"A sabkha (Arabic: \u0633\u0628\u062E\u0629) is a coastal, supratidal mudflat or sandflat in which evaporite-saline minerals accumulate as the result of semiarid to arid climate. Sabkhas are gradational between land and intertidal zone within restricted coastal plains just above normal high-tide level. Within a sabkha, evaporite-saline minerals sediments typically accumulate below the surface of mudflats or sandflats. Evaporite-saline minerals, tidal-flood, and aeolian deposits characterize many sabkhas found along modern coastlines. The accepted type locality for a sabkha is at the southern coast of the Persian Gulf, in the United Arab Emirates. Sabkha is a phonetic transliteration of the Arabic word used to describe any form of salt flat. A sabkha is also known as a sabkhah, sebkha, or coastal sabkha. The term sabkha has also been used as a general term for any flat area, coastal or interior, where, as the result of evaporation, salt and other evaporite minerals precipitate near or at the surface. The term continental sabkha is used for such environments found within deserts. Because of the confusion created by using sabkha for salt flats and playas, it has been proposed that the usage of this term be abandoned for playas and other intracontinental basins and flats."@en . . "Una sebkha (en \u00E1rabe, \u0633\u0628\u062E\u0629\u200E, sab\u1E96a, una palabra usada para designar los salares) \u2014tambi\u00E9n transcrita como sabkha, sebkhat o sebkhet\u2014, es un t\u00E9rmino usado en geolog\u00EDa y geomorfolog\u00EDa para designar en regiones \u00E1ridas un dep\u00F3sito sedimentario, parecido a una dura costra superficial, que ocupa la parte inferior de una depresi\u00F3n de alta salinidad y que est\u00E1 m\u00E1s o menos separada de un medio marino. Las sebkhas son form\u00E1ndose a lo largo de costas \u00E1ridas y siempre se caracterizan por la existencia de dep\u00F3sitos de carbonatos-evaporitas con algunos . Algunas calizas org\u00E1nicas se forman de fragmentos de conchas (ricas en calcita) y otros por verdaderos cementerios de restos de moluscos (como son las coquinas) y de invertebrados como radiolarios y foramin\u00EDferos.\u200B Las sebkhas forman secuencias suba\u00E9reas, progradantes y bancos de arena elevados\u200B que tienen un espesor medio de un metro o menos. El t\u00E9rmino sebkha tambi\u00E9n designa ciertos lagos someros salinos, que generalmente se secan estacionalmente. La depresi\u00F3n tambi\u00E9n puede estar en contacto con el medio marino, ya sea por una corriente muy peque\u00F1a de agua (piscinas de aguas profundas), o por infiltraciones (piscinas de poca profundidad). En este \u00FAltimo caso, puede haber desbordamientos peri\u00F3dicos de agua de mar hacia la cuenca. En ambos casos habr\u00E1 un aumento de la salinidad, una evaporaci\u00F3n importante, aparici\u00F3n de salmuera y precipitaci\u00F3n de evaporitas en el fondo de la cuenca, si la profundidad es baja, o en un extremo, si la profundidad es importante. Hay sebkhas principalmente en las costas del norte de \u00C1frica \u2014, , , , , , , , y \u2014, en Oriente Medio \u2014t\u00EDpicas las de la costa de los Emiratos \u00C1rabes Unidos\u2014, en la Baja California y en Shark Bay, en Australia."