cyanic-selkie/wikianc huggingface dataset:
Sarah Adegoke
Sarah Adegoke (an haife ta a shekara ta 1997) 'yar wasan tennis ce ta Najeriya. A halin yanzu ita ce ta daya a jerin ‘yan wasan Tennis na mata guda daya a cewar hukumar kwallon tennis ta Najeriya.
Sana'a/aiki
An haife ta ne a Ibadan, jihar Oyo, Adegoke ta koyi wasan tennis ta hannun mahaifinta, Adedapo Adegoke, wanda ta lura ba ta da kwarewa sosai amma tana karanta labaran wasanni da mujallu don koya mata dokokin wasan. Ta fara wakiltar Najeriya ne a shekarar 2010, kuma a shekarar 2014 ta kasance mace ta farko a fagen wasan tennis a Najeriya. Ta bayyana Serena Williams a matsayin babban kwarin gwiwarta a wasan. Adegoke ita ce ta zo ta farko a matakin manyan mata a gasar cin kofin Tennis ta CBN karo na 34 a shekarar 2012. Har ila yau, tana daya daga cikin 'yan Najeriya kalilan da suka samu nasarar zuwa wasan karshe na gasar cin kofin gwamna a jihar Legas, abin da ta yi a shekarar 2014, ta sha kashi a hannun Zarah Razafimahatratra ta Madagascar a wasan karshe. A Gasar Tennis ta Ikoyi Club Masters Championship a shekarar 2014, Adegoke mai shekaru 16 a lokacin, ta haifar da bacin rai lokacin da ta lashe gasar cin kofin Tennis na CBN na shekarar 2013, Ronke Akingbade a wasan karshe na mata guda daya.
A watan Fabrairun 2017, ta ci gasar Ikoyi Club Masters Championship. Daga baya a shekarar, ta lashe babbar gasar mata ta daya a gasar cin kofin Tennis ta CBN karo na 39, inda ta doke Marylove Edwards. A watan Disambar 2017, ta doke abokiyar hamayyarta, Blessing Samuel, 6–3, 6–3 inda ta lashe gasar wasan Tennis ta Rainoil Open a babban kulob din Legas.
A watan Agustan 2018, ta kasance a matsayi na daya da na uku a rukunin ‘yan wasa daya da na biyu kamar yadda hukumar kwallon tennis ta Najeriya ta bayyana.
Ibrananci
Ibrananci Ya kasan ce wani yare ne na Semitic. An fara magana da shi a Isra'ila. Yawancin yahudawa da yawa suna magana da Ibrananci, saboda Ibrananci ɓangare ne na addinin Yahudanci. Cibiyar Nazarin Harshen Ibrananci ita ce babbar cibiyar Ibrananci.
Isra'ilawa ne sukae yin shi tun da daɗewa, a lokacin da aka rubuta Littafi Mai-Tsarki. Bayan da Babiloniya ta ci Yahuza da yaƙi, aka kame Yahudawa zuwa Babila suka fara magana da Aramaic. Ba a amfani da Ibrananci sosai a rayuwar yau da kullun, amma har yanzu yahudawa waɗanda ke nazarin littattafan addini sun san shi.
Filin jirgin saman Tokyo Haneda
Filin jirgin saman Tokyo Haneda shi ne babban filin jirgin saman dake birnin Tokyo, babban birnin ƙasar Japan.
Ibrananci
Kamar yadda yake a yau, <sup class="noprint Inline-Template" style="white-space:nowrap;">] Ibrananci shine kawai harshen ɗaya mutu kuma aka sake farfaɗo da shi.
Rasha Kelej
Rasha Kelej (رشا قلج) Sanatan Masar ce. Daga cikin nade-nade 100 da shugaba Abdel Fattah el-Sisi ya yi a majalisar dattawa a shekarar 2020, za ta yi wa'adi na shekaru biyar. Kelej ta kasance tana aiki don ƙarfafa mata da inganta hanyoyin samun lafiya a Afirka da sauran ƙasashe masu tasowa.
Ibrananci
A Littafi Mai Tsarki asali an rubuta a cikin Littafi Mai-Tsarki Hebrew, Littafi Mai-Tsarki Aramaic da kuma Koine Greek.
Rasha Kelej
Tarihin rayuwa
An haifi Kelej a cikin 1972 a Alexandria kuma ta yi digiri a cikin kantin magani a Jami'ar Alexandria. Daga baya ta kammala MBA a CSR Integration with Business dabarun a Jami'ar Robert Gordon. Ta fara aiki a masana'antar harhada magunguna a 1994 kuma ta shiga Merck KGaA a 1996. An nada ta a matsayin Shugabar Merck Foundation a 2016.
Ibrananci
Nahawu
Ibrananci yare ne na Semitic kuma saboda haka yana da yawa kamar Larabci. Ana yin kalmomin Ibrananci ta hanyar haɗa tushe da tsari. A yaren Ibrananci na Isra'ila, ana fassara wasu kalmomi daga yarukan Turai kamar Ingilishi, Faransanci, Jamusanci, da Rasha. Yawancin kalmomi daga Tsohon Alkawari an ba su sababbin ma'anoni a Ibrananci na Isra'ila. Mutanen da ke koyan Ibrananci suna bukatar yin nazarin nahawu da farko don su iya karatu daidai ba tare da wasula ba.
A yaren Ibraniyanci na Isra’ila, babu wata fi’ili “da za a kasance” a halin yanzu, amma kawai a nan gaba da lokutan da suka gabata. A cikin Ibrananci na Baibul, babu wasu kalmomi amma abubuwa biyu ne kawai: ajizai da kamala. A ajizanci wani abu ne kamar na gaba da na yanzu. Kammalallen wani abu ne kamar lokacin da ya gabata. An yi magana da Ibrananci na Mishnaic da kuma Yahuza-Aramaic a zamanin Yesu da kuma a lokacin Bar-Kokhba tawaye ( ƙarni na 2 AD) har zuwa Byzantine Empire of Justinian ( ƙarni na 6 AD).
Rasha Kelej
Tarihin rayuwa
Rasha kuma ta ba da damar horar da ma'aikatan kiwon lafiya da yawa a cikin ƙwararrun ƙwararru masu mahimmanci da ƙarancin aiki kamar su oncology, ciwon sukari, cututtukan zuciya, numfashi, kulawa mai zurfi, ilimin endocrinology da ilimin jima'i da haihuwa ta hanyar shirye-shiryen Merck Foundation.
Ibrananci
Nahawu
An tsara haruffan Ibrananci don rubuta Yiddish, wani yaren yahudawa. Koyaya, Yiddish yana da banbanci da Ibrananci tunda yaren Jamusanci ne.
Rasha Kelej
Tarihin rayuwa
A cikin 2019, Kelej ta kasance cikin jerin 'yan Afirka 100 Mafi Tasirin Sabon Mujallar Afirka.
Ibrananci
Haruffa
Haruffan Ibrananci suna da haruffa 22. Biyar daga cikinsu suna canzawa lokacin da suke ƙarshen kalma. Ibrananci ana karanta shi kuma ana rubuta shi daga dama zuwa hagu. Haruffa ukun farko, aleph, beth da gimel, ana amfani dasu a cikin ilimin lissafi a cikin mahallin lambobi marasa iyaka.
Haruffan Ibrananci abjad ne don haka baƙaƙe ne kawai ake rubutu, kuma masu karatu dole ne su samar da wasula. Tunda hakan na iya zama da wahala, ana iya sanya wasula a matsayin ɗigo da ake kira alamun "nikkud" ko "tnuah" (jam'i "nikkud" da "tnuot" bi da bi. ) A cikin Ibraniyancin Zamani, wasu haruffa na iya nuna wasula, waɗanda ake kira matres lectionis (iyayen karatu) tunda suna taimakawa karatun sosai. Vav (ko Waw) na iya yin sautin 'oo' (/ u / a cikin IPA) kamar a cikin f oo d. Yodh (ko Yud) na iya yin sautin 'ee' (/ i / a cikin IPA) kamar a cikin f ee d.
