地理记忆顺口溜.pdf
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1、地理记忆顺口溜1、九大行星水金地火木土天,海王冥王绕外边;唯有地球生物现,温气液水是由缘。温,适宜的温度。气,适宜生物呼吸的大气。2、地球特点赤道略略鼓,两极稍稍扁。自西向东转,时间始变迁。南北为纬线,相对成等圈。东西为经线,独成平行圈;赤道为最长,两极化为点。3、东西南北半球的划分西经二十度,东经一百六,一刀切下去,东西两半球。南北半球分,赤道零纬度,四季温带显,南北相反出。4、昼夜交替和四季变化地球自转,昼夜更换。绕日公转,四季出现。自转一日,公转一年。自西向东,方向不变。5、地球五带地球有五带,全靠四线分;回归间热带,极圈分寒温;寒温各有二,五带温不均。温,指温度。6、地图辨方向地图方向
2、辨,摆正放眼前;上北下为南,左西右东边。标图易分辨,经纬网较难;纬线指南北,东西经线圈。极地投影图,定向较特殊:对于北半球,心北四周南;北纬圈东西,自转反时走。对于南半球,心南北四周;南纬圈东西,自转顺时走。7、大洲和大洋地球表面积,总共五亿一;水陆百分比,海洋占七一。陆地六大块,含岛分七洲;亚非南北美,南极大洋欧。水域四大洋,太平最深广;大西“S”样,印度北冰洋。板块构造学,六块来拼合;块内较稳定,交界地震多。8、大洋和大洲的位置洋以洲为界,洲以洋分野。太平洋为四洋首,位于亚澳两美间。大西洋西南北美,东岸临界欧与非。印度洋临亚非澳,南部三洋水相连。北冰洋面为最小,亚欧北美三洲环。9、七大洲分
3、界和位置地表十分陆占三,亚欧非洋两美南。亚欧两洲本一体,乌拉高加分两边;亚非原本相结连,苏伊运河来割断;亚洲北美隔水望,白令海峡在中间;中美南北来牵线,巴拿运河又阻拦;数大洋洲面积小,似断不断亚下边。亚欧非洋东半球,南北美占西半边,唯有南极搞独立,冰层覆盖称高原。洋,大洋洲。两美,南美洲和北美洲。南,南极洲。乌拉,乌拉尔山脉和乌拉尔河。高加,高加索山脉。苏伊运河,苏伊士运河。巴拿运河,巴拿马运河。10、七大洲地形(1)亚洲亚洲地形杂,中高四周洼。冲积平原广,山地高原大。江河放射流,水资源可夸。(2)欧洲半岛缘海多,形体分节肢;山地居南北,中部平原低;地形平原主,海拔倒第一。(3)北美洲东部高原
4、联山地,西部山地接高原。东西相间高大陆,世称湖海在其间。(4)南美洲安第斯山雄踞西,东部平原高原区。文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9
5、U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码
6、:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4
7、G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E
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9、6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3
10、S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1地形多为世界最,高原平原列首位。西部山脉为最长,亚马逊河流域广。热带
11、雨林居世首,草原要数潘帕斯。(5)非洲平均海拔六百米,号称大陆高原洲,东部高原连一体,西部沙漠平原有。(6)大洋洲面积小,分两区,一大陆,二岛屿。大陆东西高,中部是盆地。(7)南极洲四周环三洋,多年冰雪积;超过二千米,海拔数第一。11、海底地形浅海大陆架,外缘大陆坡;洋盆海沟岭,洋底不可测。12、地形变化地形变化,内外力加。沧海桑田,内部力大;板块运动,拉伸挤压,断层褶皱,出现高洼;火山地震,板块缘发。外部力量,不可轻它;风浪水冰,侵蚀变化,天长日久,削高填洼。13、天气和气候天气:短时阴晴雨雪冷热风气候:多年平均春夏和秋冬14、气温分布规律气温分布有差异,低纬高来高纬低;陆地海洋不一样,夏陆
12、温高海温低,地势高低也影响,每千米相差6。15、地球变暖危害大气污染,地球变暖;冰川融化,沿海被淹。采取措施,刻不容缓。16、风的形成温高气上升,低压下形成;文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G
13、8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7
14、 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6
15、V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S
16、5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X
17、1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U
18、1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1气自高压来
19、,流动形成风。17、地球气压带高气压带四,低气压带三:南北五度间,高温气上翻,赤道低气压,降水造方便;南北三十度,气流下偏转,副热高气压,少雨常干旱;极地气压低,靠近两极点;南北六十度,副极低压然。18、地球风带气压带相隔,风带共有六:信风赤道搂,东风两极出,南北西风带,四十、六十度11 楼19、降水形成条件空汽饱,气温降;凝结核,相碰撞;体重加,雨雪降。20、降水分布规律赤道热,降水多:两极寒,降水难。回归线,分西边;陆西岸,副高带,信风吹,降水亏;陆东岸,季风故,气候温,降水富。中纬度,居内部;距海远,气候干。21、影响气候的因素影响气候因素,四个方面兼顾;纬度位置第一,赤道两极悬殊;其次
20、要看海陆,远海夏季干酷;地形也很重要,高寒背风雨勿;洋流不可低估,暖流到来水富22、陆地自然带分布与特征地表气候不一般,植被动物随着变。九自然带分布谈,热温类型各有三;亚寒苔原冰原带,另外高山垂直变。文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 Z
21、X5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3
22、V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档
23、编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6
24、D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A1
25、0E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV8I6V10G3S5 ZX5X1P3V9U1文档编码:CK6D4G8A10E7 HV
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