@es . . . . . . . . . . . . . . . . . "Sabkha o sebkha (de l'\u00E0rab \u0633\u0628\u062E\u0629, sab\u1E96a) \u00E9s el nom en \u00E0rab de les llacunes salades. S\u00F3n molt abundants a Tun\u00EDsia, especialment a la zona central costera del Sahel tunisi\u00E0, i Alg\u00E8ria, per\u00F2 tamb\u00E9 en altres llocs. Les m\u00E9s grans o importants s\u00F3n la sabkha de Sidi El Hani, la sabkha de Monastir, la sabkha d'El Djem, la sabkha d'El Ghorra, la sabkha d'En Noual, la sabkha de Boujemal, la sabkha de Tadder i la sabkha d'El Makta. A la vora de la ciutat de Tunis, hi ha la sabkha de Sejoumi, al sud-oest, i la sabkha d'Ariana, al nord-est. Aquestes llacunes, normalment humides, produeixen sal en assecar-se a l'estiu o mitjan\u00E7ant la intervenci\u00F3 humana."@ca . . "Sebkha"@pt . . . . . . . . . "Sabkha"@en . . "Eine oder ein Sabcha (auch Sebcha; arabisch \u0633\u0628\u062E\u0629, DMG Sab\u1E2Ba; englisch Sabkha, Sebkha, auch Sebkhat, Sebkhet, in der westlichen Sahara Grara genannt) ist ein flaches, zeitweise mit Wasser gef\u00FClltes Becken ohne Oberfl\u00E4chenabfluss in einem semiariden Gebiet."@de . "\u0421\u0435\u0431\u0445\u0430, \u0441\u0435\u0431\u043A\u0440\u0430 (\u0430\u0440\u0430\u0431. \u0633\u0628\u062E\u0629\u200E) \u2014 \u0437\u0430\u043C\u043A\u043D\u0443\u0442\u0430 \u0431\u0435\u0437\u0441\u0442\u0456\u0447\u043D\u0430, \u0430\u0431\u043E \u043F\u0440\u0438\u0431\u0435\u0440\u0435\u0436\u043D\u043E-\u043C\u043E\u0440\u0441\u044C\u043A\u0430 \u043D\u0438\u0437\u043E\u0432\u0438\u043D\u0430 \u0437 \u043F\u043B\u0430\u0441\u043A\u0438\u043C \u0434\u043D\u043E\u043C, \u044F\u043A\u0435 \u0432\u043A\u0440\u0438\u0442\u0435 \u0441\u043E\u043B\u043E\u043D\u0447\u0430\u043A\u0430\u043C\u0438. \u041F\u0456\u0434\u0432\u0438\u0449\u0435\u043D\u0430 \u043E\u043A\u043E\u043B\u0438\u0446\u044F \u0441\u0435\u0431\u0445\u0438 \u043D\u0430\u0437\u0438\u0432\u0430\u0454\u0442\u044C\u0441\u044F \u0448\u043E\u0442\u0442\u043E\u043C."@uk . . . . . . . . "6381951"^^ . . . . "\u0627\u0644\u0633\u064E\u0651\u0628\u064E\u062E\u064E\u0629\u064F \u0623\u0648 \u0627\u0644\u0633\u064E\u0651\u0628\u0652\u062E\u064E\u0629\u064F \u0647\u064A \u0623\u0631\u0636 \u0645\u0633\u062A\u0648\u064A\u0629\u060C \u0639\u0627\u062F\u0629 \u0645\u0627 \u062A\u0642\u0639 \u0628\u064A\u0646 \u0635\u062D\u0631\u0627\u0621 \u0648\u0645\u062D\u064A\u0637 \u0623\u0648 \u0643\u0627\u0646\u062A \u0641\u064A\u0645\u0627 \u0633\u0628\u0642 \u0628\u062D\u064A\u0631\u0629 \u0623\u0648 \u0628\u062D\u064A\u0631\u0629 \u0645\u0644\u062D\u064A\u0629\u060C \u0648\u064A\u062A\u0645\u064A\u0632 \u0633\u0637\u062D\u0647\u0627 \u0628\u0648\u062C\u0648\u062F \u062A\u0631\u0633\u0628\u0627\u062A \u0645\u0644\u062D\u064A\u0651\u0629 \u0648\u062C\u0628\u0633\u064A\u0651\u0629 \u0648\u062A\u0631\u0633\u0628\u0627\u062A \u0643\u0631\u0628\u0648\u0646\u0627\u062A \u0627\u0644\u0643\u0627\u0644\u0633\u064A\u0648\u0645 \u0648\u0643\u0630\u0644\u0643 \u0631\u0648\u0627\u0633\u0628 \u062C\u0644\u0628\u062A\u0647\u0627 \u0627\u0644\u0631\u064A\u0627\u062D \u0648\u0627\u0644\u0645\u062F \u0627\u0644\u0645\u0627\u0626\u064A\u0651\u060C \u0648\u0642\u062F \u062A\u062D\u0648\u064A \u0639\u0644\u0649 \u0627\u0644\u0645\u0627\u0621 \u0637\u0628\u0642\u0627\u064B \u0644\u0637\u0648\u0631 \u062A\u0643\u0648\u0651\u0646\u0647\u0627."@ar . . . . . . "Uma sebkha, sabkha, sabcha, sebkhat ou sebkhet \u00E9 um termo \u00E1rabe que significa terreno salgado, laguna salgada ou deserto de sal, que \u00E9 usado em geologia para designar, em regi\u00F5es \u00E1ridas, dep\u00F3sitos sedimentares, semelhantes a duras crostas superficiais que ocupam a parte inferior de uma depress\u00E3o de alta salinidade e que est\u00E1 mais ou menos separada de um meio marinho. No entanto, o contacto com o meio marinho pode ser permanente, por meio de uma corrente muito fraca (lagoas de \u00E1guas profundas), ou, pelo contr\u00E1rio, por infiltra\u00E7\u00F5es (lagoas pouco profundas). Neste \u00FAltimo caso, pode haver derrames peri\u00F3dicos da \u00E1gua salgada para a bacia hidrogr\u00E1fica. Em ambos os casos, h\u00E1 um aumento da salinidade, uma evapora\u00E7\u00E3o importante, a apari\u00E7\u00E3o de salmoura e a precipita\u00E7\u00E3o de evaporitos (dep\u00F3sitos salinos) no fundo da bacia, se a profundidade \u00E9 baixa, ou num dos extremos se a profundidade \u00E9 grande. As sebkhas situam-se em \"zonas sobrelitorais\", ou seja, imediatamente acima do n\u00EDvel das mar\u00E9s altas e formam-se em costas \u00E1ridas. Encontram-se sebkhas principalmente nas costas do Norte de \u00C1frica, no M\u00E9dio Oriente, na Baixa Calif\u00F3rnia e na Ba\u00EDa Shark, na Austr\u00E1lia."@pt . . "\u30B5\u30D6\u30AB\uFF08\u963F: \u0633\u0628\u062E\u0629\u200E\u3001sabkha\u3001sebkhat\uFF09\u3042\u308B\u3044\u306F\u30B5\u30D6\u30CF\u306F\u3001\u5869\u539F\u306E\u30A2\u30E9\u30D3\u30A2\u8A9E\u3067\u3001\u7802\u6F20\u6C17\u5019\u306E\u6D77\u5CB8\u306E\u6F6E\u4E0A\u5E2F\u306B\u3067\u304D\u308B\u84B8\u767A\u5CA9\u3068\u70AD\u9178\u5869\u5CA9\u3067\u3042\u308B\u3002\u6D77\u6C34\u304C\u9AD8\u3044\u6C17\u6E29\u306E\u4E0B\u3067\u84B8\u767A\u3059\u308B\u3053\u3068\u306B\u3088\u308A\u3001\u5CA9\u5869\u3001\u77F3\u818F\u3001\u9730\u77F3\u306E\u6C88\u6BBF\u5C64\u304C\u8868\u9762\u304B\u3089\u5730\u4E0B\u306B\u5411\u304B\u3063\u3066\u898B\u3089\u308C\u308B\u3002\u6D77\u5CB8\u3067\u306F\u3042\u308B\u7A0B\u5EA