Does A Sump Pump Pit Need To Be Vented, Are Cake Delta 8 Carts Safe, Articles T

WebA tombolo is formed when a spit connects the mainland coast to an island. The relationship between wave steepness and beach angle is a two way affair. An example of this is Chesil Beach on the south coast of England. /*background-color: #9ac7ee;*/ A tombolo is a sediment deposit at the coast formed by wave refraction and diffraction at the edges of an obstacle (natural or artificial) originally detached from the mainland. Catalan: tmbol; English: tombolo; Etymology 2 . Tigertail And Mary Yelp, versa. This island-like landform is actually attached to the coast by a thin sand bar or spit. Example:Frank Island near Tofino, British Columbia, is a good example of a tombolo. line-height: 29px; Longshore drift occurs as waves push sediment (which may consist of sand, silt, and clay) towards the coastline at an angle. Webtombolo Bedeutung, Definition tombolo: 1. a narrow area of sand or shingle (= small stones) that joins an island to the coast: 2. a. Webtombolo [ tm b-l ] A sand or gravel bar that connects an island to the mainland or to another island. .epyt-gallery-thumb { Shingle/pebbles allow rapid infiltration and percolation, so the impact of swash and backwash are reduced. Company Reg no: 04489574. This shows grade level based on the word's complexity. The formation of a tombolo is caused by the diffraction of the wave at the ends of an obstacle, creating a convergence of opposing flows of sediment transport. The islands are generally 200-400 m wide, but some are wider. Our editors will review what youve submitted and determine whether to revise the article. VAT reg no 816865400. If a ridge of material links an island with the mainland, this ridge is called a tombolo. A tombolo is a sand spit or sand bar that connects an island to the mainland, creating an ismas The tombolo is made of sand. The result is waves break on to the beach obliquely at an angle of around 45 degrees. text-align: center; } padding: 0 20px; The distinction between the two is clear (now). } Why does wave refraction occur at a shoreline? They form as a simple drainage route for tides. margin-top: 0; color: #000000; } Sediment budget is the amount of sediment available within a cell. The shallower waters that occur between an island and the mainland are the loci of such features because sandbars form there. color: #000000; This can include sand, sediment, and shingle, resulting in landforms of coastal deposition. Definition:A narrow piece of land made of sediment such as sand or gravel that connects an island to the mainland or another island. A beach is a narrow, gently sloping strip of land that lies along the edge of an ocean, lake, or river. window.lsow_fs = {can_use_premium_code: false}; The final phase of this process is the complete coalescence between these sediment features and the blockage of the water body located behind the obstacle, with the consequent formation of a connection between the obstacle and the mainland (i.e., the tombolo). /* Offshore bar and barrier islands: characteristic of shores with a large influx of sediment, often from major rivers and currents which deposit and build accumulations of material into long, low mounds of sediment parallel to the coast. a sand bar connecting an island to the mainland or to another island. Tombolo, one or more sandbars or spits that connect an island to the mainland. margin-top: 40px; Backwash is likely to be greater than on a gravel beach. /* ]]> */ img.wp-smiley, Beaches: result from the dominance of constructive waves over destructive waves leading to a net gain of beach material over time creating a store of sediment. How does hydraulic action result in erosion by waves in a coastal environment? Saltation -Stones and pebbles bounce along the channel and hit each other. By far the worlds longest series is that of roughly 300 islands along the East and Southern coasts of the USA. [CDATA[ */ Are your language skills up to the task of telling the difference? Thus the same beach may produce two very different profiles at different times of the year. In turn, a low gradient produces shallow water which in turn increases wave steepness. font-size: 16px; !function(e,a,t){var n,r,o,i=a.createElement("canvas"),p=i.getContext&&i.getContext("2d");function s(e,t){var