Tawang yang memang sinting itu mengharapkan semua orang sama menjijikkan 
kelakuannnya dengan nabi junjungannya yang tukang entotin bocah cilik berumur 9 
tahun...


--- In [email protected], "Tawangalun" <tawangalun@...> wrote:
>
> Orang yg paling ciloko itu yo kamu ini Fiq,sudah jauh2 ninggalin kampuongnya 
> harapannya dapet yg kayak Ginalolo Brigidha jebul cuman dapet Londo tuwo,wah 
> itu kamu jelas jam 6.00 Fiq.Kasihan pasakmu gak bisa menghunjam ke 
> Marlene.Tapi begitu kamu didepan cewek lain atau ITEM Abu aja bisa jam 
> 15.00.Ha ha ha.
> 
> Paulus Anak Wedus.
> 
> --- In [email protected], "Bukan Pedanda" <bukan.pedanda@> wrote:
> >
> > 
> > 
> > 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 [email protected], "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]
> > > > >> >
> > > > >> >
> > > > >>
> > > > >
> > > > >
> > > > >
> > > >
> > >
> >
>




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