Zainab Gimba
Zainab Gimba (an haife ta a ranar 25 ga Disamba, 1972) yar siyasan Najeriya ce. An zabe ta a Majalisar Wakilan Najeriya a matsayin ‘yar takarar jam’iyya mai mulki ta APC a mazabar tarayya na mazabar Bama / Ngala / Kala Balge, Jihar Borno. Mamba ce a kungiyar mata ta Commonwealth Women Parliamentaries (CWP) kuma mai ba da shawara ga wakilci da kiyaye daidaiton jinsi. kuma tana fafutikan nema ma mata yanci ta bangaren jinsi da kuma daidaito a tsakanin su da maza.
Ilimi
Zainab tana da BS.c a cikin Gudanar da Jama'a. Ta kuma kara bunkasa karatunta sannan ta samu digiri na biyu a bangaren mulki. Tana da PhD a cikin Gudanar da Jama'a da Nazarin Manufofi.
Ayyuka
Lokacin 2011 zuwa 2014, ta yi aiki a matsayin Hon. Kwamishina Ma'aikatar rage talauci da karfafawa matasa a jihar ta Borno. Ta kuma yi aiki a matsayin Hon. Kwamishina Hukumar Kula da Ilimin Farko ta Jihar Borno daga 2014 zuwa 2015. An nada ta a matsayin Hon. Kwamishina Ma'aikatar Albarkatun Ruwa ta Jihar Borno a 2015 kuma ya yi aiki har zuwa 2018.
A yayin taron majalisar dokoki na Commonwealth karo na 64 (CPC) a Speke Resort Munyonyo, Kampala a shekarar 2019, an zabi Zainab a matsayin mataimakiyar shugabar mata ta kungiyar mata ta Commonwealth (CWP) a yankin Afirka.
Adralés
Adralés ya kasan ce kuma yana ɗaya daga cikin majami'u 54 a cikin Cangas del Narcea, wata karamar hukuma ce a cikin lardin kuma tana da ikon mallakar Asturias, a arewacin Spain. Ikklesiyar ta ƙunshi ƙauyuka uku: Adralés, Villar de Adralés da El Altu Santarvás. Kauyen Adralés yana da nisan kilomita uku kudu maso gabas na babban birnin Cangas del Narcea.
Tattalin arzikin Adralés koyaushe yana dogara ne akan kiwon shanu. Dangane da kusancin ƙauyen da garin Cangas del Narcea, manoma daga Adralés koyaushe suna cikin kasuwannin ta har ma suna iya ba shi madara, alhali mafi yawan ƙauyukan karamar hukumar suna kiwon shanu ne kawai don naman su tunda ba su iyawa safara ko adana madara. A halin yanzu yawancin mazaunan Adralés manoma ne da suka yi ritaya ko matasa da ke aiki a Cangas.
A kuma ƙarnin da suka gabata mutane da yawa sun yi ƙaura zuwa Cuba da Philippines daga wannan yankin. A zahiri, "Adrales" suna ne gama gari a cikin Filipinas, wanda ya samo asali daga wannan lardin na Asturia.
A cikin ƙarni na 19 kuma ya ci gaba har zuwa 1970s, Adralés ya rasa yawancin yawansa zuwa ƙaura. Yawancin ƙaura sun yi hanyar zuwa Madrid a matsayin masu tsaron dare. Yawancin mutane sun yi ƙaura zuwa Argentina da Venezuela, yayin da a cikin shekarun 1960s da 1970s kusan kowane magidanci a ƙauyen ya aika ɗayan membobinsa zuwa Switzerland.
Shahararrun mazauna
José Calvo Martínez, ya kasan ce wani babban sakatare na Unión de Campesinos Asturianos (Union of Asturian Farmworkers) tun 1995
Aurelio Ordás Rodríguez (1942-), wanda ya kafa kuma ya taɓa zama shugaban cibiyar Asturian sau uku a Basel, Switzerland da kuma darektan gida na Socialungiyar Partyan kwadagon Spanishan kwadagon Spain a Basel. Yayi hijira zuwa Faransa a 1961 sannan daga baya zuwa Switzerland. Ya kuma kasance darektan sauran ƙungiyoyin baƙi na ƙasar Sifen a Switzerland.
Rimi
Rimi (Ceiba pentandra) bishiya ce data shahara a yawancin garuruwan hausawa arewacin Nijeriya.
1980
1980 ita ce shekara ta dubu ɗaya da dari tara da tamanin a ƙirgar Miladiyya.
Mogakolodi Ngele
Mogakolodi Ngele (an haife shi a ranar 6 ga watan Oktoba 1990 a Gaborone) ɗan wasan ƙwallon ƙafa ne na ƙasar Botswana wanda a halin yanzu yana buga wasa a ƙungiyar ƙwallon ƙafa ta ƙasar Afirka ta Kudu wato Chippa United da kuma ƙungiyar ƙwallon ƙafa ta ƙasar Botswana a matsayin ɗan wasan tsakiya. Ya koma Bidvest Wits daga Mamelodi Sundowns. Ya kasance dan takara a gasar cin kofin Afrika na shekarar 2012. A cikin shekarar 2014, ya rattaba hannu kan kwantiragin shekaru 5 da Mamelodi Sundowns FC duk da haka, zai ci gaba da zama a kulob din da yake yanzu har zuwa karshen kakar wasa ta 2014-15. Bidvest Wits daga nan kuma ta sake rattaba hannu da shi aro har zuwa karshen kakar wasa ta 2016–17 wanda Bidvest Wits da Ngele suka lashe kofin Absa Premiership inda suka doke irin su Cape Town, Mamelodi Sundowns da Kaizer Chiefs.
Bayan ya dawo daga matsayin aro a Bidvest Wit, a kakar wasa ta 2017-2018 ya yi fama da rashin samun lokacin buga wasa, yana buga wasa ne kawai a duk kakar wasa, inda kocin Mamelodi Sundowns Pitso Mosimane ya ce "yana bukatar ya nuna kansa don fara wasa acikin goma sha daya farko".
Tafsirin Nisaburi
Ghara'ib al-Qur'an wa Ragha'ib al-Furqan ( غرائب القرآن ورغائب الفرقان  ; lit.  '  Abubuwan Al'ajabi na Kur'ani da Desiderata na Ma'auni ' ) ko, mai suna a takaice, Ghara'ib al-Qur'an ( lit.  '  Abubuwan Al'ajabi na Kur'ani ' ), wanda aka fi sani da Tafsir al-Nisaburi ( تفسير النيسابوري   ), Sunni ne na gargajiya – Sufi  tafsir (exegesis) of the Qur'an,  tafsir ( tafsirin Alqur'ani,  wanda Shafi'i - malamin Ash'ari Nizam al-Din al-Nisaburi ya rubuta (ya rasu a c. 730 AH ; c. 1330 CE), wanda ke bin tafsir al-Fakhr al-Razi a wurare da dama.
Shi ne tafsirin Alkur'ani na farko da aka rubuta a Indiya. Ana samun kwafin wannan sharhin da aka rubuta da hannu a ɗakin karatu na kabarin Hadrat Peer Muhammad Shah Sahib a Ahmedabad.
liyafar
A cewar Muhammad Husayn al-Dhahabi,  ya yaba da tafsirin. (ya rasu a shekarar 1313 AH ; 1895 CE ) a cikin littafinsa Rawdhat al-Jannat.
Game da marubucin
Shi masanin lissafin Farisa ne, masanin taurari, Faqīh (masanin shari'a), tafsirin Kur'ani, mawaƙi, kuma galibi ana ɗaukarsa a matsayin mai hikima, wato wanda ya dace da falsafa da dabaru. An haife shi a Nisapur kuma an san shi da Nizam al-A'raj. Asalin danginsa da danginsa shi ne birnin Kum. Bayan kammala karatunsa ya zo Indiya, ya zauna a can, mai yiwuwa a Daulatabad. Ya rubuta littafai da dama a kan Falsafa, Geography da Sufanci. Ya sake rubuta wani tafsirin Alkur'ani a wani mujalladi da ake kira Lub al-Ta'wil fi Tafsir al-Qur'an. Ba a san ainihin shekarar mutuwarsa ba, amma ta kasance bayan shekarar 1329 CE. Ana ba da rahoto akai-akai a cikin bayanan da aka samu kamar yadda ya faru a cikin shekaru daga shekarar 710 AH zuwa ta 728 AH.