a=String.fromCharCode;p.clearRect(0,0,i.width,i.height),p.fillText(a.apply(this,e),0,0);e=i.toDataURL();return p.clearRect(0,0,i.width,i.height),p.fillText(a.apply(this,t),0,0),e===i.toDataURL()}function c(e){var t=a.createElement("script");t.src=e,t.defer=t.type="text/javascript",a.getElementsByTagName("head")[0].appendChild(t)}for(o=Array("flag","emoji"),t.supports={everything:!0,everythingExceptFlag:!0},r=0;r */ WebA tombolo is a narrow ridge of sand or shingle connecting an island to the mainland. } (geography) tombolo 2015 November 4, Diez hbitats costeros nicos en Espaa, in El Pas[1]: De entre los accidentes geogrficos, el tmbolo destaca por su esbeltez: una lengua de arena o istmo que solo en bajamar si le rodea el Atlntico- permite llegar a una franja de tierra. [C20: from Italian, from Latin tumulus /* */ The seaward edge of the berm is often scalloped and irregular due to the creation of beach cusps. It appears to be a small island that has not fully separated from the mainland. -los. 1973-2017 Fondation Flix Houphouet-Boigny pour la Recherche de la Paix. These types of lagoons are likely to fill with sediment over time. a sand bar connecting an island to the mainland or to another island. Tombolo definition is - a sand or gravel bar connecting an island with the mainland or another island. The Royal Canadian Geographical Society acknowledges that its offices are located on the unceded territory of the Algonquin Peoples, who have been guardians of, and in relationship with, these lands since time immemorial. line-height: 29px; .entry-content a{ } width: 33.333%; A single tombolo may connect a tied island to the mainland, as at Marblehead, Mass. color: #f5853b; Gyms In Chatham, #colophon #theme-attribution, #colophon #site-info { display: inline !important; There are often a series of smaller ridges formed beneath the storm ridge known as berms. color: #8f8f8f; Test your knowledge - and maybe learn something along the way. Delivered to your inbox! Need an example of a salt marsh? .entry-content table { Ridges are areas of the foreshore that are raised above the adjacent shore which dips into a Runnel. If the swash is stronger than the backwash then deposition may occur. } What Does Stella Mean In Hebrew, .archive #page-title { The coarse material is found deposited in the backshore and foreshore zones as littoral deposits. American Heritage Dictionary of the English Language, Fifth Edition. This transports the material out to sea. font-weight: bolder; Influence on the Natural Greenhouse Effect. These formation can be either solitary or found in clusters. Two ways they can form are: On drift aligned font-size: 20px; Spits are eroded by the sea and wind but a constant supply of sediment from longshore drift ensures their continued existence. You are using an outdated browser. .contenu { In the UK, we have two high and low tides a day. .layout-full #colophon { If Dogecoin Hit 1 How Much Will I Get Calculator, It appears to be a small island that has not fully separated from the mainland. padding: 10px 20px; Let's find out! This island-like landform is actually attached to the coast by a thin sand bar or spit. width: 1em !important; Tombolo definition: a narrow sand or shingle bar linking a small island with another island or the mainland | Meaning, pronunciation, translations and examples Brush up on your geography and finally learn what countries are in Eastern Europe with our maps. Tomobolos are linear ridges (or bar) of sand and shingle connecting an offshore island to the coastline of the mainland. text-align: center; All content on this website, including dictionary, thesaurus, literature, geography, and other reference data is for informational purposes only. https://doi.org/10.1007/978-94-017-8801-4_349, DOI: https://doi.org/10.1007/978-94-017-8801-4_349, eBook Packages: Earth and Environmental ScienceReference Module Physical and Materials Science. The largest particles, the products of cliff recession, are found at the rear of a beach. See all questions in Wave Erosion and Deposition. They develop where there is a sudden change in the shape of the coastline such as at a headland. A smaller sediment protrusion can also be developed in the back side of the obstacle. margin: 1em 0; } padding: 0 !important; Accessed 4 Mar. margin-bottom: 15px; https://www.worldatlas.com/articles/coastal-landforms-what-is-a-tombolo.html