6\u6D77\u6C34\u304C\u9678\u5730\u306E\u7802\u306B\u5730\u4E0B\u3067\u6D78\u307F\u8FBC\u3093\u3067\u304A\u308A\u3001\u6BDB\u7D30\u7BA1\u5727\u306B\u3088\u308A\u6C34\u5206\u304C\u5730\u8868\u3078\u4E0A\u6607\u3059\u308B\u4F5C\u7528\u304C\u50CD\u304F\u3002\u3055\u3089\u306B\u7D9A\u6210\u4F5C\u7528\u306B\u3088\u308A\u77F3\u818F\u306F\u786C\u77F3\u818F\u306B\u3001\u9730\u77F3\u306F\u82E6\u7070\u77F3\u306B\u5909\u5316\u3059\u308B\u3002\u5927\u6F6E\u3084\u5F37\u98A8\u306B\u3088\u308B\u9AD8\u6CE2\u6D2A\u6C34\u3082\u6D77\u6C34\u3092\u88DC\u7D66\u3057\u3001\u30B5\u30D6\u30AB\u5C64\u306E\u539A\u3055\u306F\u6700\u59271\u30E1\u30FC\u30C8\u30EB\u7A0B\u5EA6\u306B\u306A\u308B\u3002\u307E\u305F\u3001\u7802\u6F20\u5730\u57DF\u306B\u7279\u5FB4\u7684\u306A\u9AD8\u5869\u5206\u306E\u5730\u4E0B\u6C34\u304C\u6D77\u5CB8\u306B\u9054\u3059\u308B\u3053\u3068\u306B\u3088\u3063\u3066\u3082\u3001\u5869\u5206\u304C\u4F9B\u7D66\u3055\u308C\u308B\u3002 \u5178\u578B\u7684\u306A\u30B5\u30D6\u30AB\u306F\u30A2\u30E9\u30D6\u9996\u9577\u56FD\u9023\u90A6\u306E\u6D77\u5CB8\u306B\u898B\u3089\u308C\u308B\u3002\u30A2\u30D6\u30C0\u30D3\u9996\u9577\u56FD\u897F\u7AEF\u306B\u306FSabkha Matti\u3068\u547C\u3070\u308C\u308B\u5E83\u5927\u306A\u5E73\u5766\u5730\u304C\u5E83\u304C\u308A\u3001\u30A2\u30E9\u30D3\u30A2\u534A\u5CF6\u306E\u30EB\u30D6\u30A2\u30EB\u30CF\u30EA\u7802\u6F20\u306E\u4E00\u90E8\u3067\u3042\u308B\u3002\u30C1\u30E5\u30CB\u30B8\u30A2\u306E\u6D77\u5CB8\u8FD1\u304F\u306B\u3082\u30B5\u30D6\u30AB\u3092\u51A0\u3059\u308B\u6E56\u304C\u3044\u304F\u3064\u3082\u5B58\u5728\u3059\u308B\u3002"@ja . . . . "Une sebkha, de l'arabe \u0633\u0628\u062E\u0629, ou une playa, est une d\u00E9pression \u00E0 fond plat, g\u00E9n\u00E9ralement inondable, o\u00F9 les sols sal\u00E9s limitent la v\u00E9g\u00E9tation. La sebkha peut \u00EAtre lacustre \u2014 les eaux s'\u00E9vaporent et laissent des sels \u2014 ou en communication avec la mer (actuellement ou dans le pass\u00E9). Toutes les r\u00E9gions d\u00E9sertiques chaudes pr\u00E9sentent des sebkhas. On a tr\u00E8s longtemps confondu la bordure (chott) et la d\u00E9pression \u00E0 proprement parler (sebkha) ; cette confusion de termes est actuellement en voie de disparition. Le Chott el-J\u00E9rid est la plus grande des sebkha du Maghreb."@fr . . . "Sebha"@pl . . . . . . . . . . "\u30B5\u30D6\u30AB\uFF08\u963F: \u0633\u0628\u062E\u0629\u200E\u3001sabkha\u3001sebkhat\uFF09\u3042\u308B\u3044\u306F\u30B5\u30D6\u30CF\u306F\u3001\u5869\u539F\u306E\u30A2\u30E9\u30D3\u30A2\u8A9E\u3067\u3001\u7802\u6F20\u6C17\u5019\u306E\u6D77\u5CB8\u306E\u6F6E\u4E0A\u5E2F\u306B\u3067\u304D\u308B\u84B8\u767A\u5CA9\u3068\u70AD\u9178\u5869\u5CA9\u3067\u3042\u308B\u3002\u6D77\u6C34\u304C\u9AD8\u3044\u6C17\u6E29\u306E\u4E0B\u3067\u84B8\u767A\u3059\u308B\u3053\u3068\u306B\u3088\u308A\u3001\u5CA9\u5869\u3001\u77F3\u818F\u3001\u9730\u77F3\u306E\u6C88\u6BBF\u5C64\u304C\u8868