Lusaka
Lusaka (lafazi : /lusaka/) birni ne, da ke a ƙasar Zambiya. Shi ne babban birnin ƙasar Zambiya. Lusaka yana da yawan jama'a 2,400,000, bisa ga jimillar 2010. An gina birnin Lusaka a farkon karni na ashirin.
Hotuna
<Gallery> File:Downtown Lusaka.JPG|Downtown Lusaka File:Embassy of Russia in Lusaka.jpg|Ofishin Jakadancin Rasha a Lusaka File:Lusaka International Airport, Zambia - entrance, 2015.jpg|Kofar shiga filin jirgin sama, Lusaka Zambia File:Lusaka Central Fire Station.JPG|Tashar kashe gobara ta tsakiyar birnin Lusaka. File:Zambia - Street in Lusaka.jpg|Wani titi a birnin Lusaka </Gallery>
Zaizayar Kasa
A cikin ilimin kimiyyar ƙasa, yashewar shi ne aikin hanyoyin ƙasa (kamar kwararar ruwa ko iska) wanda ke cire ƙasa, dutse, ko narkar da abu daga wuri guda a kan bagon duniya, sannan ya ɗauke shi zuwa wani wuri. Rushewa ya bambanta da yanayin wanda bai ƙumshi motsi ba. Kau da dutse ko ƙasa kamar yadda "classic" laka ake cewa jiki ko inji yashewa. Wannan ya bambanta da lalacewar sinadarai, inda kuma ake cire ƙasa ko kayan dutse daga wani yanki ta hanyar narkewa. Za a iya safarar gurɓataccen ruwa ko ɗan ƙaramin milimita, ko kuma na dubban kilomita.
Duk da yake zaizayar ƙasa tsari ne na halitta, ayyukan ɗan adam sun ƙaru da sau 10-40 ƙimar da zaizayar ƙasa ke faruwa a duniya. A wuraren aikin gona da ke tsaunukan "Appalachian", ayyukan noma mai zurfi sun haifar da zaizayar ƙasa har sau ɗari bisa ɗari na yawan zaizayar ƙasa a yankin. Yawan zaizayar ƙasa (ko hanzarta) zai haifar da matsalolin “a-site” da “off-site”. Tasirin yanar-gizon ya haɗa da raguwar yawan amfanin gona da (a kan shimfidar wurare na halitta) rushewar muhalli da duka saboda asarar raƙuman ƙasa mai wadataccen abinci mai gina jiki. A wasu lokuta, wannan yana haifar da kwararowar hamada. Kashe-site effects hada sedimentation na waterways da eutrophication na ruwa jikinsu, kazalika da laka lalacewar hanyoyi da kuma gidaje. Raguwar ruwa da iska sune manyan abubuwan da ke haifar da lalacewar ƙasa ; a hade, su ke da alhakin kusan kashi tamanin da biyar (84%) na yawan ƙasashen duniya na ƙasƙantar da ƙasa, suna mai da yaƙar wuce gona da iri ɗaya daga cikin mahimman matsalolin muhalli a duka duniya.
Noma mai zurfi, sare bishiyoyi, hanyoyi, canjin yanayi na ɗan adam da yaɗuwar birane suna daga cikin mahimman ayyukan ɗan adam dangane da tasirin su a kan kwararowar. Koyaya, akwai hanyoyin rigakafi da gyara da yawa waɗand n zasu iya ragewa ko iyakance yaƙar ƙasa mai rauni.
Tsarin jiki
Ruwan sama, da kuma surface dake kwarara wanda zai iya haifar da daga ruwan sama, samar hudu main iri ƙasa yashewa : fantsama yashewa, takardar yashewa, rill yashewa, kuma gully yashewa. Ana ganin ɓarkewar ɓarna a matsayin mataki na farko kuma mafi ƙanƙanta a cikin ɓarnawar ƙasa, wanda ke biye da ɓarna ta takarda, sannan yayyafin yaƙi kuma a ƙarshe gully erosion(mafi tsananin huɗu).
A cikin zaizayar ƙasa, tasirin saukar ruwan sama yana haifar da ƙaramin rami a cikin ƙasa, yana fitar da ƙwayoyin ƙasa. Nisan da waɗannan ƙwayoyin ƙasa ke tafiya na iya zama har zuwa 0.6 m (ƙafa biyu) a tsaye da 1.5 m (ƙafa biyar) a kwance a ƙasa.
Idan ƙasa ta ƙoshi, ko kuma idan ruwan sama ya fi yadda ruwan zai iya shiga cikin ƙasa, kwararar ruwa na faruwa. Idan gudun ruwan yana da isasshen karfi, shi zai safarar gãshin ƙasa barbashi ( laka ) saukar da gangara. Rushewar takarda ita ce safarar barbashin ƙasa da aka sassaƙa ta kwararar ƙasa. Zaaizayar kasa na - Rill yana nufin ci gaban da kananan, ephemeral da mayar da hankali da kwarara hanyoyi da aiki kamar yadda biyu laka tushen da laka isarwa tsarin for yashewa a kan hillslopes. Gabaɗaya, inda ƙimar yashewar ruwa a yankunan da ke cikin tashin hankali ya fi girma, rills yana aiki. Zurfin zurfafa a cikin rills yawanci tsari ne na 'yan santimita (kusan inci) ko ƙasa da haka kuma gangarawar tasha na iya zama mai tsayi. Wannan yana nufin cewa rills suna nuna kimiyyar hydraulic sun sha bamban da ruwan da ke gudana ta cikin zurfi, manyan hanyoyin rafi da koguna.
Rushewar haushi yana faruwa lokacin da ruwa ya kwarara kuma yana gudana cikin sauri a cikin kunkuntar tashoshi yayin ko nan da nan bayan ruwan sama mai ƙarfi ko narkewar dusar ƙanƙara, yana cire ƙasa zuwa zurfin zurfi.
Matsanancin zaizayar ƙasa zai iya ci gaba zuwa samuwar gandun daji. Waɗannan suna samuwa a ƙarƙashin yanayin babban taimako a kan sauƙaƙƙen gindin ƙasa a cikin yanayin da ya dace da zaizayar ƙasa. Yanayi ko hargitsi da ke iyakance haɓakar tsirowar kariya (rhexistasy) sune babban jigon samuwar badland.
Kogi da rafi
Zaizayar kasa na rafi ko kogi na faruwa tare da ci gaba da kwararar ruwa tare da sifa mai layi. Rushewar yana ƙasa duka, yana zurfafa kwarin, kuma yana kan gaba, yana faɗaɗa kwarin zuwa cikin tsauni, yana haifar da yanke kai da bankunan tudu. A matakin farko na yashewar rafi, aikin lalata yana da yawa a tsaye, kwaruruka suna da sashi mai fasali na V kuma raƙuman rafi yana da tsayi. Lokacin da aka kai wani matakin tushe, aikin lalata zai canza zuwa yashewar gefe, wanda ke faɗaɗa kwarin kuma yana haifar da kunkuntar ambaliyar ruwa. Jigon rafi ya zama kusa da leɓe, kuma ɗorawar ɓoyayyen ɓoyayyiyar ƙasa ta zama mai mahimmanci yayin da rafin ke ratsa ƙasan kwarin. A duk matakai na yashewar rafi, zuwa yanzu mafi yawan zaizayar ƙasa tana faruwa a lokutan ambaliyar ruwa lokacin da ake samun ƙarin ruwa mai sauri da sauri don ɗaukar nauyin rami mafi girma. A cikin irin waɗannan hanyoyin, ba ruwa kaɗai ne ke ɓarna ba: dakatar da barbashi, tsakuwa, da duwatsu suma suna iya yin lalata yayin da suke wucewa ta farfajiya, a cikin tsarin da ake kira traction.