These may be temporary and altered during high energy conditions, but re-formed once conditions calm and a state of dynamic equilibrium is restored. font-weight: bold; })(); Sediment moves along the coast in sediment cells. A bar is a ridge of material that is connected at both ends to the mainland. A bar is a spit that joins together two headlands. Rutgers University, New Brunswick, New Jersey, USA, 2016 Springer Science+Business Media Dordrecht, de Mahiques, M.M. }. WebThe tombolo of Chesil Beach connects the Isle of Portland, a limestone island in the English channel to Abbotsbury, though it continues westwards to West Bay near Bridport. Nous utilisons des cookies pour vous garantir la meilleure exprience sur notre site web. Michel Michaelovitch de Mahiques . A tombolo, from the Italian tombolocode: ita promoted to code: it , meaning 'pillow' or 'cushion', and sometimes translated incorrectly as ayre (an ayre is a shingle beach of any kind), is a deposition landform by which an island becomes attached to the mainland by a narrow piece of land such as a spit or bar. Blog. You can support Canadian Geographic in3 ways: David Boyd, a Canadian environmental lawyer and UN Special Rapporteur on Human Rights and the Environment, reveals how recognizing the human right to a healthy environment can spur positive action for the planet, The story of how a critically endangered Indigenous language can be saved, As cities and towns continue to expand into our wild landscapes, conservation gardens can provide refuge for Canadas plummeting biodiversity. border-collapse: collapse; As the result longshore drift transports material from the beach to the south of the groyne and is not replenished (as the groyne blocks it). Tombolos are a type of isthmus. These act as systems which inputs (sources), processes (transfers or flows) and outputs (sinks). Tombolos. Looking for tombolos? 2002-2023 Tutor2u Limited. } 'pa pdd chac-sb tc-bd bw hbr-20 hbss lpt-25' : 'hdn'">, Test your vocabulary with our fun image quizzes, Clear explanations of natural written and spoken English. } border-bottom: 10px solid #33ac08; A long, narrow accumulation of sand or shingle, with one end attached to the land, and the other projecting at a narrow angle either into the sea or across a river estuary. Materials such as sand, pebbles, rocks, and seashell fragments cover beaches. #footer-widgets .widget { width: 25%; } A true tombolo is formed by wave diffraction and refraction. Bars are particularly obvious at low tide when they become exposed. #masthead .hgroup .logo { geography specialized us / tm.b.lo / uk / tm.b.l / plural tombolos a narrow area of sand or shingle (= small stones) that joins an island to the coast: Azorella Peninsula is linked by a (The built-up sandbar "ties" the island to the mainland.) a ridge of sand and a ridge of sand and a ridge of sand and shingle projecting shingle joining the shingle which has from the mainland mainland to an joined two into the sea island headlands, cutting off a bayHow does it form? WebTombolos Tomobolos are linear ridges (or bar) of sand and shingle connecting an offshore island to the coastline of the mainland. As the water moves more slowly around the island, it picks up sediment along the way. A single tombolo may connect a tied island to the mainland, as at Marblehead, Mass. var sibErrMsg = {"invalidMail":"Please fill out valid email address","requiredField":"Please fill out required fields","invalidDateFormat":"Please fill out valid date format","invalidSMSFormat":"Please fill out valid phone number"}; border: none !important; When the waves meet on the other side of the island (the side facing the coast), the sediment is deposited. Cuspate forelands consist of shingle ridges deposited in a triangular shape, and are the result of two separate spits joining, or the combined effects of two distinct sets of regular storm waves. Send us feedback. /*Archives*/ PubMedGoogle Scholar. .tablepress .column-1 { Instead of landing on the beach, this sediment begins to build up between the beach and an island, creating the bar mentioned above and effectively tying the island to the mainland. Swash and backwash movements move material up and down the beach producing many coastal features. A sandbar that connects an island to the mainland or to another vertical-align: -0.1em !important; The island and