Ireland’s highest Waterfall<\/b>, located in a beautiful Wicklow Valley at Powerscourt Estate.<\/p>\n
Waterfall<\/b> (Japanese: —<\/b> Waterfall Climb<\/i>) is a damage-dealing Water-type<\/a> move<\/a> introduced in Generation I<\/a>. It is HM07<\/a> in Generations II<\/a>, III<\/a>, and IV<\/a>; it is HM05<\/a> as of Generation V<\/a>. Prior to Generation II, it was the signature move<\/a> of Goldeen<\/a> and Seaking<\/a>. (Bulbapedia<\/a>)<\/p>\n Waterfall<\/b> enables brands, agencies and technology providers to directly engage subscribers across SMS, Passbook, QR Codes, mobile wallets, mobile coupons, MMS, IVR, etc<\/p>\n waterfall model – The waterfall model is a sequential design process, used in software development processes, in which progress is seen as flowing steadily downwards through the phases of conception, initiation, analysis, design, construction, testing, production\/implementation and maintenance.<\/p>\n Definition: “A waterfall<\/b> is a place where water flows over a vertical drop in the course of a stream<\/a> or river<\/a>. Waterfalls also occur where meltwater<\/a> drops over the edge of a tabular iceberg<\/a> or ice shelf<\/a>.<\/p>\n Waterfalls are commonly formed in the upper course of the river.[1]<\/a><\/sup> At these times the channel is often narrow and deep. When the river courses over resistant bedrock<\/a>, erosion happens slowly, while downstream the erosion occurs more rapidly.[1]<\/a><\/sup>[2]<\/a><\/sup> As the watercourse increases its velocity at the edge of the waterfall, it plucks material from the riverbed. Whirlpools<\/a> created in the turbulence as well as sand and stones carried by the watercourse increase the erosion capacity.[1]<\/a><\/sup> This causes the waterfall to carve deeper into the bed and to recede upstream. Often over time, the waterfall will recede back to form a canyon or gorge downstream as it recedes upstream, and it will carve deeper into the ridge above it.[3]<\/a><\/sup> The rate of retreat for a waterfall can be as high as one and half meters per year.[1]<\/a><\/sup><\/p>\n Often, the rock stratum<\/a> just below the more resistant shelf will be of a softer type, meaning that undercutting due to splashback will occur here to form a shallow cave-like formation known as a rock shelter<\/a> under and behind the waterfall. Eventually, the outcropping<\/a>, more resistant cap rock will collapse under pressure to add blocks of rock to the base of the waterfall. These blocks of rock are then broken down into smaller boulders by attrition<\/a> as they collide with each other, and they also erode the base of the waterfall by abrasion<\/a>, creating a deep plunge pool or gorge.<\/p>\n Streams become wider and shallower just above waterfalls due to flowing over the rock shelf, and there is usually a deep area just below the waterfall because of the kinetic energy<\/a> of the water hitting the bottom. Waterfalls normally form in a rocky area due to erosion. After a long period of being fully formed, the water falling off the ledge will retreat, causing a horizontal pit parallel to the waterfall wall. Eventually, as the pit grows deeper, the waterfall collapses to be replaced by a steeply sloping stretch of river bed.[1]<\/a><\/sup> In addition to gradual processes such as erosion, earth movement caused by earthquakes<\/a> or landslides<\/a> or volcanoes<\/a> can cause a differential in land heights which interfere with the natural course of a water flow, and result in waterfalls.<\/p>\n A river sometimes flows over a large step in the rocks that may have been formed by a fault line<\/a>. Waterfalls can occur along the edge of a glacial trough<\/a>, where a stream or river flowing into a glacier<\/a> continues to flow into a valley after the glacier has receded or melted. The large waterfalls in Yosemite Valley<\/a> are examples of this phenomenon, which is referred to as a hanging valley<\/a>. Another reason hanging valleys may form is where two rivers join and one is flowing faster than the other.[1]<\/a><\/sup> Waterfalls can be grouped into ten broad classes based on the average volume of water present on the fall (which depends on both the waterfall’s average flow and its height) using a logarithmic scale<\/a>. Class 10 waterfalls include Niagara Falls<\/a>, Paulo Afonso Falls<\/a> and Khone Falls<\/a>.<\/p>\n Classes of other well-known waterfalls include Victoria Falls<\/a> and Kaieteur Falls<\/a> (Class 9); Rhine Falls<\/a> and Gullfoss<\/a> (Class 8); Angel Falls<\/a> and Dettifoss<\/a> (Class 7); Yosemite Falls<\/a>, Lower Yellowstone Falls<\/a> and Umphang Thee Lor Sue Waterfall<\/a> (Class 6); Sutherland Falls<\/a> (Class 5).[4]<\/a><\/sup>” (Wikipedia<\/a>)<\/p>\n A free screensaver is definitely cheaper than a round-trip ticket to an exotic locale. This Waterfall<\/b> Screensaver displays a realistic picture of a waterfall.<\/b><\/p>\n indoor waterfalls<\/p>\n waterfall kits<\/p>\n Post the direct URL (link) where your drawing, doodle, artwork is posted (e.g. your blog, Flickr) in the comments area of this post. I would really like to keep all the artwork together and provide a way for others to see your work and get familiar with your blog or website.<\/p>\n The Creative Prompt Project, also, has a Flickr group<\/a>, which you can join to\u00a0 post your responses. I created this spot so those of you without blogs and websites would have a place to post your responses.<\/p>\n We are also talking about this on Twitter and Instagram. Use the hashtag #CPP<\/p>\n Waterfall<\/b> or waterfalls<\/b> may also refer to:<\/p>\n Ireland’s highest Waterfall, located in a beautiful Wicklow Valley at Powerscourt Estate. Waterfall (Japanese: — Waterfall Climb) is a damage-dealing Water-type move introduced in Generation I. It is HM07 in Generations II, III, and IV; it is HM05 as of Generation V. Prior to Generation II, it was the signature move of Goldeen and Seaking. … Continue reading “Creative Prompt #362: Waterfall”<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"ngg_post_thumbnail":0,"_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_feature_clip_id":0,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_post_was_ever_published":false},"categories":[374],"tags":[79,311,72],"class_list":["post-31551","post","type-post","status-publish","format-standard","hentry","category-374","tag-creative-prompt","tag-creativity","tag-group-project"],"jetpack_featured_media_url":"","jetpack_likes_enabled":true,"jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/artquiltmaker.com\/blog\/wp-json\/wp\/v2\/posts\/31551","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/artquiltmaker.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/artquiltmaker.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/artquiltmaker.com\/blog\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/artquiltmaker.com\/blog\/wp-json\/wp\/v2\/comments?post=31551"}],"version-history":[{"count":0,"href":"https:\/\/artquiltmaker.com\/blog\/wp-json\/wp\/v2\/posts\/31551\/revisions"}],"wp:attachment":[{"href":"https:\/\/artquiltmaker.com\/blog\/wp-json\/wp\/v2\/media?parent=31551"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/artquiltmaker.com\/blog\/wp-json\/wp\/v2\/categories?post=31551"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/artquiltmaker.com\/blog\/wp-json\/wp\/v2\/tags?post=31551"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}Places<\/span><\/h2>\n
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Alcohol and drugs<\/span><\/h2>\n
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Art and architecture<\/span><\/h2>\n
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Information displays<\/span><\/h2>\n
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Music<\/span><\/h2>\n
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Railway stations<\/span><\/h2>\n
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Other uses<\/span><\/h2>\n
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See also<\/span><\/h2>\n
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