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永靖縣吧咪山景區怎么樣

吧咪(mi)(mi)山(shan)(shan)位于甘肅省中部，地(di)處(chu)臨(lin)(lin)夏回(hui)族自治州所屬(shu)永(yong)靖、東(dong)鄉(xiang)(xiang)族自治縣(xian)和定西地(di)區所屬(shu)臨(lin)(lin)洮(tao)縣(xian)交界處(chu)，主峰(feng)在今永(yong)靖縣(xian)三(san)(san)條(tiao)峴(xian)(xian)鄉(xiang)(xiang)塔(ta)什堡境(jing)內。洮(tao)河由唐(tang)汪川(chuan)入(ru)茅隴(long)峽，繞(rao)吧咪(mi)(mi)山(shan)(shan)南(nan)麓西行(xing)，在茅隴(long)峽口的鸚鴿嘴(zui)匯入(ru)黃河，入(ru)劉家(jia)(jia)峽水庫。吧咪(mi)(mi)山(shan)(shan)與(yu)(yu)洮(tao)河形成(cheng)山(shan)(shan)環(huan)水繞(rao)之勢。吧咪(mi)(mi)山(shan)(shan)正處(chu)于兩河匯流(liu)、雙峽交峙(zhi)的三(san)(san)角(jiao)地(di)帶。吧咪(mi)(mi)山(shan)(shan)區域(yu)南(nan)瀕洮(tao)河與(yu)(yu)東(dong)鄉(xiang)(xiang)族自治縣(xian)唐(tang)汪、董嶺鄉(xiang)(xiang)隔水相望(wang)；北至前(qian)霧宿山(shan)(shan)柳(liu)(liu)木夾峴(xian)(xian)(海拔2500米)為(wei)界與(yu)(yu)本(ben)縣(xian)陳井鎮(zhen)張家(jia)(jia)溝村、年(nian)家(jia)(jia)灣村、陳井村為(wei)鄰；東(dong)至格水嶺(又(you)名官水嶺)、八面臺與(yu)(yu)徐(xu)頂(ding)鄉(xiang)(xiang)久長溝村和臨(lin)(lin)洮(tao)縣(xian)紅旗鄉(xiang)(xiang)扎馬圈村接壤；西依(yi)荀子溝嶺、深峴(xian)(xian)子、大峴(xian)(xian)子與(yu)(yu)劉家(jia)(jia)峽鎮(zhen)紅柳(liu)(liu)村和三(san)(san)條(tiao)峴(xian)(xian)鄉(xiang)(xiang)紅峴(xian)(xian)子村、三(san)(san)條(tiao)峴(xian)(xian)村相毗鄰。區域(yu)南(nan)北長約14公(gong)里(li)，東(dong)西寬約11公(gong)里(li)，總(zong)土地(di)面積為(wei)84.36平(ping)方公(gong)里(li)。另外，加(jia)上吧咪(mi)(mi)山(shan)(shan)東(dong)延余(yu)脈臨(lin)(lin)洮(tao)縣(xian)境(jing)地(di)約2平(ping)方公(gong)里(li)，構成(cheng)較為(wei)完整的吧咪(mi)(mi)山(shan)(shan)景區全貌，總(zong)面積86.36平(ping)方公(gong)里(li)。

景點景觀

吧咪山內(nei)有金(jin)花菩薩大殿,前殿、水晶宮(gong)、山神廟(miao)、土地廟(miao)、百子宮(gong)、龍王(wang)宮(gong)、灶王(wang)殿、鐘樓(lou)、鼓樓(lou)等古典(dian)建(jian)筑群,亭(ting)臺樓(lou)閣,金(jin)碧輝煌(huang)。吧咪山山巒起伏,奇(qi)峰競秀(xiu),怪石嶂峋,峭(qiao)巖絕(jue)壁,似物(wu)象形(xing)者枚不勝數，還(huan)有洶涌澎湃(pai)的(de)洮河水一瀉千(qian)里，形(xing)成了獨特(te)的(de)自然景觀。

