> >> Dimana bulan dan bintang? Sampe sekarang si tawang ga ngejawab. Dan ga > >> akan ngejawab.
Plintat plintut terus. On 7/2/13, Tawangalun <[email protected]> wrote: > Yang satu langit sebagai pelindung itu atmosfir yg ternyata 7 lapis juga > ,setiap ada batu meteor yg masuk keatmosfir kan terbakar makane Q bilang > langit itu sebagai pelindung. > "Dan Kami menjadikan langit itu sebagai atap yang terpelihara, sedang mereka > berpaling dari segala tanda-tanda (kekuasaan Allah) yang ada padanya." (QS > Al-Anbiya : 32) > > Yg kedua langit yg tiap hari naik dg kadar 1 hari dibumi sama dg 1000 tahun > (Qs. Al-Hajj [22]:47) "Dia mengatur urusan dari langit ke bumi, kemudian > urusan itu naik kepada-Nya pada satu hari yang kadarnya (lamanya) adalah > seribu tahun menurut perhitunganmu . > > Memangnya kalau ada dua penegertian ttg langit ngopo? siapa sing melarang? > > Paulus Anak Wedus. > > --- In [email protected], itemabu2 <itemabu2@...> wrote: >> >> 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 <tawangalun@...> 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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