<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss' xmlns:gd='http://schemas.google.com/g/2005' xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-6149900924900634616</id><updated>2011-11-27T17:07:25.271-08:00</updated><title type='text'>AKYATERO</title><subtitle type='html'>"Take nothing but pictures. Kill nothing but time. Leave nothing but footprints."</subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://mga-akyatero.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/6149900924900634616/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://mga-akyatero.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>GOLEM</name><uri>http://www.blogger.com/profile/08190418755030137303</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>1</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>100</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-6149900924900634616.post-3238144084095226774</id><published>2008-03-17T17:34:00.000-07:00</published><updated>2008-12-10T16:46:03.852-08:00</updated><title type='text'></title><content type='html'>&lt;span style="color: rgb(0, 0, 0);font-family:arial;font-size:85%;"  &gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/_WoMwzzYuWp0/R98QAbo_AvI/AAAAAAAAAAs/YQ9bM9lp1G8/s1600-h/mt+pinatubo+crater.jpg"&gt;&lt;img style="margin: 0pt 0pt 10px 10px; float: right; cursor: pointer; width: 181px; height: 202px;" src="http://2.bp.blogspot.com/_WoMwzzYuWp0/R98QAbo_AvI/AAAAAAAAAAs/YQ9bM9lp1G8/s320/mt+pinatubo+crater.jpg" alt="" id="BLOGGER_PHOTO_ID_5178875696105063154" border="0" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;div  style="text-align: justify; color: rgb(0, 0, 0);font-family:arial;"&gt;&lt;span style="font-size:85%;"&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_WoMwzzYuWp0/R98P5ro_AuI/AAAAAAAAAAk/ZDeVNCE7R60/s1600-h/pinatubo.jpg"&gt;&lt;img style="margin: 0pt 10px 10px 0pt; float: left; cursor: pointer; width: 187px; height: 177px;" src="http://3.bp.blogspot.com/_WoMwzzYuWp0/R98P5ro_AuI/AAAAAAAAAAk/ZDeVNCE7R60/s320/pinatubo.jpg" alt="" id="BLOGGER_PHOTO_ID_5178875580140946146" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;Mount Pinatubo is an active &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Stratovolcano" title="Stratovolcano"&gt;stratovolcano&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; located on &lt;/span&gt;&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt;the island of &lt;a href="http://en.wikipedia.org/wiki/Luzon" title="Luzon"&gt;Luzon&lt;/a&gt; in the &lt;a href="http://en.wikipedia.org/wiki/Philippines" title="Philippines"&gt;P&lt;/a&gt;&lt;a href="http://en.wikipedia.org/wiki/Philippines" title="Philippines"&gt;h&lt;/a&gt;&lt;a href="http://en.wikipedia.org/wiki/Philippines" title="Philippines"&gt;ilippines&lt;/a&gt;, at the intersection of the borders of the prov&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt;inces o&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt;f &lt;a href="http://en.wikipedia.org/wiki/Zambales" title="Zambales"&gt;Zamb&lt;/a&gt;&lt;a href="http://en.wikipedia.org/wiki/Zambales" title="Zambales"&gt;ales&lt;/a&gt;, &lt;a href="http://en.wikipedia.org/wiki/Tarlac" title="Tarlac"&gt;Tarlac&lt;/a&gt;, and &lt;a href="http://en.wikipedia.org/wiki/Pampanga" title="Pampanga"&gt;Pampanga&lt;/a&gt;. Ancestral Pinatubo was a stratovolcano made of &lt;a href="http://en.wikipedia.org/wiki/Andesite" title="Andesite"&gt;andesi&lt;/a&gt;&lt;a href="http://en.wikipedia.org/wiki/Andesite" title="Andesite"&gt;te&lt;/a&gt;&lt;a href="http://en.wikipedia.org/wiki/Dacite" title="Dacite"&gt;dacite&lt;/a&gt;. Before 1991, the mountain was inconspicuous and heavily &lt;a href="http://en.wikipedia.org/wiki/Erosion" title="Erosion"&gt;eroded&lt;/a&gt;. It was covered in dense &lt;a href="http://en.wikipedia.org/wiki/Forest" title="Forest"&gt;forest&lt;/a&gt; which supported a population of several thousand indigenous people, the &lt;a href="http://en.wikipedia.org/wiki/Aeta" title="Aeta"&gt;Aeta&lt;/a&gt;, who