Oh jadi ada langit lain lagi selain yg 7 lapis itu. >> Dimana bulan dan bintang? Sampe sekarang si tawang ga ngejawab. Dan ga >> akan ngejawab.
tawang ini cuma ngebual plintat plintut ga keruan, ocehan yg satu akan kontradiksi dgn ocehannya yg lain. Dan dia ga akan ngejawab sesuatu yg jelas2 nunjukin ketololannya, dlm hal ini, dia sedikit ada pinternya. On 7/2/13, Tawangalun <[email protected]> wrote: > La yg Exosphere itu utk langit yg sebagai pelindung kita,yg telah dibuktikan > ada 7 lapis, kalau langit ketika Israk Mikraj lain lagi > itu Yupiter adalah lapisan 1 yg terluar.Ini belum bisa dibuktikan tapi Kitab > saya sudah ngomong duluan ada 7 lapisan juga.Nek bumi kita ini kedalam yo > sama ada 7 lapisan juga,dah terbukti. > > Paulus Anak Wedus. > > --- In [email protected], itemabu2 <itemabu2@...> wrote: >> >> Hehehe... katanya 7 lapis langit itu yg terluar adalah exosphere yg >> cuma ada di ketinggian beberapa ratus km, eh ternyata Yupiter ada di >> lapisan ke 1. Jadi Yupiter itu dekat sekali dgn bumi, hehehe... >> >> Dimana bulan dan bintang? Sampe sekarang si tawang ga ngejawab. Dan ga >> akan ngejawab. >> >> Tuh, auloh bilangnya nyiptain 7 langit, bukannya nyiptain 7 lapisan >> langit. Jadi bumi itu hrsnya ada 7, bukannya ada 7 lapisan bumi. >> >> Si tawang ini ga lbh make otaknya unt mlintir2 apa yg ditulis auloh, >> krn auloh itu salah ngasih penjelasan. >> >> Apa itu yg dimaksud dgn Quran itu unt orang yg mikir berhubung auloh >> terlalu goblok shg ga becus nulis? >> >> >> >> On 7/2/13, Tawangalun <tawangalun@...> wrote: >> > 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! 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