Zaizayar bakin rafi shine lalacewar bankunan rafi ko kogi. An bambanta wannan daga canje -canje a kan gado na magudanar ruwa, wanda ake kira scour. Ana iya auna gurɓacewa da canje -canje a cikin yanayin bankunan kogi ta hanyar saka sandunan ƙarfe a cikin bankin tare da yin alamar matsayin saman bankin tare da sandunan a lokuta daban -daban.
Zaizayar Thermal kuwa shine sakamakon narkewa da raunana permafrost saboda ruwa mai motsi. Zai iya faruwa a gefen koguna da a bakin teku. Gudun hijirar tashar kogi mai saurin gani da aka gani a cikin Kogin Lena na Siberia ya faru ne saboda lalacewar ɗumbin zafi, saboda waɗannan ɓangarorin bankunan sun haɗa da kayan da ba a haɗe da permafrost-ciminti ba. Yawancin wannan rushewar yana faruwa yayin da bankunan da aka raunana suka gaza a cikin manyan raguwa. Har ila yau, zaizayar ƙasa tana shafar tekun Arctic, inda aikin raƙuman ruwa da yanayin zafi kusa da tudu ke haɗuwa don lalata gandun dajin permafrost a gefen tekun kuma ya sa su kasa. Yawan lalacewar shekara-shekara tare da yanki 100 km na Tekun Beaufort ya kai 5.6 m a kowace shekara daga 1955 zuwa 2002.
RI
RI ko ri na iya nufin to:
Zaizayar Kasa
Kogi da rafi
Yawancin yashewar kogi yana faruwa kusa da bakin kogi. A kan lanƙwasa kogi, mafi ƙarancin mafi kaifi yana da ruwa mai motsi a hankali. A nan ana yin ajiya. A kan mafi ƙanƙantar da gefen lanƙwasa, akwai ruwa mai motsi da sauri don haka wannan gefen  yana ɓarna galibi.
Rushewa da sauri ta hanyar babban kogi na iya cire isasshen gurɓataccen ruwa don samar da layin kogin, kamar yadda koma baya na ɗaga gadajen dutse waɗanda ba su da nauyi ta lalacewar gadaje masu wuce gona da iri.
Zaizayar bakin teku
Zaizayewar bakin teku, wanda ke faruwa a kan wuraren da aka fallasa da kuma mafaka, da farko yana faruwa ta hanyar aiki na raƙuman ruwa da raƙuman ruwa amma canjin matakin teku (tidal) shima zai iya taka rawa. Lamari da ake kira hydraulic na farywa ne lokacin da iska a cikin haɗin gwiwa ba zato ba tsammani ta matsa ta hanyar igiyar ruwa ta rufe ƙofar haɗin gwiwa. Wannan sai ya fashe. Tashin igiyar ruwa shine lokacin da kuzarin kuzarin da ke bugun dutse ko dutse ya fashe. Abrasion ko corrasion yana faruwa ne sakamakon raƙuman ruwa da ke ɗora ruwan teku a dutsen. Ita ce mafi inganci da saurin gurɓataccen yashi (kada a ruɗe da lalata). Gurbatawa shine narkar da dutsen ta hanyar carbonic acid a cikin ruwan teku. Ƙwanƙolin duwatsu suna da haɗari musamman ga irin wannan zaizayar ƙasa. Haɗuwa shine inda barbashi/nauyin ruwan da raƙuman ruwa ke ɗauke da su yayin da suke bugun junansu da duwatsu. Wannan to yana sauƙaƙe kayan don wankewa. Kayan ya ƙare kamar shingle da yashi. Wani muhimmin tushen zaizayar ƙasa, musamman a gabar tekun carbonate, yana da ban sha'awa, ɓarna da niƙa ƙwayoyin cuta, tsarin da ake kira bioerosion.
Laka da aka dauko tare da bakin tekun a cikin shugabanci na da rinjaye halin yanzu ( longshore gantali ). Lokacin da samar da gurɓataccen ruwa ya yi ƙasa da adadin da ake ɗauka, zaizayar ƙasa na faruwa. Lokacin da yawan ɓoyayyen ɗimbin ya yi yawa, yashi ko bankunan tsakuwa za su kasance suna haifar da sakamakon sakawa. Waɗannan bankunan na iya yin sannu a hankali yin ƙaura tare da bakin tekun a cikin hanyar tsallaken tekun, a lokaci guda suna karewa da fallasa sassan gabar teku. Inda akwai lanƙwasawa a cikin gabar teku, galibi ana samun ɓataccen abu mai ɓarna wanda ke haifar da dogon bankin mai kunkuntar ( tofa ). Armoured rairayin bakin teku da kuma kura idon teku sandbanks yiwu ma kare sassa na wani ƙirin daga yashewa. A cikin shekarun da suka gabata, yayin da sandunan ke canzawa sannu a hankali, ana iya juyar da zaizayar zuwa farmaki sassa daban -daban na gabar.
Rushewar sunadarai
Samuwar ramuka da sauran fasalulluka na karst - topography misali ne na yaɗuwar sunadarai da yawa.
Cyril Ramaphosa
Cyril Ramaphosa (lafazi: [siril ramafosa]) ɗan siyasan Afirka ta Kudu ne. An haife shi a shekara ta 1952 a Soweto, Afirka ta Kudu. Cyril Ramaphosa shugaban kasar Afirka ta Kudu ne daga watan Fabrairu a shekara ta 2018 (bayan Jacob Zuma).
Zaizayar Kasa
Glaciers
Glaciers sun zaizaye galibi ta hanyoyi daban -daban guda uku: abrasion/scouring, plucking, and ice thrusting. A cikin tsarin abrasion, tarkace a cikin ƙanƙara mai ƙanƙara a kan gado, gogewa da goge duwatsun da ke ƙarƙashinsu, kama da sandpaper akan itace. Masana kimiyya sun nuna cewa, baya ga rawar zafin da ake takawa a cikin zurfafa kwarin, sauran hanyoyin glaciological, kamar zaizayar ƙasa kuma tana sarrafa bambancin giciye. A cikin tsarin gurɓataccen ɗigon ƙasa, an ƙirƙiri sashe mai lanƙwasa a ƙarƙashin kankara. Kodayake dusar ƙanƙara tana ci gaba da ɓacewa a tsaye, siffar tashar da ke ƙarƙashin kankara a ƙarshe za ta kasance mai ɗorewa, ta kai sifar U-dimbin kwatankwacin hali kamar yadda muke gani yanzu a cikin kwaruruka masu ƙanƙara. Masana kimiyya kuma suna ba da adadi na adadi na lokacin da ake buƙata don samun kyakkyawan kwarin siffa mai kama da U — kusan shekaru 100,000. A cikin ƙasa mai rauni (yana ɗauke da kayan da za a iya ƙerawa fiye da duwatsun da ke kewaye) ƙirar ɓarna, a akasin haka, an ƙuntata yawan zurfin zurfin saboda ƙanƙara da ƙanƙara na raguwa.