had fled to the mountains from the lowlands when the &lt;a href="http://en.wikipedia.org/wiki/Spanish_Empire" title="Spanish Empire"&gt;Spa&lt;/a&gt;&lt;a href="http://en.wikipedia.org/wiki/Spanish_Empire" title="Spanish Empire"&gt;nish&lt;/a&gt; conquered the Philippines in 1565. &lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt; and&lt;/span&gt; &lt;/div&gt;&lt;p  style="text-align: justify; color: rgb(0, 0, 0);font-family:arial;"&gt;&lt;span style="font-size:85%;"&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/_WoMwzzYuWp0/R98ZF7o_A5I/AAAAAAAAAB8/MuxoCmXhyPc/s1600-h/mt+pinatubo.jpg"&gt;&lt;img style="margin: 0pt 10px 10px 0pt; float: left; cursor: pointer; width: 256px; height: 156px;" src="http://4.bp.blogspot.com/_WoMwzzYuWp0/R98ZF7o_A5I/AAAAAAAAAB8/MuxoCmXhyPc/s320/mt+pinatubo.jpg" alt="" id="BLOGGER_PHOTO_ID_5178885686198993810" border="0" /&gt;&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;The volcano's eruption in June 1991 produced the second largest terrestrial eruption of the 20th century.&lt;/span&gt;&lt;sup style="color: rgb(0, 0, 0);" id="_ref-Pinatubo1991_0" class="reference"&gt;&lt;a href="http://en.wikipedia.org/wiki/Mount_Pinatubo#_note-Pinatubo1991" title=""&gt;[2]&lt;/a&gt;&lt;/sup&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; The 1991 eruption had a &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Volcanic_Explosivity_Index" title="Volcanic Explosivity Index"&gt;Volcanic Explosivity Index&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; (VEI) of 6, and came some 450-500 years after the volcano's last known eruptive activity (estimated as VEI 5, the level of the &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/1980_eruption_of_Mount_St._Helens" title="1980 eruption of Mount St. Helens"&gt;1980 &lt;/a&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/1980_eruption_of_Mount_St._Helens" title="1980 eruption of Mount St. Helens"&gt;eruption of Mount St. Helens&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;), and some 500-1000 years after previous VEI 6 eruptive activity.&lt;/span&gt;&lt;sup style="color: rgb(0, 0, 0);" id="_ref-0" class="reference"&gt;&lt;a href="http://en.wikipedia.org/wiki/Mount_Pinatubo#_note-0" title=""&gt;[3]&lt;/a&gt;&lt;/sup&gt; &lt;span style="color: rgb(0, 0, 0);"&gt;Successful predictions of the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives, but as the surrounding areas were severely damaged by&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Pyroclastic_flow" title="Pyroclastic flow"&gt;pyroclastic flows&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;, ash deposits, and later, &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Lahar" title="Lahar"&gt;lahars&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; caused by rainwater remobilizing earlier volcanic deposits, thousands of houses and other buildings were destroyed.&lt;/span&gt;&lt;sup style="color: rgb(0, 0, 0);" id="_ref-Pinatubo1991_1" class="reference"&gt;&lt;a href="http://en.wikipedia.org/wiki/Mount_Pinatubo#_note-Pinatubo1991" title=""&gt;[2]&lt;/a&gt;&lt;/sup&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/_WoMwzzYuWp0/R98Xzbo_A3I/AAAAAAAAABs/zXVbbgAsVeM/s1600-h/pinatubo+trail2.jpg"&gt;&lt;img style="margin: 0pt 0pt 10px 10px; float: right; cursor: pointer; width: 283px; height: 158px;" src="http://2.bp.blogspot.com/_WoMwzzYuWp0/R98Xzbo_A3I/AAAAAAAAABs/zXVbbgAsVeM/s320/pinatubo+trail2.jpg" alt="" id="BLOGGER_PHOTO_ID_5178884268859786098" border="0" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;/p&gt;&lt;div style="color: rgb(0, 0, 0); font-family: arial;"&gt; &lt;/div&gt;&lt;p  style="text-align: justify; color: rgb(0, 0, 0);font-family:arial;"&gt;                          &lt;/p&gt;&lt;span style="color: rgb(0, 0, 0);font-family:arial;font-size:85%;"  &gt;&lt;span style="color: rgb(0, 0, 0);"&gt;Its summit was 1,745 m (5,725 ft) above sea level, but only about 600 m above nearby &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Plain" title="Plain"&gt;plains&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;, and about 200 m higher than surrounding peaks, which largely obscured it from view.