Surah At-Thalaq No12. Allah yang menciptakan tujuh langit dan seperti itu pula bumi.
Jadi nurut Kitab saya ada 7 lapisan langit dan 7 lapisan bumi.Jadi dari bumi keatas ada 7 lapis langit,sebaliknya bumi masuk ketanah juga ada 7 lapisan.Yang 7 lapisan didalam atmosfir sudah terbukti,so do lapisan didalam tanah.La yg belum terbukti 7 lapisan langit,soale roketnya NASA baru sampai Yupiter(lapis ke-1 yg terluar). Paulus Anak Wedus. --- In [email protected], itemabu2 <itemabu2@...> wrote: > > Gua nanya bulan dan bintang ada di langit yg mana, si tawang ga berani jawab. > > Quran itu bilang ada 7 langit dan bumi sama banyaknya yg berarti ada 7 > bumi, bukannya bilang bumi terdiri dr 7 lapisan. > > Masalahnya, si tawang ini ga punya kemampuan unt ngejelaskan kutipan > yg diberikannya, bisanya cuma copas. > > > > On 7/2/13, Tawangalun <tawangalun@...> wrote: > > > > Ha ha bumipun ada 7 lapisan juga podo dg Kitab saya. > > > > Paulus Anak Wedus. > > The Layer of Earth [hor_green_bar1.jpg] > > [The interior of the Earth - copyright Calvin J. Hamilton] What is the > > use of locating seismic discontinuities? Locating these disturbances > > enable scientists to map the inner regions of the Earth. This science, > > known as tomography originates from the knowledge gained from > > discontinuities. > > > > Tomographists have found that this planet is divided into six regions: > > the inner core, the outer core, the lower mantle, the upper mantle, the > > transition region, and the crust (oceanic and continental). > > > > Here is a brief synopsis of the depths of each layer (in kilometers): > > > > > > 1. 0- 40 Crust > > 2. 40- 400 Upper mantle > > 3. 400- 650 Transition region > > 4. 650-2700 Lower mantle > > 5. 2700-2890 D'' layer > > 6. 2890-5150 Outer core > > 7. 5150-6378 Inner core > > > > > > > > [The Interior of the Earth - copyright Calvin J. Hamilton] The inner > > core is a solid section of the Earth and is unattached to the mantle, > > being suspended by the molten outer core. This solidified state is the > > result of a very intense pressure-freezing process that occurs in most > > liquids when temperature decreases or pressure increases. The outer > > core of Earth is a scorching hot, electrically conductive liquid in > > which convection takes place. This inner layer in mutual combination > > with the rotational motion of the Earth creates a dynamo effect where a > > force ield of electrical currents is generated. This field is also > > known as Earth's magnetic field, which is responsible for the > > functioning of mechanical and biological compasses. This field also > > causes a subtle jerking motion in the Earth's daily rotation. In terms > > of the physical aspects of the outer core, the layer is dense, but not > > as dense as pure molten iron, evidencing the presence of multiple > > impurities having a lighter chemical makeup. According to scientists, > > about 10% of this layer is composed of sulfur and/or oxygen due to the > > fact that these two elements are abundant in the cosmos and dissolve > > readily in molten iron. > > > > [Crustal Plate Boudaries] > > > > 1. The outer core is in the range of 200 to 300 kilometers (125 to > > 188 miles) thick and represents about 4% of the mantle-crust mass. This > > layer is sometimes identified as part of the lower mantle due to its > > geographical nature. However, studies on seismic discontinuities > > suggest that this "D" layer might differ chemically rom the lower > > mantle lying above it. > > > > > > 2. Looking at the lower mantle, its chemical omposition includes > > silicon, magnesium, and oxygen. Most likely, it probably also contains > > some iron, calcium, and aluminum. This layer is comprised of 72.9% of > > the antle-crust mass, making the Earth abundant in the chemical > > elements of silicon, magnesium and oxygen, the layer's primary > > components. > > > > > > [A View of Saudi Arabia - courtesy NASA] 3. 3. Higher up, we > > encounter the upper mantle. Through excavations in volcanoes, > > scientists have found that this part of the crust composes of 15.3% of > > the total mantle-crust mass and is made of crystalline forms of Olivine > > (Mg,Fe)2SiO4 and pyroxene (Mg,Fe)SiO3. The upper mantle makes up 10.3% > > of the Earth's mass, extending a depth of 6-250 miles (10-400 > > kilometers). A relatively large portion when compared to the other > > interior layers. This layer is not completely made of solid minerals > > for scientists speculate that the asthenosphere could be partly liquid > > molten. > > > > > > 4. D: The D" layer of Earth is about 3% of Earth's mass, is 125 to > > 188 miles (200 to 300 kilometers) thick and covers about 4% of the > > mantle-crust mass. This layer, in terms of whether it is part of the > > lower mantle or an independent layer is still somewhat unclear. Based > > on evidence collected from seismic discontinuities, the D" layer might > > differ in chemical composition from the lower mantle above it. > > > > > > 5. The next layer, the Transition region comprises 7.5% of Earth's > > mass with a depth of 250-406 miles (400-650 kilometers). This layer is > > also known as the mesosphere and is 11.1% of the mantle-crust. It is > > made of mainly basaltic magmas with amounts of calcium, aluminum and > > garnet (an aluminum-bearing silicate mineral). The layer becomes dense > > when the garnet mineral cools but is buoyant and light when subject to > > heat due to the low melting points. > > > > > > [Earth] 6. The outer most layer, the crust, is categorized into two > > parts, the Oceanic crust and the continental crust. The Oceanic crust is > > the smallest part of Earth, only 0.099% of its mass and reaching a > > small depth of 0-6 miles (0-10 kilometers). In the beginning of time, > > it was possible that this area did not exist for through frequent > > volcanic activity does only the crust form. Evidence of this is marked > > by the oceanic ridge system, which is a 25,000 mile (40,000-kilometer) > > array of many volcanoes which creates layer after layer of new crust at > > the rate of 17 km3 per year. The ocean floor is covered in basalt > > originating from volcanic activity and as a matter of fact, Iceland and > > Hawaii are two island systems that emerged from the accumulated basalt. > > > > > > 7. Continental crust: The second smallest area of the Earth is the > > Continental crust, making up only 0.374% of the Earth's mass and > > extending a short depth of 0 - 31 miles (0-50 kilometers). Looking at > > the percent by composition, the continental crust makes up only 0.554% > > of the mantle-crust mass. The layer is composed primarily of > > crystalline rocks made of low-density buoyant minerals dominated mostly > > by quartz (SiO2) and feldspars (metal-poor silicates). This is the > > outer part of the Earth composed essentially of crystalline rocks. The > > continental crust and the oceanic crust are also referred to as the > > lithosphere because of the cool and rocky conditions that exist in its > > chemical composition. > > > > > > > > > > > > > > [Non-text portions of this message have been removed] > > > > > ------------------------------------ Post message: [email protected] Subscribe : [email protected] Unsubscribe : [email protected] List owner : [email protected] Homepage : http://proletar.8m.com/Yahoo! Groups Links <*> To visit your group on the web, go to: http://groups.yahoo.com/group/proletar/ <*> Your email settings: Individual Email | Traditional <*> To change settings online go to: http://groups.yahoo.com/group/proletar/join (Yahoo! ID required) <*> To change settings via email: [email protected] [email protected] <*> To unsubscribe from this group, send an email to: [email protected] <*> Your use of Yahoo! Groups is subject to: http://docs.yahoo.com/info/terms/
