Dorbath, L.; Fairhead, J. D.; Stuart, G. W. (1986). &amp;quot;A teleseismic delay time study throughout the Central African Shear Zone within the Adamawa region of Cameroon, West Africa&amp;quot;. Foulger, Gillian R.; Jurdy, Donna M. (2007). Plates, plumes, and planetary processes. Geological Society of America. Ibrahim, A. E.; Ebinger, C. J.; Fairhead, J. D. (20 April 1996). &amp;quot;Lithospheric extension northwest of the Central African Shear Zone in Sudan from potential subject research&amp;quot;. Pankhurst, Robert J. (2008). West Gondwana: pre-Cenozoic correlations across the South Atlantic Region. Plomerova, J; Babuska, V; Dorbath, C.; Dorbath, L.; Lillie, R. J. (1993). &amp;quot;Deep lithospheric structure throughout the Central African Shear Zone in Cameroon&amp;quot;. Geophysical Journal International. One hundred fifteen (2): 381-390. Bibcode:1993GeoJI.115..381P. Selley, Richard C. (1997). African basins. Schlüter, Thomas; Trauth, Martin H. (2008). Geological atlas of Africa: with notes on stratigraphy, tectonics, financial geology, geohazards, geosites and geoscientific education of every country. シュプリンガー・ジャパン株式会社.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Viscosity is a measure of a fluid's rate-dependent resistance to a change in form or to motion of its neighboring parts relative to each other. 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		<author><name>YolandaHupp3</name></author>
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		<title>利用者:YolandaHupp3</title>
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		<updated>2025-10-20T13:42:33Z</updated>

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