東(dong)太行(xing)(xing)景(jing)區(qu)位于河北(bei)邯鄲武安市境內(nei),因所處太行(xing)(xing)山(shan)東(dong)麓而得名。規(gui)劃總面(mian)積26平方(fang)公里,最高(gao)海(hai)拔1428米,與美國(guo)科(ke)羅拉多大(da)峽谷同屬丹霞地貌(mao)。是一處集(ji)太行(xing)(xing)山(shan)雄、奇(qi)、險(xian)、峻和(he)巧石、云(yun)海(hai)、清幽、變幻(huan)于一體(ti)的山(shan)岳(yue)型(xing)自然景(jing)區(qu)。歷史上著名的129師和(he)許多老一輩革命家曾在這里駐(zhu)扎戰斗(dou)、生(sheng)活。東(dong)太行(xing)(xing)景(jing)區(qu)由中景(jing)信集(ji)團投資(zi)打造,修建(jian)在海(hai)拔千米上的絕(jue)壁玻璃棧道,堪稱太行(xing)(xing)山(shan)人(ren)工奇(qi)觀。漫(man)步棧道,行(xing)(xing)云(yun)繚(liao)繞,猶如踏云(yun)仙境。登臨東(dong)太行(xing)(xing),“天脊(ji)攬勝(sheng),云(yun)端漫(man)步”,人(ren)生(sheng)從此豁然開朗。
東(dong)太行景區內旅(lv)游資源(yuan)豐富(fu),主要以石英砂巖峰林(lin)地(di)貌景觀為(wei)特征(zheng),絕(jue)壁天險,奇石林(lin)立、山(shan)勢磅(bang)礴、雄偉壯觀,山(shan)峰、山(shan)頂巖石形(xing)狀變化萬千,如(ru)動物(wu)(wu)、如(ru)神物(wu)(wu)、如(ru)人物(wu)(wu)等(deng)。
這是11月(yue)20日無人(ren)機拍(pai)攝(she)的武安(an)市東太行景區。河北(bei)省武安(an)市加(jia)速建(jian)設旅(lv)游(you)(you)項目、實施旅(lv)游(you)(you)富民工(gong)程(cheng),基本形成生(sheng)態(tai)游(you)(you)、文化游(you)(you)、紅(hong)色游(you)(you)、鄉村游(you)(you)、休閑康(kang)養游(you)(you)等(deng)多業態(tai)支(zhi)撐的全域旅(lv)游(you)(you)格局。
修建在海拔1000米以(yi)上(shang)(shang)的(de)絕壁上(shang)(shang),蜿(wan)蜒盤旋于山脊之(zhi)上(shang)(shang),神似游龍(long),玻璃棧(zhan)(zhan)(zhan)(zhan)(zhan)道(dao)(dao)、石質(zhi)棧(zhan)(zhan)(zhan)(zhan)(zhan)道(dao)(dao)、觀景臺等一應俱全,建成后將成為(wei)華(hua)北(bei)地區最長的(de)山脊棧(zhan)(zhan)(zhan)(zhan)(zhan)道(dao)(dao)。景區開放(fang)后,游客可登(deng)臨棧(zhan)(zhan)(zhan)(zhan)(zhan)道(dao)(dao),近(jin)距離感受大山的(de)雄壯與秀美(mei)。因地勢高,雨(yu)后乍(zha)晴,常有繚繞的(de)白云沿著(zhu)山谷升起,沿著(zhu)站到綿(mian)延(yan),行走于棧(zhan)(zhan)(zhan)(zhan)(zhan)道(dao)(dao)之(zhi)上(shang)(shang),如踏(ta)云而行,此(ci)時漫步棧(zhan)(zhan)(zhan)(zhan)(zhan)道(dao)(dao),美(mei)哉壯哉,因此(ci)有“云端(duan)棧(zhan)(zhan)(zhan)(zhan)(zhan)道(dao)(dao)”之(zhi)美(mei)譽。
東(dong)太行景區位于河北武安市活水鄉境內,規劃范圍(wei)位于東(dong)經113°52′48.61"—113°55′54.12",北緯36°54′17.03"—36°59′06.12"之間,平均海拔位于600-1480米。東(dong)鄰(lin)古武當、南(nan)靠(kao)京(jing)娘(niang)湖、西觀七步(bu)溝、北聯長(chang)壽村,距離武安市區約40公(gong)里,距離邯(han)鄲市區70公(gong)里,S202省道(dao)毗鄰(lin)而過。
早(zao)在28億(yi)年(nian)前,太(tai)行山(shan)(shan)地(di)(di)(di)區被海水淹(yan)沒(mei),沉積了(le)巨厚的(de)碎(sui)屑巖(yan)(yan)、含鐵硅質(zhi)巖(yan)(yan)及(ji)碳酸鹽地(di)(di)(di)層,受五臺(tai)運(yun)動和呂梁(liang)運(yun)動的(de)影響,區內古老(lao)的(de)地(di)(di)(di)層普(pu)遍遭受褶皺(zhou)、變(bian)質(zhi),并伴隨有斷裂和石英巖(yan)(yan)脈(mo)的(de)侵(qin)入。至距今(jin)18億(yi)年(nian),形(xing)(xing)成了(le)混合巖(yan)(yan)化的(de)結晶基底巖(yan)(yan)層。六億(yi)年(nian)以前,太(tai)行山(shan)(shan)地(di)(di)(di)區仍(reng)是一片汪洋大海,后(hou)來經過了(le)頻(pin)繁(fan)的(de)地(di)(di)(di)殼活動,使太(tai)行山(shan)(shan)脈(mo)逐漸隆起。后(hou)又(you)與東(dong)(dong)(dong)西(xi)的(de)華北大平原斷裂,形(xing)(xing)成太(tai)行東(dong)(dong)(dong)部陡(dou)峭(qiao),西(xi)部徐緩(huan)的(de)地(di)(di)(di)貌形(xing)(xing)態。東(dong)(dong)(dong)太(tai)行因(yin)地(di)(di)(di)處(chu)太(tai)行山(shan)(shan)脈(mo)東(dong)(dong)(dong)麓(lu)而得名,東(dong)(dong)(dong)西(xi)兩側(ce)山(shan)(shan)坡相對平緩(huan),南北陡(dou)峭(qiao),山(shan)(shan)脊由南向北因(yin)勢而起,北側(ce)僧山(shan)(shan)峰(feng)為高(gao)峰(feng),海拔1428.2米(mi),東(dong)(dong)(dong)西(xi)兩側(ce)溪水依山(shan)(shan)而下,呈環抱之(zhi)勢,匯集至京娘湖區。