Glaciers  kuma na iya haifar da gutsuttsarin gutsuttsarin guguwa yayin aiwatar da girbi. A cikin dusar ƙanƙara, ƙanƙara ta daskare zuwa gadonta, sannan yayin da ta hau gaba, tana motsa manyan zanen daskararre a ƙasan tare da ƙanƙara. Wannan hanyar ta samar da wasu dubban tafkunan tafkin da ke gefen Garkuwar Kanada. Bambance -bambancen da ke tsakanin tsayin dutsen ba wai kawai sakamakon tasirin tectonic bane, kamar ɗaga dutse, har ma da canjin yanayi na gida. Masana kimiyya suna amfani da nazarin yanayin duniya don nuna cewa zaizayar ƙanƙara tana sarrafa matsakaicin tsayin tsaunuka, saboda sauƙaƙe tsakanin tsaunukan tsaunin da layin dusar ƙanƙara gaba ɗaya ya takaita zuwa tsaunuka ƙasa da 1500. m. Rushewar da dusar ƙanƙara ke haifarwa a duk duniya tana lalata tsaunuka yadda yakamata ta zama ana amfani da kalmar buzzsaw glacial, wanda ke bayyana iyakance tasirin kankara akan tsayin tsaunin. Yayin da tsaunuka ke ƙaruwa, galibi suna ba da damar ƙarin ayyukan ƙanƙara (musamman a yankin tarawa sama da madaidaicin layin glacial), wanda ke haifar da karuwar yuwuwar dutsen, yana rage yawan taro da sauri fiye da sake dawo da isostatic zai iya ƙarawa kan dutsen. Wannan yana ba da kyakkyawan misali na madaidaicin madaidaicin amsa. Binciken da ke gudana yana nuna cewa yayin da ƙanƙara ke ƙoƙarin rage girman dutsen, a wasu yankuna, ƙanƙara na iya rage haɓakar zaizayar ƙasa, yana aiki a matsayin kayan yaƙi na kankara. Kankara ba zai iya lalata duwatsu kawai ba amma kuma yana iya kare su daga ɓarna. Dangane da tsarin ƙanƙara, har ma da ƙasa mai tsayi mai tsayi ana iya kiyaye ta ta lokaci tare da taimakon kankara. Masana kimiyya sun tabbatar da wannan ka’idar ta hanyar yin samfarin taro takwas na arewa maso yammacin Svalbard ta amfani da Be10 da Al26, suna nuna cewa arewa maso yammacin Svalbard ya canza daga yanayin ƙanƙara-ƙanƙara a ƙarƙashin matsakaicin matsakaicin ƙanƙara mai tsananin ƙanƙara, zuwa yanayin ƙanƙara-makamai da ke cike da sanyi, kankara mai kariya lokacin da yawan sanyin sanyi mafi yawa na glaima yayin da shekarun ƙanƙara na Quaternary ya cigaba.
Waɗannan matakai, haɗe da yashewa da sufuri ta hanyar ta hanyar ruwa a ƙarƙashin ƙanƙara, suna barin yanayin ƙasa mai ƙyalli kamar moraines, drumlins, moraine na ƙasa (har), kames, kame deltas, moulins, da kura -kurai a cikin farkawarsu, yawanci a tashar ko a lokacin komawar kankara.
Mafi kyawun ci-gaban yanayin kwarin gwal yana bayyana cewa an iyakance shi ga shimfidar wurare tare da ƙarancin ƙimar dutsen (ƙasa da ko daidai da 2mm a kowace shekara) da babban taimako, wanda ke haifar da lokutan juyawa. Inda yawan hauhawar dutsen ya zarce 2mm a kowace shekara, ilimin halittar kwarin gwal na gaba ɗaya an canza shi sosai a cikin lokacin postlalacial. Haɗuwa da yaɗuwar kankara da tilasta tectonic shine ke jagorantar tasirin ilimin glaciations akan orogens masu aiki, ta hanyar tasiri tsayin su, da kuma canza fasalin ɓarna a cikin lokutan glacial mai zuwa ta hanyar haɗin gwiwa tsakanin dutsen dutsen da siffar giciye.
Ambaliya
A manyan kwarara, kolks, ko vortices ana samun su ta manyan kundin ruwa mai saurin gudu. Kolks yana haifar da matsanancin zaizayar ƙasa, yana ɗebo gindin ƙasa da ƙirƙirar fasali irin na tudun ƙasa da ake kira kwandon dutse. Ana iya ganin misalai a cikin yankunan ambaliyar ruwa sakamakon tafkin Lake Missoula, wanda ya haifar da ɓarna a yankin Columbia Basin na gabashin Washington.
Ruwan iska
Zaizayar iska ya kasance muhimmin abu a labarin kasa e, musamman a yankuna masu bushewa da bushewa. Hakanan babban tushen lalata ƙasa, ƙaura, hamada, ɓarna mai iska mai cutarwa, da lalacewar amfanin gona - musamman bayan an ƙaru sama da ƙimar dabi'a ta ayyukan ɗan adam kamar gandun daji, birane, da aikin gona.
Rushewar iska na iri biyu ne na farko: ɓarna, inda iska ke ɗauka kuma ta kwashe barbashi mara nauyi; da abrasion, inda saman yake lalacewa yayin da guguwar iska ke ɗauke da su. An raba rabe -raben gida gida uku: (1) rarrafe a saman, inda mafi girma, barbashi masu nauyi ke zamewa ko mirgina a ƙasa; (2) gishiri, inda ake ɗaga barbashi a ɗan gajeren tsawo zuwa cikin iska, kuma ya yi tawaye da gishiri a ƙasan ƙasa; da (3) dakatarwa, inda ƙanana da ƙanƙara masu sauƙi iska ke ɗaga su cikin iska, kuma galibi ana ɗaukar su zuwa nesa mai nisa. Gishirin yana da alhakin yawancin (50-70%) na yashewar iska, sannan dakatarwa (30-40%), sannan rarrafewar ƙasa (5-25%).
Zaizayar iska ya fi tsanani a yankunan da ba su da ruwa da kuma lokacin fari. Misali, a cikin Manyan Filaye, an kiyasta cewa asarar ƙasa saboda ɓarnawar iska na iya ninka har sau 6100 a cikin shekarun fari fiye da na damina.
Tafiya taro
Motsawar babban jiki 9wao (Mass Movement) shine motsi na ƙasa da na waje na dutsen da gutsuttsura a kan tudu, galibi saboda ƙarfin nauyi.
Motsawar jama'a wani muhimmin sashi ne na tsarin gurɓataccen yanayi kuma galibi shine matakin farko a cikin ɓarna da jigilar kayan masarufi a cikin tsaunuka. Yana motsa abu daga tsaunuka masu tsayi zuwa mafi ƙasƙanci inda sauran wakilan da ke lalata abubuwa kamar rafuffuka da ƙanƙara za su iya ɗaukar kayan kuma su motsa shi har ma da ƙananan tsaunuka. Tsarin motsi-motsi koyaushe yana faruwa akai-akai akan duk gangaren; wasu matakan motsi-taro suna aiki a hankali; wasu na faruwa ba zato ba tsammani, galibi tare da munanan sakamako. Duk wani motsi mai gangarawa-ƙasa na dutsen ko ɓarna galibi ana kiran su gaba ɗaya azaman zaftarewar ƙasa. Koyaya, zaftarewar ƙasa za a iya rarrabasu ta hanyar cikakken bayani wanda ke nuna hanyoyin da ke da alhakin motsi da saurin motsi. Daya daga cikin wanda ake iya gani topographical manifestations na wani sosai m nau'i na irin wannan aiki shi ne wani scree gangara.
Slumping yana faruwa a kan kasa masu tudu, yana faruwa tare da yankuna daban -daban masu fashewa, galibi a cikin kayan kamar yumɓu wanda, da zarar an sake shi, na iya motsawa cikin sauri. Sau da yawa za su nuna ɓacin rai isostatic mai siffa mai siffa, wanda kayan ya fara zamewa ƙasa. A wasu lokuta, raunin yana faruwa ne ta hanyar ruwa ƙarƙashin gangaren yana raunana shi. A lokuta da yawa kawai sakamakon ƙarancin injiniyanci ne akan manyan hanyoyin inda abin yake a kai a kai.
Roslyne Akombe
Roselyn Kwamboka Akombe (an haife ta a shekara ta 1976) tsohuwar kwamishiniyar Kenya ce ta Hukumar Zaɓe da Kan Iyakoki (IEBC) ta Kenya.
Zaizayar Kasa
Tafiya taro
Surface creep shine jinkirin motsin ƙasa da tarkace dutsen ta hanyar nauyi wanda galibi ba a iya fahimtarsa sai ta tsawaita kallo. Koyaya, kalmar kuma tana iya bayyana mirgina barbashi ƙasa da aka watsa 0.5 to 1.0 mm a cikin diamita ta iska tare da saman ƙasa.