the beach belong to the Jurassic Coast, a UNESCO World Heritage Site, which is protected due to its unique geological formation. Some scientists, however, have suggested that Chesil Beach is not actually a true tombolo. background-color: #f5853b; As storm waves are more frequent in winter and swell waves more important in summer, many beaches differ in their winter and summer profile. Does Walgreens Sell Lane Bryant Gift Cards, } } British English and American English are only different when it comes to slang words. font-size: 20px; LS23 6AD background-color: #f5853b; An example of this is Chesil Beach which joins the Isle of Portland to the south of mainland Britain. river estuaries of sea-bed stores. Large, rounded material on the upper beach is probably supplied only during the highest spring times and is unaffected by average conditions. William Collins Sons & Co. Ltd. 1979, 1986 HarperCollins What is wave pounding and how does it result in erosion? The tombolo is made of sand. 'Hiemal,' 'brumation,' & other rare wintry words. As a result, material is transported along the beach via longshore drift. Spit: the deposition of material transported along a coast by longshore drift (littoral movement) at a break in coast orientation and where the dominant current slows and weakens to produce an extended finger of depositional material, often with a recurved end. While every effort has been made to follow citation style rules, there may be some discrepancies. If you live for 2.4 billion seconds how old will you be? Two or more can form a lagoon. On another visit to the island, Cushman and I had anchored in Presque Isle Bay, and trekked on a, Poipu Beach, Kauai, Hawaii Located on the sunny southern shore of Kauai, Poipu Beach is actually made up of two spectacular beaches separated by a narrow sand spit called a, After its shadowy start in a deep pine forest, the canopy opens overhead as the trail winds past a large swamp and across swaths of huge rocks to the, The trail crosses swaths of huge rocks to a, Post the Definition of tombolo to Facebook, Share the Definition of tombolo on Twitter. Steep destructive waves reduce beach angle whereas gentle constructive waves increase it. When the shape of the coastline changes substantially however, longshore drift continues to transport material in the same direction rather than following the coastline. UNESCO Chair A sandbar that connects an island to the mainland or to another island. text-align: right; To save this word, you'll need to log in. Drift aligned coasts: beaches are produced where waves break at an angle to the coast. Please refer to the appropriate style manual or other sources if you have any questions. WebFor Higher Geography study the formation of erosion and depositional features in coastal landscapes and identify features on an OS map. A tombolo is a spit connecting an island to the mainland. font-size: 16px; var cnArgs = {"ajaxUrl":"https:\/\/www.fondation-fhb.org\/wp-admin\/admin-ajax.php","nonce":"914110b2e1","hideEffect":"fade","position":"bottom","onScroll":"0","onScrollOffset":"100","onClick":"0","cookieName":"cookie_notice_accepted","cookieTime":"2592000","cookieTimeRejected":"2592000","cookiePath":"\/","cookieDomain":"","redirection":"0","cache":"0","refuse":"0","revokeCookies":"0","revokeCookiesOpt":"automatic","secure":"1"}; var mobileNav = {"search":{"url":"https:\/\/www.fondation-fhb.org\/en\/home","placeholder":"Search"},"text":{"navigate":"Menu","back":"Back","close":"Close"},"nextIconUrl":"https:\/\/www.fondation-fhb.org\/wp-content\/themes\/vantage\/inc\/mobilenav\/images\/next.png","mobileMenuClose":"<\/i>"}; Part of Springer Nature. Vegan Certification Usa, It was destroyed several thousand years ago by a slight change in mean sea level, and only a chain of sandbanks that seriously hinder navigation exists there today. https://www.youtube.com/watch?v=U9EhVa4MmEs. Sand Lance also occur in deep water (>30 m) on sand wave fields in the San Juan Channel (Blaine 2006; Gary Greene, La presente biografia, que supone un notable enriquecimiento respecto a esa anterior, esta estructurada en siete capitulos, el primero dedicado a los estudios y formacion del joven sacerdote y los seis siguientes a las seis etapas que forman la <> de Giuseppe Sarto: vicario parroquial en, The name is derived from Partridge Island, a headland near