蚌埠是多民族聚居城市，少数民族中以回族为主，尚有人口数量极少的蒙古族、藏族、维吾尔族、苗族、彝族、布依族、瑶族、白族、畲族。接下来是小编为大家整理的关于蚌埠英语导游词，方便大家阅读与鉴赏!蚌埠英语导
BengbuCityislocatedinthenorthofAnhuiProvince,32°43′nto33°30′n,116°45′eto118°04′e,borderingSuzhouCity,SuixiCounty,LingbicountyandSixianCountyinthenorth,HuainanCityandFengyangCountyinthesouth,MingguangCityandSihongCountyinJiangsuProvinceintheEast,MengchengCountyandFengtaiCountyinthewest,HuainanCityinthesouthwestandSuixiandMengchengCountyinthenorthwest.ThelongestdistancebetweenEastandwestofthecityis32.3km,andthelargestspanbetweenNorthandsouthis23.5km.Jinpurailwayrunsthroughthenorthandsouthfromthemiddleofthearea,andHuaiheRiverflowsfromwesttoEastthroughthesouth.
BengbuCityislocatedinthetransitionzonebetweentheHuangHuaiHaiPlainandtheJiangHuaihillyregion,attheendoftheJiangHuaiwatershed.Theterritoryismainlyplain,withhillsscatteredintheSouth;thegroundtendstothenorthwestandSoutheast,andthenaturalslopeisabout1/10000.MostoftheurbanareaislocatedontheSouthBankoftheHuaiheRiver.Apartfromtheisolatedbengshan(Xiaonanshan)inthecenterofthecity,therearemorethan20mountainsintheEast,Southandwestofthecity.On445.4squarekilometersoflandintheurbanarea,thereare50squarekilometersofhillsand15.3squarekilometersofwater.Thelandformismainlydividedintoplain,hillandplatform.TheplainintheterritoryismainlytheYellowRiverfloodplain,andtherearealsoshallowdepressionplainbetweenrivers,lowterraceofriverswithhillsandbeachlandbesiderivers.Theplatformismainlydistributedinthewavyareatothesouthoftheriver,whichiscomposedofloessofqizuiformation,andcanbedividedintotwotypes:flatandinclined.BengbuhillsaremainlydistributedinthesouthofHuaiheRiver,whichisthenorthernedgeofJianghuaihills.Thebedrockofthehillismostlyexposedafterweatheringanddenudation,andoccasionallythereareresidualslopedeposits,whicharebasicallyundevelopedandcoarsebony.Accordingtothegroundheight,itcanbedividedintohighhillsandlowhills.
Tectonically,BengbusheetislocatedinthecompositepartofthesecondNeocathaysiansubsidencezoneandtheQinlinglatitudinalstructuralzone.ItbelongstothesecondarystructuralunitoftheZhonghuaiRiverplatformdepressionoftheSinoKoreanparaplatform,whichiscalled"Bengbuplatformarch".IthadbeenupliftedobviouslyasearlyastheSinian,andformedalandinthelateCambrian,andhasbeeninthestateofancientlandeversince.Bengbugeologyexperiencedfiveperiodsofrapidtectonicmovement,namelyBengbuperiod,Fengyangperiod,Caledonianperiod,YanshanianperiodandHimalayanperiod.TheHuaihedivisionoftheNorthChinastratigraphicarealacksthemiddleandlatePaleozoic.TheprePaleozoicstrataaredominatedbymetamorphicrocksandmarinestrata,whiletheMesozoicandCenozoicstrataaredominatedbycontinentalandvolcanicrocks.ThestratainBengbucanbedividedintoupperArchean,LowerProterozoic,UpperProterozoic,Qingbaikou,Cambrian,Jurassic,Cretaceous,tertiaryandQuaternary.ThegeologicalstructureandsedimentationofBengbuarecomplex.Foldsformedbymultipletectoniccyclesarewidelyexposed.TheplatformdomeinBengbuareabecomesthenaturalboundaryofHuaibeiandHuainancoalbearingareas.
Bengbuisatransitionalzonebetweenthehumidmonsoonclimateinthenorthsubtropicalzoneandthesemihumidmonsoonclimateinthesouthtemperatezone.Themonsoonissignificant,thefourseasonsaredistinct,theclimateismild,therainfallismoderate,thelightissufficient,andthefrostfreeperiodislong.However,inthemiddlelatitudes,thecoldandwarmairmassactivitiesmeetfrequentlyandchangegreatly.Inaddition,theprecipitationisconcentrated,anddroughtandwaterloggingclimatedisastersoftenoccur,whichhasacertainimpactonagriculturalproduction.BengbuCityisrichinsunshineandsufficientradiationheat,whichcanmeettheneedsoftwocropsayear.Theannualsunshinehoursareestimatedtobe4429.2hoursbytheobservatoryand4440.1hoursinleapyears.However,duetorain,fogandotherfactors,theaverageannualsunshinehoursisonly2167.5hours,andthesunshinerateis49%.Theactualsunshinehoursvarygreatlyfromyeartoyear.Accordingtohistoricalmeteorologicaldata,thesunshinehoursin1956werethemost,reaching2461.5hours;thesunshinehoursin1985weretheleast,only1675.1hours.TheannualandmonthlytemperaturechangesinBengbuhaveacertainperiodiclaw.Theannualaveragetemperatureis15.1℃,whichishigherthanthatinHuaibeiandWanximountainareas.TheannualvariationoftemperatureisthelowestinJanuarywithanaveragetemperatureof1°C,andthehighestinJulywithanaveragetemperatureof28.1℃.Theannualtemperaturedifferenceis27.1℃.