Anda itu jelas sinting Tawang...

Yang ada dibatok kepala anda itu adalah otak anjing.

Tidak ada bukti langit itu tujuh lapis...

Dan bintang-bintang itu juga tidak ada dilapisn langit yang paling rendah.

Kitab suci anda itu ngibul.

 

--- In proletar@yahoogroups.com, "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 proletar@yahoogroups.com, 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 proletar@yahoogroups.com, 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]
> > >> >
> > >> >
> > >>
> > >
> > >
> > >
> >
>




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