Roslyne Akombe
Ta shahara a kafafen yada labarai na kasar Kenya bayan ta bayyana a gaban hukumar da ke tattaunawa da wadanda za su nada a hukumar, ta kuma ce a shirye ta ke ta karbi sabon mukaminta na kwamishina, duk da cewa hakan na nufin za a rage ma ta albashi da kashi 70 cikin 100 daga aikinta na baya. a matsayin Mataimakin Sakatare a Majalisar Dinkin Duniya. Ta ce wannan sadaukarwa ce da ta ke a shirye ta yi wa kasarta. Ta shahara a duniya bayan ta yi murabus daga mukaminta na kwamishina a ranar 18 ga Oktoba 2017 a cikin rikicin siyasa a Kenya.
Zaizayar Kasa
Yanayi (Climate)
Adadi da tsananin tsananin zubar ruwa, kankara ko raba daga sama shine babban abin da ke haifar da lalacewar ƙasa ta ruwa. Dangantaka ne musamman karfi idan nauyi ruwan sama ya auku a sau a lokacin, ko a wurare inda, kasar gona ta surface ba da kariya da ciyayi. Wannan na iya kasancewa a lokacin lokutan da ayyukan noma ke barin ƙasa babu ruwa, ko kuma a cikin yankuna masu ƙarancin bushe inda ciyayi ba su da yawa. Rushewar iska na buƙatar iska mai ƙarfi, musamman a lokutan fari lokacin da ciyayi ba su da yawa kuma ƙasa ta bushe (haka ma ya fi ƙaruwa). Wasu dalilai na yanayi kamar matsakaicin zafin jiki da kewayon zafin jiki na iya shafar zaizayar ƙasa, ta hanyar tasirin su akan ciyayi da kaddarorin ƙasa. Gabaɗaya, idan aka ba da irin wannan ciyayi da tsirrai, yankunan da ke da ƙarin hazo (musamman ruwan sama mai ƙarfi), ƙarin iska, ko guguwa ana tsammanin za su sami ƙarin lalata.
Roslyne Akombe
Jim kadan bayan murabus din nata, ta tashi daga kasar saboda fargabar rayuwarta a cikin yanayin siyasar da ake ciki.
Zaizayar Kasa
Yanayi (Climate)
A wasu yankunan na duniya (misali tsakiyar Amurka ta yamma ), tsananin ruwan sama shine babban abin da zai ƙaddara ƙaƙƙarfan gurɓataccen iska (don ma’anar bincike na ɓarna, ) tare da ƙara yawan ruwan sama gabaɗaya wanda ke haifar da ƙarin lalata ƙasa. Girman da gudun ruwan sama yana da mahimmanci. Ruwan ruwan sama mai girma da girma yana da kuzari mai ƙarfi, don haka tasirin su zai kawar da barbashin ƙasa ta nesa mafi girma fiye da ƙarami, mai h sauƙaƙan motsi.
Roslyne Akombe
Rayuwar farko da ilimi
An haife ta a cikin 1976, a gundumar Nyamira ta yau, a cikin lardin Nyanza a lokacin, Kenya. Ta girma ta halarci makarantun firamare da sakandare na cikin gida. Ta sami digiri na farko, Digiri na Ilimi, daga Jami'ar Nairobi.Daga baya, ta sami digiri na biyu na Kimiyya a Harkokin Duniya, daga Jami'ar Rutgers, ta Amurka, sannan ta sami digiri na biyu a fannin Falsafa, a cikin wannan fanni, kuma daga Jami'ar Rutgers.
Aiki
An dauki Akombe a matsayin babban mai ba da shawara ga Mataimakin Sakatare-Janar kan harkokin siyasa a hedikwatar Majalisar Dinkin Duniya da ke birnin New York.
Zaizayar Kasa
Yanayi (Climate)
A wasu yankuna na duniya (misali Yammacin Turai ), kwararar ruwa da zaizayar ƙasa suna haifar da ƙarancin ƙarancin ruwan sama wanda ke fadowa akan ƙasa mai cike da ƙima. A irin wannan yanayi, yawan ruwan sama maimakon tsananin ƙarfi shine babban abin da ke tantance tsananin lalacewar ƙasa taruwa.
Roslyne Akombe
Aikin a IEBC
A watan Janairun 2017, aka nada ta a matsayin kwamishina a hukumar ta IEBC, lamarin da ya bai wa jama’a mamaki lokacin da jama’a suka fahimci cewa za ta rage albashin kashi 70 cikin 100 daga tsohuwar aikinta ta yin aiki da hukumar. Ta bayyana cewa wannan lamari ne na kishin kasa ga kasarta kuma tana da burin taimakawa kasar ta gudanar da sahihin zabe da kuma fatan taka rawa a cikinsa. Kafofin yada labarai sun kuma bayar da rahoton cewa, "An ba ta hutu na musamman ba tare da albashi ba don yin aiki a hukumar zabe mai zaman kanta ta Kenya," kuma "za ta ba da goyon baya na fasaha ga hukumar a shirye-shiryen zaben 2017 da kuma goyon bayan kokarin hanawa. rikicin bayan zabe a Kenya." Ta yi aiki tare da IEBC Akombe ba zata karɓi kowane albashi a matsayin ma'aikacin Majalisar Dinkin Duniya.Matsakaicin albashin Akombe a matsayinsa na kwamishinan IEBC an kiyasta shi akan KES 800,000 (kimanin dalar Amurka 8000) a wata.
Zaizayar Kasa
Yanayi (Climate)
A kasarTaiwan, inda yawan guguwa ta ƙaru sosai a cikin ƙarni na 21, an sami haɗin haɗin gwiwa tsakanin ƙaruwar yawan guguwa tare da ƙaruwar ɗimbin laka a cikin koguna da madatsun ruwa, wanda ke nuna tasirin canjin yanayi na iya haifar da rushewar ƙasa.
Ciyayi/Tsirran wuri
Tsirrai suna aiki azaman abin dubawa tsakanin yanayi da ƙasa. Yana qara permeability na ƙasa zuwa tara ruwan sama, haka ragewa dake kwarara. Yana ba da kariya ga ƙasa daga iska, wanda ke haifar da raguwar gurɓataccen iska, gami da canje -canje masu fa'ida a cikin microclimate. Tushen shuke -shuke suna ɗaure ƙasa tare, kuma suna yin hulɗa da wasu tushen, suna samar da ƙarin ƙarfi wanda ba shi da saukin kamuwa da ruwa da zaizayar iska. Cire ciyayi yana ƙaruwa da yawan yashewar ƙasa.
Roslyne Akombe
Aikin a IEBC
Bayan aikinta a IEBC, nan take Roselyn ta zama fuskar hukumar, kuma ta halarci taron manema labarai da yawa da aka baiwa jama'a. Hasali ma, ita ce ke da alhakin fitar da da yawa daga cikin wadannan tarukan manema labarai, inda ake ganin ta a matsayin mai iya magana da santsi. Hakan ya sa mutane da yawa suke ganin ita ce mataimakiyar shugabar hukumar, duk da cewa ita kwamishina ce kawai. A cewar jaridar Daily Nation ta Kenya, Akombe "wata matasa ce, mai magana da kai tsaye kuma kwamishina mara kunya tare da manyan kunci wanda ya bayyana abubuwa da murmushi." Ayyukanta a hukumar sun hada da horas da jami'ai, yin jawabi ga taron manema labarai, bayar da rahoto ga shugaba da babban jami'in hukumar da kuma daukar wasu ayyuka don tabbatar da gaskiya da adalci a zaben Kenya.