&lt;/span&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;span style="color: rgb(255, 255, 255);"&gt;-------------------------------------------------------------------------------------------------&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;p  style="text-align: justify; color: rgb(0, 0, 0);font-family:arial;"&gt;                                                                                                      &lt;/p&gt;&lt;span style="color: rgb(0, 0, 0);font-family:arial;font-size:85%;"  &gt;&lt;br /&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_WoMwzzYuWp0/R98eZro_A9I/AAAAAAAAACc/-NpIqcLpTtk/s1600-h/mt+banahaw.jpg"&gt;&lt;img style="margin: 0pt 10px 10px 0pt; float: left; cursor: pointer; width: 226px; height: 138px;" src="http://3.bp.blogspot.com/_WoMwzzYuWp0/R98eZro_A9I/AAAAAAAAACc/-NpIqcLpTtk/s320/mt+banahaw.jpg" alt="" id="BLOGGER_PHOTO_ID_5178891523059549138" border="0" /&gt;&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;Mount Banahaw&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; (alternatively Banáhao) is a &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Dormant_volcano" title="Dormant volcano"&gt;dormant&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; volcanic complex located on the boundary of &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Majayjay%2C_Laguna" title="Majayjay, Laguna"&gt;Majayjay&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;, &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Laguna_province" class="mw-redirect" title="Laguna province"&gt;Laguna&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; and &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Lucban%2C_Quezon" title="Lucban, Quezon"&gt;Lucban&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;, &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Quezon" title="Quezon"&gt;Quezon&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; in &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Luzon" title="Luzon"&gt;Luzon&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;, &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/wiki/Philippines" title="Philippines"&gt;Philippines&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;. Itis considered to be sacred by the local residents because of its "holy water"and "&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;puwesto&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;"s, or holy sites. These are composed of natural features with shrines located in or on them, revealed to a man by the "&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;Santo Boses&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;" or Holy Voice. It has another of this mountain and it was named as &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/w/index.php?title=Mount_Banahaw_de_Lucban&amp;amp;action=edit&amp;amp;redlink=1" class="new" title="Mount Banahaw de Lucban (page does not exist)"&gt;Mount Banahaw de &lt;/a&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://en.wikipedia.org/w/index.php?title=Mount_Banahaw_de_Lucban&amp;amp;action=edit&amp;amp;redlink=1" class="new" title="Mount Banahaw de Lucban (page does not exist)"&gt;Lucban&lt;/a&gt;&lt;span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;.