地理環境

地理位置

吧(ba)咪(mi)(mi)山(shan)(shan)位于(yu)甘肅省中部，地(di)(di)處臨(lin)(lin)夏(xia)回族自治(zhi)州(zhou)(zhou)(zhou)所屬永(yong)靖、東鄉(xiang)(xiang)族自治(zhi)縣(xian)(xian)和定西(xi)地(di)(di)區所屬臨(lin)(lin)洮縣(xian)(xian)交界處，主峰(feng)在今永(yong)靖縣(xian)(xian)三(san)條峴鄉(xiang)(xiang)塔(ta)什(shen)堡境內。另外，加上吧(ba)咪(mi)(mi)山(shan)(shan)東延余脈臨(lin)(lin)洮縣(xian)(xian)境地(di)(di)約2平方(fang)公(gong)里(li)(li)，構成較為完整的吧(ba)咪(mi)(mi)山(shan)(shan)景區全貌，總面(mian)積86.36平方(fang)公(gong)里(li)(li)。地(di)(di)理坐(zuo)標介于(yu)東經103°25′～103°30 ′，北緯35°53 ′～36°01′之間(jian)，主峰(feng)海拔2660.4米。吧(ba)咪(mi)(mi)山(shan)(shan)主峰(feng)西(xi)距永(yong)靖縣(xian)(xian)城劉家峽(xia)鎮12公(gong)里(li)(li)，至臨(lin)(lin)夏(xia)州(zhou)(zhou)(zhou)府91公(gong)里(li)(li)；赴省會蘭(lan)州(zhou)(zhou)(zhou)有兩條道路(lu)：一條經縣(xian)(xian)城達蘭(lan)州(zhou)(zhou)(zhou)85公(gong)里(li)(li)，另一條由沿東北林(lin)區三(san)級道路(lu)接309、213線(xian)國道達蘭(lan)州(zhou)(zhou)(zhou)45公(gong)里(li)(li)。

