Romance Fan Fiction ❯ The Truth Will Be Revealed ❯ The Beginning of the Truth that lies behind her. ( Chapter 1 )

[ T - Teen: Not suitable for readers under 13 ]
By: VampireZac
Truth had been kept far away from me,
I lost my everything, my normal life, what else?
All I'm asking is what the real me is...

Miscellaneous: Romance Fan Fiction | Genre(s): Drama / Fantasy / Romance / Supernatural / Suspense | Type: Other | Uploaded On: 02.21.2009 | Pages: 1 | Words: 1.2K | Visits: 486 | Status: Work In Progress

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-ЅЋiΣLδ-
♪A shield volcano is a large volcano with shallow-sloping sides. The name derives from a translation of "Skjaldbreiður", an Icelandic shield volcano whose name means "broad shield", from its resemblance to a warrior's shield. Shield volcanoes are formed by lava flows of low viscosity — lava that flows easily. Consequently, a volcanic mountain having a broad profile is built up over time by flow after flow of relatively fluid basaltic lava issuing from vents or fissures on the surface of the volcano. Many of the largest volcanoes on Earth are shield volcanoes. The largest in terms of area covered is Mauna Loa of Hawai'i; the tallest measured from its base under the ocean, however, is Mauna Kea of Hawai'i. All the volcanoes in the Hawaiian Islands are shield volcanoes ♪
 
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A stratovolcano, sometimes called a composite volcano is a tall, conical volcano with many layers (strata) of hardened lava, tephra, and volcanic ash. Stratovolcanoes are characterized by a steep profile and periodic, explosive eruptions. The lava that flows from stratovolcanoes tends to be viscous; it cools and hardens before spreading far. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Although stratovolcanoes are sometimes called composite volcanoes because of their composite layered structure built up from sequential outpourings of eruptive materials, volcanologists prefer stratovolcano. The term composite volcano, is best reserved for those edifices with more than one eruptive peak. Stratovolcanoes are one of the most common types of volcanoes.
 
 
-Ċϊпđε ;Ѓ Ċοпė-
A cinder cone or scoria cone is a steep conical hill of volcanic fragments that accumulate around and downwind from a volcanic vent. The rock fragments, often called cinders or scoria, are glassy and contain numerous gas bubbles "frozen" into place as magma exploded into the air and then cooled quickly. Cinder cones range in size from tens to hundreds of meters tall. Cinder cones are made of pyroclastic material. Many cinder cones have a bowl-shaped crater at the summit. Lava flows are usually erupted by cinder cones, either through a breach on one side of the crater or from a vent located on a flank. If the crater is fully breached, the remaining walls form an amphitheatre or horseshoe shape around the vent. Lava rarely issues from the top (except as a fountain) because the loose, uncemented cinders are too weak to support the pressure exerted by molten rock as it rises toward the surface through the central vent.
Composite volcano. Mt.St, Helens

Hualalai Sunrise- Shield Volcano


Sunset Crater -Cinder Cone