and the water lead me to find the cell where she was imprisoned. Now that I had found her‚ we needed to escape but I thought we were lost in the maze. We needed to find the way out‚ but waiting for us was only despair because in here there was only magma‚ swamp‚ water‚ lever mechanisms and a whole maze completely locked dead‚. I saw a mossy room‚ I heard the rain dripping down and the sound made us have the desire to survive. I smelled the rotting bodies of people who tried to escape but couldn’t.
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fertilize the soil for better growth of plants and similarly the sun’s light provides energy to green plants through photosynthesis. Although nature acts positively in many ways it also acts in a negatively. For example volcanoes release boiling hot magma that destroys land and causes deaths‚ in 1815 a volcano erupted in Indonesia which killed approximately 92‚000 people. Similarly this year there was an earthquake in Haiti on the 12th of January that had a magnitude of 7.0 and killed about 230‚000
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at destructive plate boundaries. Volcanoes can also be formed at a destructive plate boundary‚ for example in New Zealand where the Pacific Plate descends swiftly as it is pushed under the Indo-Austrailian Plate‚ this causes the crust to melt and magma to rise to the surface. New Zealand and the Japanese Islands (shown in the diagram above) are both examples of Island archs‚ these are formed when the edge of the less dense continental plate is pushed upwards by the subduction. Earthquakes are also
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Unlike other power plants that rely on coal or other ¬¬¬fossil fuels to create electricity for homes and businesses‚ geothermal power plants use superheated fluids from the earth’s geothermal energy to generate electricity. When magma heats up the water from underground‚ it creates superheated fluids. When these super-heated fluids reach the surface they will be turned into steam. This steam will then power a turbine‚ which will in turn power a conductor. The conductor will then produce electrical
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temperature of 136 degrees Fahrenheit has allowed the massive gypsum crystals to take their shape. For about 600‚000 year’s mineral-rich water filtered through the cave‚ depositing molecules of calcium sulfate in great amounts. The intrusive magma deep below the surface superheated the water‚ and then about half a million years ago the water temperature cooled to about 136 degrees Fahrenheit which then allowed the calcium sulfate in the water to form Selenite crystals. The water levels in the
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1.North American Continent Boundary: The North American Continent Boundary is where North America used to meet the pacific Ocean. Until subcontinents (Example:Northern Cascade Subcontinent‚ Okanagan Subcontinent) latched onto our continent and made most of Washington. The North American Continent is also slowly moving west due to Pangea breaking apart. That means that the Pacific Ocean is slowly getting smaller and that the Atlantic Ocean is slowly getting bigger 2 to 3 inches per year. 2.Kootenay
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Suggested time allotment: 14 hours MODULE 1 THE PHILIPPINE ENVIRONMENT Overview Everything that we see around us makes up our environment. The landforms and bodies of water that make up the landscape‚ the mountains and valleys‚ rivers and seas; the climate‚ the rains brought by the monsoons‚ the warm‚ humid weather that we frequently experience; the natural resources that we make use of; every plant and animal that live around us. Truly‚ the environment
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spacecraft and from Earth very difficult. There are many craters on Mercury that are made from a particular impact. There is also balsatic rock and plains which are made in the event of a massive volcanic eruption. There are also vents‚ made when a magma chamber collapses. Mercury’s density has produced a solid iron core that accounts for 60% of its volume. As of 2011‚ 99% of Mercury’s surface has been mapped by NASA. Overall‚ Mercury’s surface has many similarities to the Moon’s surface with many
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upon them. Part of geology is classifying and determining what was happening on our planet over time through rocks. Rocks are divided into three major classifications; • Igneous- rocks created by volcanism and the cooling/ crystallization of magma. • Sedimentary- rocks created by the compaction and cementation of sediment created by the weathering of pre-existing rocks of igneous‚ metamorphic or sedimentary origin. • Metamorphic- rocks that are formed by metamorphosing pre-existing
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1. What was Earth like in its infancy? How does it compare with the Earth today? In the very beginning of earth’s history‚ this planet was a giant‚ red hot‚ roiling‚ boiling sea of molten rock - a magma ocean. The heat had been generated by the repeated high speed collisions of much smaller bodies of space rocks that continually clumped together as they collided to form this planet. As the collisions tapered off the earth‚ it began to cool‚ forming a thin crust on its surface. As the cooling continued
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