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هل تريد التفاعل مع هذه المساهمة؟ كل ما عليك هو إنشاء حساب جديد ببضع خطوات أو تسجيل الدخول للمتابعة.

2 “And He has affixed into the earth mountains standing firm,

استعرض الموضوع التالي استعرض الموضوع السابق اذهب الى الأسفل

  2 “And He has affixed into the earth mountains standing firm, Empty 2 “And He has affixed into the earth mountains standing firm,

مُساهمة من طرف اعصار الثلاثاء 10 يوليو - 11:46:26

There are two theories to explain the origin of mountains in the earth.




  • The Geosynclines Theory:



  2 “And He has affixed into the earth mountains standing firm, 27033_250There
were large depositional basins from seas and oceans ranging from
hundreds of kilometers in length, tens of kilometers in width to more
than one hundred meters depth. Many clastic and non-clastic
types of sediments were deposited and accumulated in the floors of
theses basins, in the form of throwing from up to down to form
sedimentary rocks. The continuous thickening of these rocks caused loads
and led to subsidence of the basin floor. This subsidence was
accompanied by volcanic activity in the form of eruptions throwing the
lava upwardly. The result was a
thick intercalated sequence (about 1500m thick) form sedimentary and
volcanic rocks. However, the depositional basins are bounded by active
deep rifting faults which keep the continuous subsidence of the basins
and two opposite wards the processes of deposition downwardly and the
eruption of lava upwardly.





  • Plate Tectonic Theory: This recent theory depends on some facts in explaining the origin of mountains as follow:




  • The
    earth’s crust is broken up into plates or partitions called “tectonic
    plates” through cracks that can range from 65 to 150 kilometers in
    depth. The plate that forms the ocean floor is called ‘oceanic plate’
    and that which forms the continent is called ‘continental plate’. Around
    the earth there are about 12 large plates and several small ones. These
    plates which formed from continental or oceanic crust float on hot,
    semi-molten materials of weak sphere (Asthenosphere). There is continuous movement between the adjacent plates, which is extensional, compressional
    or transformable (sliding), occurs along a relatively narrow zone where
    plate tectonic forces are most active. Usually, these movements are
    accompanied by volcanic and seismic activities (earthquakes). The
    volcanoes erupt and throw lava and magma to the surface until the magma
    gathers and crystallize as volcanic rocks creating a mountain which can
    reach heights of up to thousands of meters above sea level. This is
    because volcano activity can last for 20- 30 years (although some
    volcanoes have been recorded as staying active for more than a thousand
    million years).




Examples of volcanic mountains include: Mount Ararat in Turkey (5100m), Mount Etna in Sicily, Italy (3300m), Mount Vesuvius in Italy (1300m), Kilimanjaro in Tanzania (5900m) and Mount Kenya in Kenya (5100m).




  • Throughout the field studies it was noted that; orogenic
    belts consist of rocks that have been folded intensively, thrust long
    distances horizontally, often metamorphosed, intruded with granite and
    elevated to form mountain chains. These belts result from the forces of
    compression and convergent movements of the plates, which makes up the
    solid outer part of the Earth’s crust. These forces usually rise at the
    margins of discrete rigid plates and are accounted for by the theory of
    plate tectonics. Two main types of plate are found as mentioned before:
    continental plates that consist of relatively light rocks and heavier
    oceanic plates, which lie under most of the ocean basins of the world.
    Compression occurs when two plates converge and one sinks below the
    other along a subduction zone. Convergence,
    and the subsequent collision that generates compression, takes in three
    forms: collision between oceanic plate with continental one, two
    continental plates or between two oceanic plates.




The
first of these forms develops when convergence occurs along active
continental margins where an oceanic plate is passing under the edge of a
continental plate. As the oceanic plate descends into the mantle of the
earth, it is melted and injected back into the crust, with volcanic
activity to form mountain chain consists mainly of volcanic rocks. The
second form of collision takes place between two oceanic plates leading
to the subsidence of one of them and forming a series of islands in the
form of ‘volcanic island arc’ in another oceanic plate. If this process
continues, the volcanic island arc can be carried on the oceanic plate
towards the continent where it collides with the continental plate—this
is called an arc-continent collision. Sedimentary rocks which have
accumulated in the sea basin between the island arc and the continental
plate are folded, faulted, and thrust into an elevated position over the
margin of the continental plate towards the centre of the continent
along a plane or surface known as a decollement.
The island arc eventually becomes involved in this compression and the
rocks of which it was composed are often metamorphosed by heat and
pressure and injected with granite.




The third form of compression and orogeny
results from continent-continent collision (two continental plates).
Typically in this type of collision, two continents converge, one with a
passive margin in which the continental and oceanic crust are welded
together, the other with an active margin where the subduction
of the oceanic crust under the continent eventually causes the closure
of the intervening ocean basin. As closure begins, slices of the oceanic
crust and any sediment that they carry are thrust on to the continental
margins. As the thrust continues the slices are folded and elevated and
eventually move horizontally, possibly sliding due to gravity on to the
continents to form huge folds or thrust-nappes. These nappes
become eroded to form the mountain chains. As compression continues in
the closing gap, high pressures and temperatures generate a linear zone
in which the rocks are metamorphosed, eventually welding the continents
together along a continental suture.