\u9762\u304B\u3089\u5730\u4E0B\u306B\u5411\u304B\u3063\u3066\u898B\u3089\u308C\u308B\u3002\u6D77\u5CB8\u3067\u306F\u3042\u308B\u7A0B\u5EA6\u6D77\u6C34\u304C\u9678\u5730\u306E\u7802\u306B\u5730\u4E0B\u3067\u6D78\u307F\u8FBC\u3093\u3067\u304A\u308A\u3001\u6BDB\u7D30\u7BA1\u5727\u306B\u3088\u308A\u6C34\u5206\u304C\u5730\u8868\u3078\u4E0A\u6607\u3059\u308B\u4F5C\u7528\u304C\u50CD\u304F\u3002\u3055\u3089\u306B\u7D9A\u6210\u4F5C\u7528\u306B\u3088\u308A\u77F3\u818F\u306F\u786C\u77F3\u818F\u306B\u3001\u9730\u77F3\u306F\u82E6\u7070\u77F3\u306B\u5909\u5316\u3059\u308B\u3002\u5927\u6F6E\u3084\u5F37\u98A8\u306B\u3088\u308B\u9AD8\u6CE2\u6D2A\u6C34\u3082\u6D77\u6C34\u3092\u88DC\u7D66\u3057\u3001\u30B5\u30D6\u30AB\u5C64\u306E\u539A\u3055\u306F\u6700\u59271\u30E1\u30FC\u30C8\u30EB\u7A0B\u5EA6\u306B\u306A\u308B\u3002\u307E\u305F\u3001\u7802\u6F20\u5730\u57DF\u306B\u7279\u5FB4\u7684\u306A\u9AD8\u5869\u5206\u306E\u5730\u4E0B\u6C34\u304C\u6D77\u5CB8\u306B\u9054\u3059\u308B\u3053\u3068\u306B\u3088\u3063\u3066\u3082\u3001\u5869\u5206\u304C\u4F9B\u7D66\u3055\u308C\u308B\u3002 \u5178\u578B\u7684\u306A\u30B5\u30D6\u30AB\u306F\u30A2\u30E9\u30D6\u9996\u9577\u56FD\u9023\u90A6\u306E\u6D77\u5CB8\u306B\u898B\u3089\u308C\u308B\u3002\u30A2\u30D6\u30C0\u30D3\u9996\u9577\u56FD\u897F\u7AEF\u306B\u306FSabkha Matti\u3068\u547C\u3070\u308C\u308B\u5E83\u5927\u306A\u5E73\u5766\u5730\u304C\u5E83\u304C\u308A\u3001\u30A2\u30E9\u30D3\u30A2\u534A\u5CF6\u306E\u30EB\u30D6\u30A2\u30EB\u30CF\u30EA\u7802\u6F20\u306E\u4E00\u90E8\u3067\u3042\u308B\u3002\u30C1\u30E5\u30CB\u30B8\u30A2\u306E\u6D77\u5CB8\u8FD1\u304F\u306B\u3082\u30B5\u30D6\u30AB\u3092\u51A0\u3059\u308B\u6E56\u304C\u3044\u304F\u3064\u3082\u5B58\u5728\u3059\u308B\u3002"@ja . "\u0633\u0628\u062E\u0629"@ar . "Sabcha"@de . . "Sebkha"@es . . . . . "A sabkha (Arabic: \u0633\u0628\u062E\u0629) is a coastal, supratidal mudflat or sandflat in which evaporite-saline minerals accumulate as the result of semiarid to arid climate. Sabkhas are gradational between land and intertidal zone within restricted coastal plains just above normal high-tide level. Within a sabkha, evaporite-saline minerals sediments typically accumulate below the surface of mudflats or sandflats. Evaporite-saline minerals, tidal-flood, and aeolian deposits characterize many sabkhas found along modern coastlines. The accepted type locality for a sabkha is at the southern coast of the Persian Gulf, in the United Arab Emirates. Sabkha is a phonetic transliteration of the Arabic word used to describe any form of salt flat. A sabkha is also known as a sabkhah, sebkha, or coastal sabkha."@en . "Sabkha"@ca . . "\u0421\u0435\u0431\u0445\u0430"@uk . . . "Sebkha"@fr . . . . "Sebha, sebkha, sabkha \u2013 r\u00F3wnina nadmorska regresywnego wybrze\u017Ca w strefie suchego i ciep\u0142ego klimatu, okresowo zalewana przez sztormy lub chwilowe ingresje morskie, w pozosta\u0142ych odcinkach czasu obszar l\u0105dowy. Termin sebha bywa te\u017C stosowany w innym znaczeniu \u2013 jako lokalny (saharyjski) odpowiednik playa."