Beaches Sandy Karangbolong Is That Enough Ramps Beach Area, The Hills The Restricted By Compiled By rocks clastic sediment-volcanic origin. The Grey Colored Sand Smooth-Rough Sized Sourced From Such rocks. The Great Waves sweep Bumping The Wall hills Produce Enough Energy To Scrape, Transporting and precipitate Back Granules rocks. Weathering The Higher Degrees This area Accelerate Such Abrasion Process. Local, Lahar The Outcrop Breccia Being Experienced In Uptown Coastal Erosion, Abrasion Generate Unique formation. Having Karangbolong Coast Potential Reverse Flow Forming Strong, So Which Is Hazardous To Swim Zone. Other activities Travelers Can Do Is Fishing, Where Some Fish Species Coral Simply Abundant At This beach.
This Coastal Region Also There Karangbolong Cave, which is located in the East Side. The Quite A Long Hallway Formed In The frozen lava breccia layer. Cave Karangbolong Sized Length 300 M, 100 M Width And Height Approximately 55 M. The Breccia Formation Known As Gabon Oligo-Miocene It Or Aged Between 300 155 Million Years Ago, Afterwards it was revealed Together With Stone Sand And Stone Inserts clays.
Cave Formation Karangbolong Influenced By tearing down Happens In Field Along the Border Between Breccia With Sand Or Stone Clay Stone. The Big Hole demolition Will Rock For The Dangling Layer Hole In Roof Collapses Due Weighing Always. The process was also Fueled By Stump-Existing Stump, The Presence Weakening Tie Between Components Power Stone. Cave Formation Process Observed Good-In South And East End Karangbolong Cave, Where the Small Scale occurred demolition rock Alongside Different Boundary Layer. Because not Limestone Caves, then at the Cave Ornament Karangbolong not found.
This Coastal Region Also There Karangbolong Cave, which is located in the East Side. The Quite A Long Hallway Formed In The frozen lava breccia layer. Cave Karangbolong Sized Length 300 M, 100 M Width And Height Approximately 55 M. The Breccia Formation Known As Gabon Oligo-Miocene It Or Aged Between 300 155 Million Years Ago, Afterwards it was revealed Together With Stone Sand And Stone Inserts clays.
Cave Formation Karangbolong Influenced By tearing down Happens In Field Along the Border Between Breccia With Sand Or Stone Clay Stone. The Big Hole demolition Will Rock For The Dangling Layer Hole In Roof Collapses Due Weighing Always. The process was also Fueled By Stump-Existing Stump, The Presence Weakening Tie Between Components Power Stone. Cave Formation Process Observed Good-In South And East End Karangbolong Cave, Where the Small Scale occurred demolition rock Alongside Different Boundary Layer. Because not Limestone Caves, then at the Cave Ornament Karangbolong not found.
Karang Bolong Beach Viewpoint
salam kenal pak guru...monggo gabung di komunitas blogger magetan :-) (tambah teman jg pak).
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Salam kenal balik Pak S. Wibowo. terimakasih kunjungannya. dan undangannya. Sukses buat bapak dan juga kota Magetan tercinta.
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