地質地貌

吧(ba)(ba)(ba)咪(mi)(mi)(mi)山(shan)石(shi)質(zhi)山(shan)地(di)(di)(di)(di)(di)(di)由(you)古(gu)老的(de)(de)前震(zhen)旦系變(bian)質(zhi)巖和(he)(he)(he)(he)早古(gu)生(sheng)(sheng)(sheng)代(dai)(dai)侵(qin)入(ru)的(de)(de)加里東期花崗巖所(suo)組(zu)成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)。前者分(fen)布在(zai)(zai)(zai)洮河(he)口茅隴(long)峽兩岸(an)，并延(yan)伸(shen)到劉(liu)家峽及(ji)其水庫(ku)大壩一帶(dai)；后(hou)者分(fen)布在(zai)(zai)(zai)青和(he)(he)(he)(he)下溝口——吧(ba)(ba)(ba)咪(mi)(mi)(mi)山(shan)頂——房子溝一帶(dai)，成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)為(wei)(wei)吧(ba)(ba)(ba)咪(mi)(mi)(mi)山(shan)的(de)(de)主體。由(you)于(yu)(yu)祁連山(shan)長期處(chu)(chu)于(yu)(yu)隆起狀態(tai)，歷經古(gu)生(sheng)(sheng)(sheng)代(dai)(dai)風化剝蝕；中(zhong)生(sheng)(sheng)(sheng)代(dai)(dai)后(hou)，又受到燕山(shan)地(di)(di)(di)(di)(di)(di)質(zhi)運動(dong)的(de)(de)影響，吧(ba)(ba)(ba)咪(mi)(mi)(mi)山(shan)及(ji)其周(zhou)圍(wei)廣(guang)大地(di)(di)(di)(di)(di)(di)區形(xing)(xing)成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)斷陷盆(pen)地(di)(di)(di)(di)(di)(di)，在(zai)(zai)(zai)盆(pen)地(di)(di)(di)(di)(di)(di)內(nei)形(xing)(xing)成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)巨厚的(de)(de)中(zhong)新(xin)生(sheng)(sheng)(sheng)代(dai)(dai)內(nei)陸紅色湖盆(pen)沉積(ji)。吧(ba)(ba)(ba)咪(mi)(mi)(mi)山(shan)之北麓的(de)(de)青和(he)(he)(he)(he)盆(pen)地(di)(di)(di)(di)(di)(di)中(zhong)所(suo)沉積(ji)的(de)(de)就是中(zhong)生(sheng)(sheng)(sheng)代(dai)(dai)白堊系紫紅色地(di)(di)(di)(di)(di)(di)層(ceng)(ceng)，西邊的(de)(de)紅峴(xian)子及(ji)黃(huang)(huang)河(he)兩岸(an)沉積(ji)的(de)(de)是新(xin)第(di)三系橘(ju)紅色地(di)(di)(di)(di)(di)(di)層(ceng)(ceng)。由(you)于(yu)(yu)當時氣候(hou)炎熱干燥，形(xing)(xing)成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)區域(yu)內(nei)嚴(yan)重干旱缺(que)水。進入(ru)新(xin)生(sheng)(sheng)(sheng)代(dai)(dai)后(hou)，到上新(xin)世隴(long)山(shan)運動(dong)強烈上升(sheng)，同時伴(ban)生(sheng)(sheng)(sheng)汾(fen)河(he)期侵(qin)蝕，使盆(pen)地(di)(di)(di)(di)(di)(di)、山(shan)地(di)(di)(di)(di)(di)(di)均遭到切割(ge)，區域(yu)地(di)(di)(di)(di)(di)(di)形(xing)(xing)地(di)(di)(di)(di)(di)(di)貌復雜化，成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)為(wei)(wei)第(di)四(si)紀(ji)沉積(ji)物各種(zhong)各樣停積(ji)場，沉積(ji)了(le)河(he)谷及(ji)溝谷地(di)(di)(di)(di)(di)(di)帶(dai)的(de)(de)礫石(shi)層(ceng)(ceng)和(he)(he)(he)(he)丘陵區的(de)(de)風成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)離石(shi)黃(huang)(huang)土(老黃(huang)(huang)土)，形(xing)(xing)成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)了(le)中(zhong)更新(xin)世的(de)(de)沉積(ji)物。特別(bie)是到了(le)第(di)四(si)紀(ji)晚更新(xin)世迎(ying)來了(le)風成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)馬蘭黃(huang)(huang)土(新(xin)黃(huang)(huang)土)，廣(guang)泛覆蓋于(yu)(yu)原(yuan)有地(di)(di)(di)(di)(di)(di)層(ceng)(ceng)之上，便(bian)構成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)了(le)黃(huang)(huang)土高(gao)原(yuan)梁峁、丘陵山(shan)地(di)(di)(di)(di)(di)(di)等現狀。吧(ba)(ba)(ba)咪(mi)(mi)(mi)山(shan)區域(yu)的(de)(de)地(di)(di)(di)(di)(di)(di)形(xing)(xing)，由(you)石(shi)質(zhi)山(shan)地(di)(di)(di)(di)(di)(di)和(he)(he)(he)(he)山(shan)間盆(pen)地(di)(di)(di)(di)(di)(di)兩部(bu)分(fen)組(zu)成(cheng)(cheng)(cheng)(cheng)(cheng)(cheng)。南北高(gao)，中(zhong)間低，東西地(di)(di)(di)(di)(di)(di)形(xing)(xing)相對高(gao)。最底處(chu)(chu)為(wei)(wei)洮河(he)岸(an)邊，海拔為(wei)(wei)1719米(mi)；最高(gao)處(chu)(chu)為(wei)(wei)吧(ba)(ba)(ba)咪(mi)(mi)(mi)山(shan)頂，海拔2660.4米(mi)。吧(ba)(ba)(ba)咪(mi)(mi)(mi)山(shan)與前霧宿山(shan)南北對峙，相距(ju)10余公里。中(zhong)間為(wei)(wei)青和(he)(he)(he)(he)盆(pen)地(di)(di)(di)(di)(di)(di)，海拔高(gao)度(du)在(zai)(zai)(zai)1900---,2400米(mi)之間。地(di)(di)(di)(di)(di)(di)貌類型可劃分(fen)為(wei)(wei)石(shi)質(zhi)中(zhong)高(gao)山(shan)地(di)(di)(di)(di)(di)(di)、黃(huang)(huang)土低山(shan)丘陵、黃(huang)(huang)土梁峁溝谷和(he)(he)(he)(he)河(he)流(liu)灘地(di)(di)(di)(di)(di)(di)四(si)種(zhong)類型。