Parrsboro, Cumberland County, Nova Scotia, connected to the mainland by a, Dictionary, Encyclopedia and Thesaurus - The Free Dictionary, the webmaster's page for free fun content, 12 paradise islands in Scotland you must visit, Starlings step up to the mark all for Rachel House cause, Low temperature brooding of Olympia oysters (Ostrea lurida) in northern Puget Sound, Abundance and spatial-temporal distribution of the shrimp Xiphopenaeus kroyeri (Decapoda: Penaeidae): an exploited species in southeast Brazil/Abundancia e distribuicao espaco-temporal do camarao Xiphopenaeus kroyeri (Decapoda: Penaeidae): uma especie em explotacao no sudeste do Brasil, Nearshore distribution of Pacific Sand Lance (Ammodytes personatus) in the inland waters of Washington State, Giampaolo Romanato, Pio x. Alle origini del cattolicesimo contemporaneo, Stratigraphic and temporal context and faunal diversity of Permian-Jurassic continental Tetrapod assemblages from the Fundy rift basin, eastern Canada. The backshore is a cliff or is marked by a line of sand dunes. overflow-x: hidden; {"@context":"https://schema.org","@graph":[{"@type":"Organization","@id":"https://www.fondation-fhb.org/#organization","name":"Fondation F\u00e9lix Houphou\u00ebt-Boigny pour la recherche de la paix","url":"https://www.fondation-fhb.org/","sameAs":["http://www.facebook.com/fondationfhb","http://fondationfhb","http://www.youtube.com/fondationfhb","https://twitter.com/fondationfhb"],"logo":{"@type":"ImageObject","@id":"https://www.fondation-fhb.org/#logo","inLanguage":"en-GB","url":"https://www.fondation-fhb.org/wp-content/uploads/2019/03/logo_ffhb.png","contentUrl":"https://www.fondation-fhb.org/wp-content/uploads/2019/03/logo_ffhb.png","width":108,"height":56,"caption":"Fondation F\u00e9lix Houphou\u00ebt-Boigny pour la recherche de la paix"},"image":{"@id":"https://www.fondation-fhb.org/#logo"}},{"@type":"WebSite","@id":"https://www.fondation-fhb.org/#website","url":"https://www.fondation-fhb.org/","name":"F\u00e9lix Houphou\u00ebt-Boigny Foundation for Peace Research","description":"","publisher":{"@id":"https://www.fondation-fhb.org/#organization"},"potentialAction":[{"@type":"SearchAction","target":"https://www.fondation-fhb.org/?s={search_term_string}","query-input":"required name=search_term_string"}],"inLanguage":"en-GB"},{"@type":"WebPage","@id":"https://www.fondation-fhb.org/2021/05/21/ljvxentm/#webpage","url":"https://www.fondation-fhb.org/2021/05/21/ljvxentm/","name":"tombolo definition geography - F\u00e9lix Houphou\u00ebt-Boigny Foundation for Peace Research","isPartOf":{"@id":"https://www.fondation-fhb.org/#website"},"datePublished":"2021-05-21T04:48:28+00:00","dateModified":"2021-05-21T04:48:28+00:00","breadcrumb":{"@id":"https://www.fondation-fhb.org/2021/05/21/ljvxentm/#breadcrumb"},"inLanguage":"en-GB","potentialAction":[{"@type":"ReadAction","target":["https://www.fondation-fhb.org/2021/05/21/ljvxentm/"]}]},{"@type":"BreadcrumbList","@id":"https://www.fondation-fhb.org/2021/05/21/ljvxentm/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"item":{"@type":"WebPage","@id":"https://www.fondation-fhb.org/en/home/","url":"https://www.fondation-fhb.org/en/home/","name":"Home"}},{"@type":"ListItem","position":2,"item":{"@type":"WebPage","@id":"https://www.fondation-fhb.org/en/activities/","url":"https://www.fondation-fhb.org/en/activities/","name":"Activities"}},{"@type":"ListItem","position":3,"item":{"@type":"WebPage","@id":"https://www.fondation-fhb.org/2021/05/21/ljvxentm/","url":"https://www.fondation-fhb.org/2021/05/21/ljvxentm/","name":"tombolo definition geography"}}]},{"@type":"Article","@id":"https://www.fondation-fhb.org/2021/05/21/ljvxentm/#article","isPartOf":{"@id":"https://www.fondation-fhb.org/2021/05/21/ljvxentm/#webpage"},"author":{"@id":""},"headline":"tombolo definition geography","datePublished":"2021-05-21T04:48:28+00:00","dateModified":"2021-05-21T04:48:28+00:00","mainEntityOfPage":{"@id":"https://www.fondation-fhb.org/2021/05/21/ljvxentm/#webpage"},"commentCount":0,"publisher":{"@id":"https://www.fondation-fhb.org/#organization"},"articleSection":"Uncategorized","inLanguage":"en-GB","potentialAction":[{"@type":"CommentAction","name":"Comment","target":["https://www.fondation-fhb.org/2021/05/21/ljvxentm/#respond"]}]}]} Orbiting objects, which are called satellites, include planets, moons, asteroids, and manmade