Forces associated with extension (spreading) or stretching in the Earth’s crust also produce
mountain ranges. Such forces occur where two plates are diverging or
moving apart. At the early stages of development this divergence can
lead to continental rupture where arching upwards and splitting of the
crust occurs. Along the line of divergence a rift valley develops with
the crack in the centre being continually filled with rising magma. Blocks on either side fall or slide down the side of the rift creating a mountainous landscape.





Description of the mountains as having deep roots and acting as anchorages:



  2 “And He has affixed into the earth mountains standing firm, 16850_250The modern theory of plate tectonics holds that mountains act as anchorages for
the earth’s crust. The crust is broken up into several tectonic plates
through cracks that range from 65 to 150 kilometers in depth; there are
about 12 large plates and several small ones. These plates, which
contain the world’s continents and oceans, float on hot, semi-molten
material, drifting and bumping against one another. Movement between the
plates occurs along a relatively narrow zone where plate tectonic
forces are most active i.e. in a weak zone of the earth’s crust. Thus
the movement of those plates floating on molten magma coupled with the
Earth’s movement around itself amount to a lot of force.




In
addition, as the ocean basin grows as the sea floor spreads, the magma
injected at the line of divergence creates a new mountain range called a
mid-oceanic ridge. Thus, the only factor that limits the ferocity of
the movement of the plates are the mountains that act as definite
stabilizers for the earth’s crust, safeguarding the continents and
oceans from constantly running into each other and not only does it
decrease their velocity, it also regulates their movement!




Modern
earth sciences have proven that mountains have deep roots under the
surface of the ground and that these roots are several times their
elevation above the surface of the Earth. We can thus safely conclude
that the Qur’an’s description is accurate;
the mountains are actually pegs in the earth’s weakest zones to anchor
it firmly in the same way that we use anchors to firmly pin ships to the
ground.




The link between the formation of mountains, rivers and paths:



  2 “And He has affixed into the earth mountains standing firm, 50911_250A
river is a flow of water along a channel from highlands to lowlands.
The great majority of rivers eventually discharge either into seas or
lakes, although some rivers disappear due to water loss through seepage
into the ground and evaporation into the air.




The
importance of rivers dwarfs their volumetric size (0.006 percent of all
the fresh water of the earth). This is because river water flows down
with gravity, giving it the power to mould the landscape through
erosion, transportation and the deposition of rocks and sediments,
making it a dynamic and renewable natural resource for human, plant, and
animal life. The water cycle begins when water evaporates from the
oceans into the atmosphere. Atmospheric water returns to Earth as
precipitation in the form of rain, hail or snow. The amount of water
reaching the ground depends on many factors but in general, highlands
receive more precipitation than lowlands and most rivers originate in
mountains. When precipitation reaches the ground, it usually seeps into
the soil, either percolating down to the water-table to become
groundwater, or flowing slowly downhill as through-flow. However, during
heavy storms, due to human activity compacting the soil surface or
covering it with concrete, or if the soil is already saturated, not all
the water is able to infiltrate and the excess collects on the surface
before flowing downhill to the nearest stream as overland flow. Water
that reaches the river either by through-flow or overland flow is termed
run-off. The role of the river in the water cycle is to complete the
cycle by collecting run-off from the surrounding area (drainage basin)
and carrying it back to the ocean or a lake in order to replace water
that has evaporated. At this point, we can guess the obvious connection between rivers and mountains explained to us in the Qur’an long ago.




However,
with the ever changing climate, rivers can eventually dry out leaving
their channels as pathways and roads for humans and animals alike to
use; this is the association the Qur’an
points out between rivers and roads. Rivers are the best means that
Allah created for pathways in otherwise inaccessible locations such as
mountains, hills and plateaus.




Conclusion



These
facts were unknown to man for a long time. He started to gather
information about nature and its mysteries slowly, but it was only in
the mid-nineteenth century that these explanations started to make some
sense and the bigger picture did not come into view until the mid 1960s.




The precise mention of such facts, is an assertion that the Noble Qur’an cannot be man-made and bears witness to the Prophethood and the message of the seal of the Prophet (SAWS) who received it. It proves how the Prophet was connected to the revelation and taught by the Creator. This come in assertion to the words of Allah that can be translated as,
“And those to whom knowledge has come see that the (Revelation) sent
down to thee from thy Lord, is the Truth, and that it guides to the Path
of the Exalted (in Might), Worthy of all praise.” (Surat Saba' (Sheba): 6).



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الرجوع الى أعلى الصفحة اذهب الى الأسفل

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مُساهمة من طرف حُ رُوفُ الْـآبْدَآع الأحد 15 يوليو - 15:22:22

بَآرَكْ الله فِيكْ
مَوْضُوعْ مُمَيَزْ
نَنْتَظِرْ الْمَزِيدْ مِنْ آبْدَآعَآتْكْ
تَقَبَلْ مُرُورِي



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مُساهمة من طرف الزعيم السبت 11 أغسطس - 21:58:19


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مُساهمة من طرف أبو سليمان الجمعة 5 أكتوبر - 19:21:04


أبو سليمان
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