Rigimar murabus
A ranar 18 ga watan Oktoban 2017, Akombe ta yi murabus daga mukaminta na kwamishiniyar hukumar ta IEBC a lokacin da kasar ke cikin rikici bayan da kotun koli ta soke zaben Kenya na 2017. A ranar 1 ga Satumba, 2017, Kotun Koli ta Kenya ta yanke hukuncin da ta bayyana sakamakon zaben shugaban kasa na ranar 8 ga watan Agustan 2017. Kotun ta ce hukumar ta IEBC ta gaza cika sharuddan da kundin tsarin mulkin kasar ya gindaya na gudanar da sahihin zabe tare da bayar da umarnin sake gudanar da zaben cikin kwanaki 60. Sakamakon haka, IEBC ta shirya gudanar da sabon zabe tare da sanar da sabon ranar zabe a matsayin ranar 17 ga Oktoba, 2017, sannan ta tura shi zuwa 26 ga Oktoba 2017. Sai dai jam'iyyar adawa ta National Super Alliance (NASA), karkashin jagorancin Raila Amolo Odinga ta yi tur da matsin lamba kan hukumar, tana mai cewa ba za ta iya gudanar da zabe kamar yadda aka tsara a halin yanzu ba. Wannan ra'ayi ya samu goyon bayan dukkanin 'yan siyasa masu alaka da dan takarar NASA, Raila Amolo Odinga, ciki har da abokin takararsa Kalonzo Musyoka. Hasali ma, hakan ya kai ga kauracewa zaman da daukacin ‘yan majalisar dokoki da na majalisar dattawa suka yi tare da cewa ba su amince da shugaba Uhuru Kenyatta a matsayin zababben shugaban kasa ba. Sai dai kuma, Uhuru Kenyatta da dukkan 'yan siyasa masu alaka da jam'iyyarsa ta Jubilee Party sun yi adawa da wannan ra'ayi, suna masu cewa Raila ba shi da hurumin jagorantar IEBC kan ayyukanta. Bambancin da ke tsakanin wadannan jiga-jigan biyu ya haifar da abin da wasu ke kira da rikicin siyasa a Kenya.
Zaizayar Kasa
Bisan Kasa
Tsarin yanayin bisan ƙasa yana ƙayyade saurin da ruwan saman zai gudana, wanda hakan ke ƙayyade lalatawar kwararar ruwan. Doguwa, gangaren tudu (musamman waɗanda ba su da isasshen murfin ciyayi) sun fi saukin kamuwa da zaizayar ƙasa a lokacin ruwan sama fiye da gajarta, ƙasa da tudu. Har ila yau, tudu mai tsauri ya fi saurin kamuwa da zaftarewar ƙasa, zaftarewar ƙasa, da sauran hanyoyin tafiyar da yaƙi.
Roslyne Akombe
Rigimar murabus
Kokarin ci gaba da kasancewa tsaka mai wuya, IEBC ta yi kokarin gudanar da tarurruka tsakanin 'yan adawa da gwamnati ba tare da cimma wata nasara ba. A kwanakin da suka biyo bayan hukuncin kotun, Raila da jam'iyyarsa ta NASA sukan bayar da wa'adi, wanda ta kira a matsayin mafi karanci da ba za a iya ragewa ba idan ba tare da wanda ba za a iya gudanar da sahihin zabe a Kenya ba. Yayin da IEBC ta fito yana cewa ba za ta iya cika wadannan ka’idoji ba, Raila Odinga ya bai wa kasar da al’ummar duniya mamaki da cewa ya janye daga takarar shugabancin kasar da aka maimaita saboda hukumar ba ta da ikon bai wa ‘yan kasar Kenya zabe mai inganci da gaskiya. Wannan ya haifar da rikicin siyasa a Kenya yayin da Raila da jam'iyyarsa suka tayar da hankali na soke zaben da aka yi a ranar 26 ga Oktoban 2017, yayin da Uhuru da jam'iyyarsa suka matsa kaimi a sake zaben. Dangane da wannan rugujewar siyasar da aka yi, ya bayyana cewa ’yan iska da ma’aikata daga jam’iyyar Jubilee Party da NASA ne suka kutsa cikin hukumar kuma an yi mata magudi.
Zaizayar Kasa
Tectonics
Hanyoyin Tectonics suna sarrafa ƙima da rarrabuwa na zaizayar ƙasa. Idan aikin tectonic ya haifar da wani ɓangaren farfajiyar Duniya (misali, tsaunin tsaunuka) a ɗaga ko saukar da shi dangane da yankunan da ke kewaye, wannan dole ne ya canza canjin yanayin ƙasa. Saboda yawan zaizayar ƙasa kusan koyaushe yana kula da gangaren gida (duba sama), wannan zai canza adadin lalacewar a yankin da aka ɗaga. Tectonics masu aiki kuma suna kawo sabo, dutsen da ba a gama juyawa zuwa farfajiya ba, inda aka fallasa shi ga aikin lalata.
Koyaya, zaizayar ƙasa na iya shafar al'amurran tectonic. Cirewa ta hanyar zaizayar dutsen mai yawa daga wani yanki, da kuma ajiye shi a wani wuri, na iya haifar da sauƙaƙe nauyi akan ƙananan ɓawon burodi da mayafi. Saboda matakan tectonic suna motsawa ta hanyar gradients a cikin filin damuwa da aka haɓaka a cikin ɓawon burodi, wannan saukarwa na iya haifar da haɓaka tectonic ko isostatic a yankin. A wasu lokuta, an yi hasashen cewa waɗannan bayanan tagwayen na iya yin aiki don keɓancewa da haɓaka yankuna na saurin hakowa na manyan duwatsu masu zurfi a ƙarƙashin wurare a saman duniyar tare da hauhawar hauhawar yanayi, alal misali, ƙarƙashin ƙasa mai zurfi na Nanga Parbat. a yammacin Himalayas. An kira irin wannan wurin " tectonic aneurysm ".
Roslyne Akombe
Rigimar murabus
A ranar 18 ga Oktoba 2017, Akombe ta tabbatar da wannan jita-jita lokacin da ta yi murabus a cikin takardar murabus din ta da aka buga a yanar gizo.
Tasiri kan maimaita zaben shugaban kasar Kenya na 2017
Murabus din da Kwamishinan ya yi ya jawo hankulan kafafen yada labarai. An ci gaba da sabon zaben duk da cewa Raila Odinga daya daga cikin manyan 'yan takara ya janye daga zaben kuma ya bukaci magoya bayansa da kada su shiga kada kuri'a. An ayyana Uhuru Kenyatta a matsayin shugaban kasa tare da rantsar da shi, kuma ‘yan sanda sun kashe masu zanga-zangar a wurare daban-daban na kasar.
Zaizayar Kasa
Ci gaba
Ci gaban ɗan adam, a cikin sifofi ciki har da bunƙasa aikin gona da birane, ana ɗaukarsa muhimmiyar rawa a cikin yaƙar ƙasa da safarar ɗimbin abinci, wanda hakan ke ƙara haifar da karancin abinci. A cikin Taiwan, ana iya samun ɗimbin ɗimbin ramuka a arewacin, tsakiya, da kudancin tsibirin tare da tsarin ci gaban kowane yanki a cikin karni na 20. Da gangan mutane suka cire ƙasa da dutsen wani nau'in ɓarna ne wanda aka sanya wa suna lisasion.
A matakin tsaunuka
An san cewa tsaunukan suna ɗaukar miliyoyin shekaru kafin su lalace har zuwa matakin da suka daina wanzuwa. Masana Pitman da Golovchenko sun ƙiyasta cewa wataƙila yana ɗaukar fiye da shekaru miliyan 450 don lalata dutsen da ya yi kama da Himalaya a cikin ɗan ƙaramin falo idan babu manyan canje-canjen matakin teku. Rushewar tarin duwatsun zai iya haifar da ƙirar babban taro daidai gwargwado da ake kira daidaiton taro. An yi jayayya cewa tsawaita lokacin rushewar orogenic shine mafi inganci hanyar rage tsayin tsaunukan orogenic fiye da zaizayar ƙasa.
Misalan zaizayar tsaunuka da aka lalata sun haɗa da Timanides na Arewacin Rasha. Rushewar wannan ogen ya samar da gurɓataccen ruwa wanda yanzu ake samu a Dandalin Gabashin Turai, gami da Tsarin Sablya na Cambrian kusa da Tafkin Ladoga. Nazarin waɗannan lamuran sun nuna cewa mai yiwuwa yuwuwar ɓarkewar ogen ya fara a cikin Cambrian sannan ya ƙaru a cikin Ordovician.