@pl . . . . . "Sabkha o sebkha (de l'\u00E0rab \u0633\u0628\u062E\u0629, sab\u1E96a) \u00E9s el nom en \u00E0rab de les llacunes salades. S\u00F3n molt abundants a Tun\u00EDsia, especialment a la zona central costera del Sahel tunisi\u00E0, i Alg\u00E8ria, per\u00F2 tamb\u00E9 en altres llocs. Les m\u00E9s grans o importants s\u00F3n la sabkha de Sidi El Hani, la sabkha de Monastir, la sabkha d'El Djem, la sabkha d'El Ghorra, la sabkha d'En Noual, la sabkha de Boujemal, la sabkha de Tadder i la sabkha d'El Makta. A la vora de la ciutat de Tunis, hi ha la sabkha de Sejoumi, al sud-oest, i la sabkha d'Ariana, al nord-est. Aquestes llacunes, normalment humides, produeixen sal en assecar-se a l'estiu o mitjan\u00E7ant la intervenci\u00F3 humana."@ca . . . . . . . . . "Une sebkha, de l'arabe \u0633\u0628\u062E\u0629, ou une playa, est une d\u00E9pression \u00E0 fond plat, g\u00E9n\u00E9ralement inondable, o\u00F9 les sols sal\u00E9s limitent la v\u00E9g\u00E9tation. La sebkha peut \u00EAtre lacustre \u2014 les eaux s'\u00E9vaporent et laissent des sels \u2014 ou en communication avec la mer (actuellement ou dans le pass\u00E9). Toutes les r\u00E9gions d\u00E9sertiques chaudes pr\u00E9sentent des sebkhas. On a tr\u00E8s longtemps confondu la bordure (chott) et la d\u00E9pression \u00E0 proprement parler (sebkha) ; cette confusion de termes est actuellement en voie de disparition. Le Chott el-J\u00E9rid est la plus grande des sebkha du Maghreb. Le mot \u00AB sebkha \u00BB est utilis\u00E9 en arabe pour d\u00E9signer le kavir, type de bassin endor\u00E9ique tr\u00E8s pr\u00E9sent dans les d\u00E9serts en Iran ; pris au sens strict les deux termes renvoient toutefois \u00E0 deux types distincts de playa."@fr . . . . . . . . . "\u0627\u0644\u0633\u064E\u0651\u0628\u064E\u062E\u064E\u0629\u064F \u0623\u0648 \u0627\u0644\u0633\u064E\u0651\u0628\u0652\u062E\u064E\u0629\u064F \u0647\u064A \u0623\u0631\u0636 \u0645\u0633\u062A\u0648\u064A\u0629\u060C \u0639\u0627\u062F\u0629 \u0645\u0627 \u062A\u0642\u0639 \u0628\u064A\u0646 \u0635\u062D\u0631\u0627\u0621 \u0648\u0645\u062D\u064A\u0637 \u0623\u0648 \u0643\u0627\u0646\u062A \u0641\u064A\u0645\u0627 \u0633\u0628\u0642 \u0628\u062D\u064A\u0631\u0629 \u0623\u0648 \u0628\u062D\u064A\u0631\u0629 \u0645\u0644\u062D\u064A\u0629\u060C \u0648\u064A\u062A\u0645\u064A\u0632 \u0633\u0637\u062D\u0647\u0627 \u0628\u0648\u062C\u0648\u062F \u062A\u0631\u0633\u0628\u0627\u062A \u0645\u0644\u062D\u064A\u0651\u0629 \u0648\u062C\u0628\u0633\u064A\u0651\u0629 \u0648\u062A\u0631\u0633\u0628\u0627\u062A \u0643\u0631\u0628\u0648\u0646\u0627\u062A \u0627\u0644\u0643\u0627\u0644\u0633\u064A\u0648\u0645 \u0648\u0643\u0630\u0644\u0643 \u0631\u0648\u0627\u0633\u0628 \u062C\u0644\u0628\u062A\u0647\u0627 \u0627\u0644\u0631\u064A\u0627\u062D \u0648\u0627\u0644\u0645\u062F \u0627\u0644\u0645\u0627\u0626\u064A\u0651\u060C \u0648\u0642\u062F \u062A\u062D\u0648\u064A \u0639\u0644\u0649 \u0627\u0644\u0645\u0627\u0621 \u0637\u0628\u0642\u0627\u064B \u0644\u0637\u0648\u0631 \u062A\u0643\u0648\u0651\u0646\u0647\u0627."