devices. Copyright 2011. Cusps are semi-circular depressions; they are smaller and more temporary features formed by a collection of waves reaching the same point. See the etymology of the Vegan Certification Usa, Adams Bridge, which connected Sri Lanka (Ceylon) with India across the 33-mile (53-kilometre) wide Palk Strait, was formerly the worlds largest tombolo. width: 1500px; Britannica.com: Encyclopedia article about tombolo. The fascinating story behind many people's favori Can you handle the (barometric) pressure? An orbit is a regular, repeating path that one object takes around another object or center of gravity. Tides changes in the water level caused by the gravitational pull of the moon (and the sun to a lesser extent). #footer-widgets aside { width : 25%; } @import url(//fonts.googleapis.com/css?family=Roboto:400&display=block); body,button,input,select,textarea { font-family: "Roboto"; font-weight: 400 } #masthead.site-header .hgroup h1 { font-family: "Roboto"; font-weight: 400 } #page-wrapper h1,#page-wrapper h2,#page-wrapper h3,#page-wrapper h4,#page-wrapper h5,#page-wrapper h6 { font-family: "Roboto"; font-weight: 400 } .main-navigation, .mobile-nav-frame, .mobile-nav-frame .title h3 { font-family: "Roboto"; font-weight: 400 } #masthead .hgroup h1, #masthead.masthead-logo-in-menu .logo > h1 { color: #000000 } #masthead .hgroup .support-text, #masthead .hgroup .site-description { font-size: 28px; color: #000000 } #page-title, article.post .entry-header h1.entry-title, article.page .entry-header h1.entry-title { font-size: 32px; color: #000000 } .entry-content { font-size: 16px } .entry-content, #comments .commentlist article .comment-meta a { color: #000000 } .entry-content h1, .entry-content h2, .entry-content h3, .entry-content h4, .entry-content h5, .entry-content h6, #comments .commentlist article .comment-author a, #comments .commentlist article .comment-author, #comments-title, #reply-title, #commentform label { color: #000000 } #comments-title, #reply-title { border-bottom-color: #000000 } .entry-content h1 { font-size: 32px } .entry-content h2 { font-size: 28px } .entry-content h3 { font-size: 24px } .entry-content h4 { font-size: 20px } .entry-content h5 { font-size: 18px } .entry-content h6 { font-size: 16px } #masthead .hgroup { padding-top: 25px; padding-bottom: 25px } .entry-content a, .entry-content a:visited, article.post .author-box .box-content .author-posts a:hover, #secondary a, #secondary a:visited, #masthead .hgroup a, #masthead .hgroup a:visited, .comment-form .logged-in-as a, .comment-form .logged-in-as a:visited { color: #f5853b } .entry-content a, .textwidget a { text-decoration: none } .entry-content a:hover, .entry-content a:focus, .entry-content a:active, #secondary a:hover, #masthead .hgroup a:hover, #masthead .hgroup a:focus, #masthead .hgroup a:active, .comment-form .logged-in-as a:hover, .comment-form .logged-in-as a:focus, .comment-form .logged-in-as a:active { color: #33ac08 } .main-navigation { background-color: #f5853b } .main-navigation a { color: #000000 } .main-navigation ul ul { background-color: #f5853b } .main-navigation ul ul a { color: #000000 } .main-navigation ul li:hover > a, .main-navigation ul li:focus > a, #search-icon #search-icon-icon:hover, #search-icon #search-icon-icon:focus { background-color: #ffffff } .main-navigation ul li:hover > a, .main-navigation ul li:focus > a, .main-navigation ul li:hover > a [class^="fa fa-"] { color: #f5853b } .main-navigation ul ul li:hover > a { background-color: #ffffff; color: #f5853b } .main-navigation [class^="fa fa-"], .main-navigation .mobile-nav-icon { color: #ffffff } #search-icon #search-icon-icon { background-color: #f5853b } #search-icon #search-icon-icon .vantage-icon-search { color: #ffffff } #search-icon #search-icon-icon:hover .vantage-icon-search, #search-icon #search-icon-icon:focus .vantage-icon-search { color: #f5853b } #search-icon .searchform { background-color: #ffffff } #search-icon .searchform input[name=s] { color: #000000 } .main-navigation ul li a { padding-top: 16px; padding-bottom: 16px } .main-navigation ul li a, #masthead.masthead-logo-in-menu .logo { padding-left: 15px; padding-right: 15px } .main-navigation ul li { font-size: 18px } a.button, button, html input[type="button"], input[type="reset"], input[type="submit"], .post-navigation a, #image-navigation a, article.post .more-link, article.page .more-link, .paging-navigation a, .woocommerce #page-wrapper .button, .woocommerce a.button, .woocommerce .checkout-button, .woocommerce input.button, #infinite-handle span { background: #f5853b; border-color: #f1d46f } a.button:hover, button:hover, html input[type="button"]:hover, input[type="reset"]:hover, input[type="submit"]:hover, .post-navigation a:hover, #image-navigation a:hover, article.post .more-link:hover, article.page .more-link:hover, .paging-navigation a:hover, .woocommerce #page-wrapper .button:hover, .woocommerce a.button:hover, .woocommerce .checkout-button:hover, .woocommerce input.button:hover, .woocommerce input.button:disabled:hover, .woocommerce input.button:disabled[disabled]:hover, #infinite-handle span:hover { background: #f5853b } a.button:hover, button:hover, html input[type="button"]:hover, input[type="reset"]:hover, input[type="submit"]:hover, .post-navigation a:hover, #image-navigation a:hover, article.post .more-link:hover, article.page .more-link:hover, .paging-navigation a:hover, .woocommerce #page-wrapper .button:hover, .woocommerce a.button:hover, .woocommerce .checkout-button:hover, .woocommerce input.button:hover, #infinite-handle span:hover { opacity: 0.75; border-color: #f1d46f } a.button:focus, button:focus, html input[type="button"]:focus, input[type="reset"]:focus, input[type="submit"]:focus, .post-navigation a:focus, #image-navigation a:focus, article.post .more-link:focus, article.page .more-link:focus, .paging-navigation a:focus, .woocommerce #page-wrapper .button:focus, .woocommerce a.button:focus, .woocommerce .checkout-button:focus, .woocommerce input.button:focus, .woocommerce input.button:disabled:focus, .woocommerce input.button:disabled[disabled]:focus, #infinite-handle span:focus { background: #f5853b } a.button:focus, button:focus, html input[type="button"]:focus, input[type="reset"]:focus, input[type="submit"]:focus, .post-navigation a:focus, #image-navigation a:focus, article.post .more-link:focus, article.page .more-link:focus, .paging-navigation a:focus, .woocommerce #page-wrapper .button:focus, .woocommerce a.button:focus, .woocommerce .checkout-button:focus, .woocommerce input.button:focus, #infinite-handle span:focus { opacity: 0.75; border-color: #f1d46f } a.button, button, html input[type="button"], input[type="reset"], input[type="submit"], .post-navigation a, #image-navigation a, article.post .more-link, article.page .more-link, .paging-navigation a, .woocommerce #page-wrapper .button, .woocommerce a.button, .woocommerce .checkout-button, .woocommerce input.button, .woocommerce #respond input#submit:hover, .woocommerce a.button:hover, .woocommerce button.button:hover, .woocommerce input.button:hover, .woocommerce input.button:disabled, .woocommerce input.button:disabled[disabled], .woocommerce input.button:disabled:hover, .woocommerce input.button:disabled[disabled]:hover, #infinite-handle span button { color: #ffffff } a.button, button, html input[type="button"], input[type="reset"], input[type="submit"], .post-navigation a, #image-navigation a, article.post .more-link, article.page .more-link, .paging-navigation a, .woocommerce #page-wrapper .button, .woocommerce a.button, .woocommerce .checkout-button, .woocommerce input.button, #infinite-handle span button { text-shadow: none } a.button, button, html input[type="button"], input[type="reset"], input[type="submit"], .post-navigation a, #image-navigation a, article.post .more-link, article.page .more-link, .paging-navigation a, .woocommerce #page-wrapper .button, .woocommerce a.button, .woocommerce .checkout-button, .woocommerce input.button, .woocommerce #respond input#submit.alt, .woocommerce a.button.alt, .woocommerce button.button.alt, .woocommerce input.button.alt, #infinite-handle span { -webkit-box-shadow: none; -moz-box-shadow: none; box-shadow: none } #footer-widgets .widget .widget-title { color: #ffffff } #footer-widgets .widget { color: #ffffff } #colophon .widget_nav_menu .menu-item a { border-color: #ffffff } #footer-widgets .widget a, #footer-widgets .widget a:visited { color: #ffffff } #footer-widgets .widget a:hover, #footer-widgets .widget a:focus, #footer-widgets .widget a:active { color: #ffffff } #colophon #theme-attribution, #colophon #site-info { color: #ffffff } #colophon #theme-attribution a, #colophon #site-info a { color: #ffffff }