XOXO

		so we are at the crossroads But I can feel my heart open again It's opening for you Just come in, and love me back That's all you have to do I must ask you one small thing Before we kiss and part Please be nice and kind to me I'm tired of broken hearts

XOXO X I N Y I 23o689 speak happyness 2/4 shuling liyi w4tchou7 biwei richard weiling minyu roseline weihong foursevener SJAB fel huihui jjcians lixin jane tommy esther jasmine tzeling qingling roui mayching 06A02 06A02 isabelle germaine yvette jishen 06A03 eunice vithiya archives December 2004 January 2005 February 2005 March 2005 April 2005 May 2005 June 2005 July 2005 August 2005 September 2005 October 2005 November 2005 December 2005 January 2006 February 2006 March 2006 April 2006 May 2006 June 2006 July 2006 August 2006 September 2006 October 2006 November 2006 December 2006 January 2007 February 2007 March 2007 April 2007 May 2007 June 2007 July 2007 August 2007 September 2007 October 2007 November 2007 December 2007 January 2008 February 2008 March 2008 April 2008 May 2008 June 2008 July 2008 August 2008 September 2008 October 2008 November 2008 December 2008 January 2009 February 2009 March 2009 April 2009 May 2009 June 2009 July 2009 August 2009 September 2009 November 2009 January 2010 credits Design: doughnutcrazy		divergent plate mragins aka construtive plate margins. oceanic oceanic plate margins: convection current. magma rise from deep below the earth's surface thru the factures. cools and hardens to form new oceanic crusts. marked by transform faults, run perpendicular to the main ridge. submarine volcanoes. frequent but weak earthquakes. found near mid ocean ridges due to plate movements. continental continental plate margins. rift valleys found nera continential areas in the world. open up new seas. hot spots: region where temp is higher than surrounding areas. may cause to rip into three-arms. convergent plate margins. aka destructive plate margins. three types. type one: oceanic continental convergent plate margin. subduction zone. oceanic crust will sink to the bottom as it's less dense. subduction plate will melt to produce magma and it will rises to the earth suface and cools and form volcanoes. marked by deep ocean trenches, deep focus earthquakes and volcanism. series of earthquakes in the Benoiff zone. stress exerted by subducting plate will cause continental plate to fold or uplifted to form mountains. eg. Andes and Peru Chile trench. type two: oceanic oceanic convergent plate margin. either one will sink. same thing. got subduction zone. marked by deep ocean trenches and island arc formation. descending plate causes stress as two plates interact and causes frequent moderate to strong earthquakes. eg. marianas trench. type three: continental continental plate margin. both will not sink. cos they are relatively light and resist downwards movements. crust will buckle or be uplifted to form fold mountains. termed as collison zone. eg, himalayan mountain. mass movements. heave: downwards movement of particles thru alternation of expanison and contraction. eg. frost heave. flow: downwards movement w/o clear defined plane. eg. earthflow, mudflow sldie: downwards movement with clear defined plane. eg. rock slides and land slides. deep landslides: rotaional slumps and slips. five key factors affecting hydological cycle. 1) climate (ppt) 2) vegatation 3) soil condition 4) geology (rock types) 5) relief (steepness) alrighty. my summary for wat`s tested for geog tml. i hope i will rmbb all these! my brain is almost dead. i still got granite landforms. and human geog. Posted on: Monday, October 02, 2006 Posted at: 10:46 PM