@ar . . . . . . . . "Eine oder ein Sabcha (auch Sebcha; arabisch \u0633\u0628\u062E\u0629, DMG Sab\u1E2Ba; englisch Sabkha, Sebkha, auch Sebkhat, Sebkhet, in der westlichen Sahara Grara genannt) ist ein flaches, zeitweise mit Wasser gef\u00FClltes Becken ohne Oberfl\u00E4chenabfluss in einem semiariden Gebiet."@de . . . "Con il termine arabo sabkhah (\u0633\u0628\u062E\u0629), o sabkha, o anche sebkha, si indicano le distese di sale o le depressioni incrostate di sale che si incontrano comunemente lungo le coste del Nordafrica e dell'Arabia Saudita. Le sabkhah sono generalmente delimitate da dune di sabbia e presentano un letto morbido, poco cementato ma impermeabile, a causa delle periodiche inondazioni ed evaporazioni. L'elevata concentrazione di acqua di mare e la capillare scomparsa delle acque sotterranee portano alla formazione di depositi di gesso, calcite e aragonite. Si ritiene che in passato la maggior parte delle sabkhah siano state piccole insenature marine e siano analoghe ai bacini in cui si sono formate evaporiti nel passato geologico."@it . . . . . "Con il termine arabo sabkhah (\u0633\u0628\u062E\u0629), o sabkha, o anche sebkha, si indicano le distese di sale o le depressioni incrostate di sale che si incontrano comunemente lungo le coste del Nordafrica e dell'Arabia Saudita. Le sabkhah sono generalmente delimitate da dune di sabbia e presentano un letto morbido, poco cementato ma impermeabile, a causa delle periodiche inondazioni ed evaporazioni. L'elevata concentrazione di acqua di mare e la capillare scomparsa delle acque sotterranee portano alla formazione di depositi di gesso, calcite e aragonite. Si ritiene che in passato la maggior parte delle sabkhah siano state piccole insenature marine e siano analoghe ai bacini in cui si sono formate evaporiti nel passato geologico."@it . . . . . . . . . . . . . . "Sabkhah"@it . . "Sebha, sebkha, sabkha \u2013 r\u00F3wnina nadmorska regresywnego wybrze\u017Ca w strefie suchego i ciep\u0142ego klimatu, okresowo zalewana przez sztormy lub chwilowe ingresje morskie, w pozosta\u0142ych odcinkach czasu obszar l\u0105dowy. Typowe dla sebhy jest gromadzenie si\u0119 wk\u0142adek ewaporat\u00F3w w\u015Br\u00F3d osad\u00F3w w\u0119glanowych, a tak\u017Ce obecno\u015B\u0107 utwor\u00F3w eolicznych. W wyniku intensywnego parowania i wytr\u0105cania si\u0119 soli z roztwor\u00F3w tworz\u0105 si\u0119 czasem nagromadzenia w postaci naskorupie\u0144 i wykwit\u00F3w lub skorup solnych, o grubo\u015Bci wystarczaj\u0105cej do podj\u0119cia ich eksploatacji. Wsp\u00F3\u0142cze\u015Bnie sebhy znane s\u0105 np. z zachodniego wybrze\u017Ca Zatoki Perskiej i z po\u0142udniowego wybrze\u017Ca Morza \u015Ar\u00F3dziemnego. Nazwa sebha pochodzi z j\u0119zyka arabskiego. Termin sebha bywa te\u017C stosowany w innym znaczeniu \u2013 jako lokalny (saharyjski) odpowiednik playa."