&lt;/span&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-family:arial;font-size:85%;"  &gt;Along Crystalino trail you will pass by the &lt;u&gt;Crystalino Falls&lt;/u&gt;, &lt;u&gt;Suplina Falls&lt;/u&gt;, &lt;u&gt;Salamin Bubog&lt;/u&gt;                  (glass mirror) which is a small pond in which the waters are still as a mirror; the &lt;u&gt;Kweba ng Dios Ama&lt;/u&gt; (cave), one of the most sacred place but you will be disgusted to see a concrete house erected by one of the local sects right in the mouth of the cave; the &lt;u&gt;Pintong Lihim&lt;/u&gt;                  (sacred door)- two large boulders with divergent paths and &lt;u&gt;Niluhuran&lt;/u&gt; (place where trees knelt) which was named due to the bent trees which abound the place and some minor pilgrim sites (holy places). At the summit try to visit the Durungawan (view points) I, II, and III (highest point), the cave near the cross and the crater view overlooking Guis-guis and two other rivers Tubig ng Gatas at Tubig ng Dugo (river of blood and milk because one is white as marble and the other red as iron oxide). Along the Tatlong Tangke route, pass by Kapatagan (plains) and the Tatlong Tangke (3 natural water tanks).&lt;/span&gt;&lt;span style=";font-family:arial;font-size:85%;"  &gt;&lt;br /&gt;&lt;/span&gt;&lt;p  style="text-align: justify; color: rgb(0, 0, 0);font-family:arial;"&gt;&lt;span style="font-size:85%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p  style="color: rgb(0, 0, 0);font-family:arial;"&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt;&lt;span&gt;Mount Makulot&lt;/span&gt;, a 600-meter (2,000 feet) high volcanic rock wall, is said to be part of Taal Volcano’s crater rim. Some scientists contend that Taal Volcano was once a massive volcano before a violent &lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt;eruption caused the slopes t&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt;o cave in. This caused water to rush in, forming a lake that left only the tip of the previous peak exposed, and that is now known as the current Volcano Island. The slopes of the previous volcano now formed ridges surrounding the lake, with Mount Makulot as the highest volcanic cone on the south side,      Tagaytay &lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt;Ridge on the north, and at lower level, the lakeshore settlements surrounding Taal Lake.&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt; &lt;/span&gt;&lt;/p&gt;&lt;span style="color: rgb(0, 0, 0);font-family:arial;font-size:85%;"  &gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/_WoMwzzYuWp0/R98epbo_A-I/AAAAAAAAACk/ToAkpsJSKzo/s1600-h/maculot.jpg"&gt;&lt;img style="margin: 0pt 10px 10px 0pt; float: left; cursor: pointer;" src="http://2.bp.blogspot.com/_WoMwzzYuWp0/R98epbo_A-I/AAAAAAAAACk/ToAkpsJSKzo/s320/maculot.jpg" alt="" id="BLOGGER_PHOTO_ID_5178891793642488802" border="0" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-family:Tahoma,Verdana,Arial,Helvetica;font-size:85%;"  &gt;The "Rockies,"&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-family:Tahoma,Verdana,Arial,Helvetica;font-size:85%;"  &gt; located at the northern edge of Mount Makulot, affords one a stunning view of the mountain, the lake and the Volcano Island from a cliff that drops far way down to t&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-family:Tahoma,Verdana,Arial,Helvetica;font-size:85%;"  &gt;he jungle below.&lt;/span&gt;&lt;p  style="text-align: justify; color: rgb(0, 0, 0);font-family:arial;"&gt;&lt;span style="font-size:85%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p face="arial" style="text-align: justify; color: rgb(0, 0, 0);"&gt;&lt;span style="font-size:85%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p face="arial" style="text-align: justify; color: rgb(0, 0, 0);"&gt;&lt;span style="font-size:85%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: justify; color: rgb(0, 0, 0); font-family: arial;"&gt;&lt;span style="font-size:85%;"&gt;&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p style="text-align: justify; color: rgb(0, 0, 0); font-family: arial;"&gt;&lt;span style="color: rgb(255, 255, 255);font-size:85%;" &gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://2.bp.blogspot.com/_WoMwzzYuWp0/R98d5bo_A8I/AAAAAAAAACU/KOYHbaxlabA/s1600-h/mt.+sembrano.jpg"&gt;&lt;img style="margin: 0pt 10px 10px 0pt; float: left; cursor: pointer; width: 226px; height: 138px;" src="http://2.bp.blogspot.com/_WoMwzzYuWp0/R98d5bo_A8I/AAAAAAAAACU/KOYHbaxlabA/s320/mt.