Ƙasa
Idan yawan zaizayar ƙasa ya yi yawa fiye da ƙimar ƙasa, ana lalata ƙasa. Inda ba a lalata ƙasa ta hanyar zaizayar ƙasa, zaizayar ƙasa a wasu lokuta na iya hana samuwar fasalulluka ƙasa waɗanda ke yin sannu a hankali. Inceptisols ƙasa ce ta yau da kullun da ke samuwa a cikin wuraren da ake lalata da sauri.
Yayin da yashewar ƙasa tsari ne na halitta, ayyukan ɗan adam sun ƙaru da sau 10-40 ƙimar da zaizayar ƙasa ke faruwa a duniya. Yawan zaizayar ƙasa (ko hanzarta) zai haifar da matsalolin “a-site” da “off-site”. Tasirin yanar-gizon ya haɗa da raguwar yawan amfanin gona da (a kan shimfidar wurare na halitta ) rushewar muhalli, duka saboda asarar raƙuman ƙasa mai wadataccen abinci mai gina jiki. A wasu lokuta, sakamakon ƙarshe shine kwararowar hamada. Kashe-site effects hada sedimentation na waterways da eutrophication na ruwa jikinsu, kazalika da laka-related lalacewar hanyoyi da kuma gidaje. Raguwar ruwa da iska sune manyan abubuwan da ke haifar da lalacewar ƙasa ; a hade, su ke da alhakin kusan kashi 84% na yawan ƙasashen duniya na ƙasƙantar da ƙasa, suna mai da yaƙar wuce gona da iri ɗaya daga cikin mahimman matsalolin muhalli.
A kasar Amurka, manoma da ke noma ƙasa mai iya ɓarna dole ne su bi tsarin kiyayewa don samun cancantar wasu nau'ikan taimakon aikin gona.
1979
1979 ita ce shekara ta dubu ɗaya da ɗari tara da saba'in da tara a ƙirgar Miladiyya.
Ronaldo (Brazil)
Ronaldo Luís Nazário de Lima (an haife shi ne a ranar 18 ga watan Satumba a shekara ta 1976), an fi saninsa da Ronaldo, tsohon ɗan wasan kwallon kafa ne na kasar Brazil, wanda ke buga bangaren gaba (striker). Popularly dubbed O Fenômeno ("The Phenomenon"), ana ganinsa a matsayin daya daga cikin shahararrun yan wasa na duniyagreatest football players of all time. In his prime, he was know his dribbling at speed, feints, and clinical finishing. At his in(1990) Ronstarre Dan kwallon gabane a kungiyar Real Madrid Cruzeiro, PSV, Barcelona, da Inter Milan. Komawarsa zuwa Spain da Italy yasa ya zama na biyu bayan DMaradona wajen kafa tarihi to break the world transfer record twice, all before his 21,st birthday. Da kaiwarsa shekaru 23, yaci kwallaye sama da 200 ,wa kulub dinsa da kasarsa. Bayan share fiye da shekara uku batare da taka leda ba, saboda ciwon gwiwa da yake fama dashi , Ronaldo yakoma Real Madrid a shekarar 2002, daga baya ya kungiyar A.C. Milan daga bisani kungiyar Corinthians sannan daga karshe ya ajiye kwallo a shekara ta 2011, baya yasha fama da raunuka.
Ronaldo yayi nasarar lashe gwarzon ɗan wasa na duniya wato FIFA World Player of the Year a cikin shekara ta 1996, zuwa 1997 da 2002, sannan da Ballon d'Or a cikin shekara ta 1997 zuwa  2002, dakuma  UEFA Club Footballer of the Year a cikin shekara ta 1998, kuma shine  Gwarzon ɗan wasa a gasar La Liga a shekara ta 1997,ya lashe European Golden Bo Bayan yaci kwallaye 34, kwallaye acikin laliga,sannankuma yalashe Serie A Footballer of the Year acikin shekara ta 1998. Yana daya daga cikin Yan kallon masu fada aji, shine na farko don lasheNike Mercurial Yayi da aka kaddamar da takalmi R9. Pele ya sanya shi acikin jerin rayayyun 'yan wasa 100 na musamman na FIFA a cikin shekara ta 2004, kuma an adana ta a gidan tarihin shahararrun 'yan wasa na Brazil wato Brazilian Football Museum Hall of Fame da kuma Gidan tunawa da shaharru na kasar Italiya.
Ronaldo ya buga wa kasar Brazil wasanni guda 98, ya zura kwallaye 62, kuma shine dan wasa na biyu da suka fi kowa zura kwallaye wa kasar ta Brazil, inda yake bin bayan Pelé.
Taapsee Pannu
Taapsee Pannu (an haife ta a ranar 1 ga watan Agustan shekarar 1987) jarumar fim ɗin Indiya ce wacce yawancin fina-finanta sun kasance na harsunan Hindi, Telugu da kuma Tamil ne. Ta karɓi kambun Filmfare Awards har sau biyu kuma mujallar Forbes India ' ta sanya ta a jerin fitattun jarumai mata 100 a shekarar 2018.
Kuruciya
Taapsee Pannu dai an haife ta a ranar 1 ga Agustan shekarar 1987 ne a New Delhi. Ta kasance 'ya ga Dilmohan Singh Pannu da kuma Nirmaljeet. Ita 'yar asalin Punjabi ce. kafin mahaifinta yayi ritaya dillalin gidaje ne yayin da mahaifiyarta kuma ta kasance mai aikin kulawa da gida. Tana da kanwa mai suna Shagun. Ta yi karatunta a makarantar Mata Jai Kaur dake Ashok Vihar sannan ta kammala karatunta na zama Injiniyar Kwamfuta daga Guru Tegh Bahadur Institute of Technology.
Aiki/Sana'a
Bayan kammala karatunta, Pannu ta kama aikin injiniyar software. Daga bisa ni kuma ta zama cikakkiyar 'yar kwalliya bayan da ta aka zabe ta don nuna gwaninta a shirin Get Gorgeous na tashar Channel V, wanda a ƙarshe ya kai ta fadawa harkar wasan kwaikwayo. Pannu ta fito cikin tallace-tallace da yawa na ɗab'i da hotunan talabijin kuma ta sami lambobi da yawa a kwanakin da ta yi na kasancewarta 'yar kwalliya, ciki har da "Pantaloons Femina Miss Fresh Face" da "Safi Femina Miss Beautiful Skin" a gasar Femina Miss India ta 2008.
2019 – present: ƙarin nasara
Pannu ya featured in Forbes India 's jerin Celebrity 100 a shekara ta 2018 a 67th matsayi da wani kimanta kudin shiga na ₹ 15.48 crore. An sake nuna ta a karo na biyu a cikin shekarata 2019 a matsayi na 68th. A cikin shekarar 2017, an saka ta a cikin jerin mujallu na 30 Under 30. Pannu tana gudanar da wani kamfani mai kula da taron da ake kira The Wedding Factory wanda take gudanarwa tare da yar uwarta Shagun da kuma aboki Farah Parvaresh. A cikin shekarata 2018, ta sayi ikon mallakar badminton Pune 7 Aces wanda ke taka leda a Premier Badminton Wasanni.
Masarautar Yauri
Yauri (ko Yawuri) masarauta ce a jihar Kebbi, Najeriya, ta mamaye ƙaramar hukumar Yauri. A yau, Yauri na ɗaya daga cikin mafi ƙanƙanta masarautu na tarihi a Arewacin Najeriya. A cikin shekara ta 1972, yawan jama'a kusan mutane dubu 112,000 ne ke zaune a wani yanki mai faɗin murabba'in 1306 sqmi  kuma ya rarrabu sama da manyan gundumomi shida.
Right to sexuality
Ma'ana
Batun 'yancin yin jima'i yana da wahalar bayyanawa, domin kuwa ya kunshi hakkoki da dama daga cikin dokokin kare hakkin dan adam na duniya.