@pl . . "Una sebkha (en \u00E1rabe, \u0633\u0628\u062E\u0629\u200E, sab\u1E96a, una palabra usada para designar los salares) \u2014tambi\u00E9n transcrita como sabkha, sebkhat o sebkhet\u2014, es un t\u00E9rmino usado en geolog\u00EDa y geomorfolog\u00EDa para designar en regiones \u00E1ridas un dep\u00F3sito sedimentario, parecido a una dura costra superficial, que ocupa la parte inferior de una depresi\u00F3n de alta salinidad y que est\u00E1 m\u00E1s o menos separada de un medio marino. Las sebkhas son form\u00E1ndose a lo largo de costas \u00E1ridas y siempre se caracterizan por la existencia de dep\u00F3sitos de carbonatos-evaporitas con algunos . Algunas calizas org\u00E1nicas se forman de fragmentos de conchas (ricas en calcita) y otros por verdaderos cementerios de restos de moluscos (como son las coquinas) y de invertebrados como radiolarios y foramin\u00EDferos.\u200B"@es . . . . . . "Uma sebkha, sabkha, sabcha, sebkhat ou sebkhet \u00E9 um termo \u00E1rabe que significa terreno salgado, laguna salgada ou deserto de sal, que \u00E9 usado em geologia para designar, em regi\u00F5es \u00E1ridas, dep\u00F3sitos sedimentares, semelhantes a duras crostas superficiais que ocupam a parte inferior de uma depress\u00E3o de alta salinidade e que est\u00E1 mais ou menos separada de um meio marinho. No entanto, o contacto com o meio marinho pode ser permanente, por meio de uma corrente muito fraca (lagoas de \u00E1guas profundas), ou, pelo contr\u00E1rio, por infiltra\u00E7\u00F5es (lagoas pouco profundas). Neste \u00FAltimo caso, pode haver derrames peri\u00F3dicos da \u00E1gua salgada para a bacia hidrogr\u00E1fica."@pt . . . . . . "1092299506"^^ . . . "14670"^^ . . "\u30B5\u30D6\u30AB"@ja . . . . . "\u0421\u0435\u0431\u0445\u0430, \u0441\u0435\u0431\u043A\u0440\u0430 (\u0430\u0440\u0430\u0431. \u0633\u0628\u062E\u0629\u200E) \u2014 \u0437\u0430\u043C\u043A\u043D\u0443\u0442\u0430 \u0431\u0435\u0437\u0441\u0442\u0456\u0447\u043D\u0430, \u0430\u0431\u043E \u043F\u0440\u0438\u0431\u0435\u0440\u0435\u0436\u043D\u043E-\u043C\u043E\u0440\u0441\u044C\u043A\u0430 \u043D\u0438\u0437\u043E\u0432\u0438\u043D\u0430 \u0437 \u043F\u043B\u0430\u0441\u043A\u0438\u043C \u0434\u043D\u043E\u043C, \u044F\u043A\u0435 \u0432\u043A\u0440\u0438\u0442\u0435 \u0441\u043E\u043B\u043E\u043D\u0447\u0430\u043A\u0430\u043C\u0438. \u041F\u0456\u0434\u0432\u0438\u0449\u0435\u043D\u0430 \u043E\u043A\u043E\u043B\u0438\u0446\u044F \u0441\u0435\u0431\u0445\u0438 \u043D\u0430\u0437\u0438\u0432\u0430\u0454\u0442\u044C\u0441\u044F \u0448\u043E\u0442\u0442\u043E\u043C."@uk .