+sembrano.jpg" alt="" id="BLOGGER_PHOTO_ID_5178890969008767938" border="0" /&gt;&lt;/a&gt;&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);font-size:85%;" &gt;M&lt;/span&gt;&lt;span style="font-size:85%;"&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;t. Romelo, a     part of the legendary Sierra Madre Mountain Range located in Famy, Laguna, is well known to     mountaineers simply as Famy. This is the most accessible trekking destination for     Manileños. It boasts of several waterfalls; namely Buruwisan, Batya-Batya, Sampaloc and     Lanzones. Buruwisan, the largest fall is an ideal place for rappelling. So if you have the     guts, include this in your itinerary and bring a harness, ropes and rappelling devices     with you.&lt;/span&gt;&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_WoMwzzYuWp0/R98hIro_A_I/AAAAAAAAACs/4MHFTD9AuY0/s1600-h/mount.jpg"&gt;&lt;img style="margin: 0pt 0pt 10px 10px; float: right; cursor: pointer;" src="http://3.bp.blogspot.com/_WoMwzzYuWp0/R98hIro_A_I/AAAAAAAAACs/4MHFTD9AuY0/s320/mount.jpg" alt="" id="BLOGGER_PHOTO_ID_5178894529536656370" border="0" /&gt;&lt;/a&gt;&lt;/span&gt;  &lt;/p&gt;&lt;p  style="color: rgb(0, 0, 0);font-family:arial;" align="left"&gt;&lt;span style="font-size:85%;"&gt;This is the most ideal venue to develop your rappelling     skills since there is water below that will break your fall. It also gives you the feeling     of rushing down with the flow of the water. The catch basin is also ideal for swimming.     Above the Buruwisan Falls is the usual campsite. From here, you can trek upstream to     Batya-Batya and Sampaloc Falls or downstream to Lanzones and another falls.&lt;/span&gt;&lt;/p&gt;&lt;p  style="color: rgb(0, 0, 0);font-family:arial;" align="left"&gt;&lt;span style="font-size:85%;"&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;span style="color: rgb(0, 0, 0);font-family:arial;font-size:85%;"  &gt;&lt;span style="color: rgb(0, 0, 0);"&gt;MEMBERS:&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; &lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; &lt;/span&gt;&lt;span style="color: rgb(255, 0, 0);"&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;POGI ,MAKO ,GELAY ,TON-TON,DARNOC ,TROY &amp;amp; ME GOLEM&lt;/span&gt;&lt;br /&gt;&lt;br /&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;We started climbing back in 1996 in &lt;/span&gt;&lt;a style="color: rgb(0, 0, 0);" href="http://www.jurgita.com/pictures-id228963.html"&gt;&lt;span style="color: rgb(51, 51, 255);"&gt;MT.ROMELO&lt;/span&gt;&lt;/a&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;(also known as mt.Famy).We're very excited in our first climb eventhough we're not have our owned backpacks,tents,and other gadgets... but still we're able to climb..My friend got extra backpacks that i've used,about the tents tnx to  M.H.S. where gelay is working he borrowed the two tents(coleman).We've decided to climb Mt.Romel in night..so we bring our flashlights..Going to Laguna..we are on top of a jeep in a road like ISAW in a very dark night coz the light post in very far from one to other post..&lt;/span&gt;&lt;br /&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;we know that its very dangerous on top but still were not able to come down and go inside the jeep..its a long drive,everybody is freezing but were very happy and excited in our first climb ever..and finally,we're in Famy,laguna...and we need to take a ride again but for now not a jeep but a tricycle..we're 6,so we take a 2 tricycle.And we ask the driver..how long it's gonna take in the PAA of Mt.Romelo?for about 25-30 mins...excited and nervous are all we have...and finally were in Mt.romelo anything else first we have to log our names in barangay i don't remeber the name manang .....