Molten Lava

Lithosphere
Lithosphere
Lithosphere Notes on the lithosphere- (rock sphere) Upper most part is crust of earth. Compiled of rocks of outer crust. Outermost shell. Upper part- rocks we see at and near the earths surface. Crust is 5 to 10 km thick under most oceans and 24 to 60 km thick under the continents. The lithosphere under the crust is solid, dense material. (more dense than surface materials). Lithosphere 100-200 km. Notes on the aesthenosphere- zone beneath the lithosphere. Thick like tar. Weak because of high t
Mountains
Mountains
Mountains I. INTRODUCTIONAmountain is an elevated land mass usually higher than its surroundings. Some are isolated, but they usually appear in ranges(MsBs95W32). A group of ranges closely related in form, origin, and alignment is a mountain system; an elongated group of systems is a chain; and a complex of ranges, systems, and chains continental in extent is a cordillera, zone, or belt.(MsBs95W32). Some mountains are remains of plateaus, mesas, and buttes, through erosion(Summerfield). Other
Internal Structure Of The Earth
Internal Structure Of The Earth
Internal Structure of the Earth What is the evidence for our knowledge of the internal structure of the Earth? As we enter the twenty first century we are beginning to learn more and more about the composition of the Earth. Early predictions have thrown up some rather strange and peculiar thoughts as to what is making up our Earth, but now day??s scientists can be confident that the Earth is made up of what they think. As from experiments and other sources of information a picture to what is rea
A Discussion On Earthquakes
A Discussion On Earthquakes
A Discussion On Earthquakes Perhaps Mother Nature offers no greater force than that of the earthquake. Across the span of time, earthquakes have been recorded for their incredible destructive forces, and their abilities to awe mankind with their unparalleled force. Earthquakes can often strike without any notice, leveling large cities and killing scores of innocent people. Not only can earthquakes bring harm to society through these methods of destruction, but they can also cause millions of dol
IS 490
IS 490
IS 490 SPECIAL TOPICS Computer Graphics May 6, 1996 Table of Contents Introduction 3 How It Was 3 How It All Began 4 Times Were Changing 6 Industry's First Attempts 7 The Second Wave 10 How the Magic is Made 11 Modeling 12 Animation 13 Rendering 13 Conclusion 15 Bibliography 16 Introduction Hollywood has gone digital, and the old ways of doing things are dying. Animation and special effects created with computers have been embraced by television networks, advertisers, and movie studios alike. F