氣候特征

吧咪山區域(yu)范(fan)圍內屬(shu)溫(wen)帶(dai)半(ban)干旱(han)季(ji)風(feng)氣(qi)候，地處內陸，帶(dai)有大(da)陸性氣(qi)候明顯特征。春(chun)季(ji)干旱(han)多(duo)風(feng)，冬季(ji)寒冷(leng)少雪‘。溫(wen)度適中(zhong)，晝夜溫(wen)差大(da)。降水量少，多(duo)集中(zhong)在(zai)夏秋(qiu)兩季(ji)；雨熱同季(ji)，．蒸發量大(da)，常有干旱(han)發生(sheng)。日照充足，無霜期短。

吧咪山的傳說

傳說，在明洪武(wu)二十二年(nian)，蘭州井兒(er)街有(you)個(ge)(ge)姑娘名叫金花，她(ta)(ta)端莊聰慧，四歲(sui)的(de)時候就(jiu)開始捻麻紡線(xian)，到了(le)該婚嫁(jia)(jia)的(de)年(nian)紀，父母把她(ta)(ta)許配(pei)給(gei)一個(ge)(ge)富豪人家的(de)子弟，金花執意不(bu)去，為(wei)逃避“父母之命，媒(mei)妁(shuo)之言”，臨出嫁(jia)(jia)前，她(ta)(ta)獨自走(zou)出家門，手拿了(le)根燒飯的(de)火(huo)棍(gun)，跑到了(le)吧(ba)咪山，喘息之間(jian)(jian)，便將(jiang)火(huo)棍(gun)插于石(shi)縫間(jian)(jian)，自己在一個(ge)(ge)山洞里(li)絕食靜坐，念念發誓永(yong)不(bu)嫁(jia)(jia)人，一心修行(xing)，達到成(cheng)佛的(de)目的(de)。金花反對包(bao)辦婚姻的(de)精神感(gan)動了(le)山神土地，頓時火(huo)棍(gun)在瞬間(jian)(jian)生枝吐葉，變成(cheng)一棵郁(yu)(yu)郁(yu)(yu)蔥蔥的(de)大(da)松樹(shu)，這棵古樹(shu)被(bei)(bei)人們稱之為(wei)“神樹(shu)”，這個(ge)(ge)地方(fang)因此(ci)也被(bei)(bei)叫做神樹(shu)峴。此(ci)后，人們為(wei)金花蓋廟塑像。每逢(feng)農歷三月(yue)初三、四月(yue)初八(ba)、七月(yue)初七、九(jiu)月(yue)初九(jiu)舉行(xing)盛(sheng)大(da)的(de)民(min)間(jian)(jian)善會(hui)(hui)，遠近的(de)善男信(xin)女就(jiu)會(hui)(hui)從水(shui)旱兩路云(yun)集而來(lai)，頂禮膜拜(bai)。

史料記載

吧(ba)咪(mi)(mi)(mi)山(shan)(shan)原名(ming)黑山(shan)(shan)。其(qi)(qi)來(lai)歷有(you)三種說法：《甘肅古跡(ji)名(ming)勝辭典》載：“傳說清(qing)光(guang)緒(xu)年間(jian)，大(da)旱饑饉，滿山(shan)(shan)忽生吧(ba)糜，味美能食”。百姓賴以度過了(le)荒年，故(gu)稱“吧(ba)咪(mi)(mi)(mi)寶山(shan)(shan)"。《黃河三峽移(yi)民(min)志》記(ji)述，除有(you)此(ci)說外(wai)，另有(you)一說：此(ci)地(di)為(wei)(wei)道教圣(sheng)地(di)，常(chang)常(chang)誦讀“嘛呢吧(ba)咪(mi)(mi)(mi)畔”而得名(ming)。除上述兩種說法外(wai)，尚有(you)子實先(xian)生撰《南北三蓮(lian)花》認為(wei)(wei)，“吧(ba)咪(mi)(mi)(mi)”為(wei)(wei)梵語，意為(wei)(wei)“蓮(lian)花”，比喻心如(ru)蓮(lian)花一樣純潔(jie)無(wu)瑕，或其(qi)(qi)山(shan)(shan)狀如(ru)蓮(lian)花也。