(it's been a long time)...and we started to trek...we stop for a while to pray for the guidance of the lord and strength for our feets and asking to finish that trek were no one is hurt...and darnoc leads the prayer in the middle of very dark and silent night were the only the light were using is the light coming from the sky from moon...so we're done...now were starting the trek...darnoc is the only one whose been here  so he leads the way...were all freezing so we decided to a wear a jacket...in a minutes we are in first BUROL were no one else is wearing their jacket..coz its very hot and very swet...&lt;/span&gt;&lt;br /&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;on the second BUROL were all tired and thingking about to go back..there's only one BUROL&lt;/span&gt;&lt;br /&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;remains the thing is were already here we know that were very tired but we want this it's a big experience that we want to fulfill and tell everyone that WE BEEN THERE...every ones agree...when were already in the third BUROL...we heard some water falls...everyones shouting..."MALAPIT NA TAYO,,YEHEY"...we want to run but it's very sleepery so we walk fast and suddenly we saw a lot of people on their tents...so first were looking for the place were we can put our tents..and pogi starting to cook our foods a heavy meal rice and canned foods..and were talking about our experience in the trek and i can see the smile in our face,tired but we conquer this..after the dinner we started to drink GIN cause its very cold here after the 2 bottles were done were going to sleep.in the morning for along sleep..i've cooked our breakfast and hot coffee so we can go to BATSA-BATSA and falls...in a way to BATSA-BATSA were walking to the water were in the middle  is deep and troy is the only man from us whose stand tall.....this is a funny experience...were walking in GILID and were holding to the stem of the tree..and suddenly troy(the tallest man)are sinking...and asking for our help..(triy is a funny guy whose always PALABIRO)so were laughing at him...we dont recognize that troy in not joking after he had find something to hold on...and he said"mga punyeta kayo mamamatay na ko wala man lang tumulong sa inyo"hehehehe...no one from us knows how to swim...not joking...we have our camera  take a picture there,here everywhere...&lt;/span&gt;&lt;br /&gt;&lt;br /&gt;&lt;span style="color: rgb(0, 0, 0);"&gt;It's a great experience so were planning to climb again but for now&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; &lt;a href="http://www.waypoints.ph/detail_gen.html?wpt=mculot"&gt;Mt.MACULOT&lt;/a&gt;&lt;/span&gt;&lt;span style="color: rgb(0, 0, 0);"&gt; in batangas...all the mountaneers started here(MT.REMOLO)minor climb...&lt;/span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;&lt;p style="text-align: justify; color: rgb(0, 0, 0); font-family: arial;"&gt; &lt;/p&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/6149900924900634616-3238144084095226774?l=mga-akyatero.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://mga-akyatero.blogspot.com/feeds/3238144084095226774/comments/default' title='Post Comments'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=6149900924900634616&amp;postID=3238144084095226774' title='0 Comments'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/6149900924900634616/posts/default/3238144084095226774'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/6149900924900634616/posts/default/3238144084095226774'/><link rel='alternate' type='text/html' href='http://mga-akyatero.blogspot.com/2008/03/mount-pinatub-o-is-active-stratovolcano.html' title=''/><author><name>GOLEM</name><uri>http://www.blogger.com/profile/08190418755030137303</uri><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='16' height='16' src='http://img2.blogblog.com/img/b16-rounded.gif'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://2.bp.blogspot.com/_WoMwzzYuWp0/R98QAbo_AvI/AAAAAAAAAAs/YQ9bM9lp1G8/s72-c/mt+pinatubo+crater.jpg' height='72' width='72'/><thr:total>0</thr:total></entry></feed>
