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شہید کی جوموت ہے وُہ قوم کی حیات ہے

شہید کی جو موت ہے وہ قوم کی حیات ہے
زندگی تو گزر جاتی ہے، جو زندہ ہے اُس نے بالآ خرسفرآخرت کرنا ہے، جو سانس لے رہا ہے اُس نے جان، جان آفریں کے سپرد کرنی ہے، کوئی بستر مرگ پر ایڑیاں رگڑ رگڑ کر مر جاتا ہے، کوئی کسی ڈوبنے والے کو سہارا دیتے ہوئے خودلہروں کے سپرد ہو جا تا ہے۔ کوئی مزمّن بیماری کا شکار ہو کر حکیموں اور ڈاکٹروں کے نسخے استعمال کرتے ہوئے داعی اجل کو لبیک کہہ دیتا ہے۔ کوئی راہزن کے ہتھے چڑھ کر اپنے بچوں کو یتیم اور اپنی زوجہ کو بیوہ کر جاتا ہے۔ لیکن قابلِ صد افتخار ہیں وہ لوگ جو ملک و ملت کی خاطر سرحدوں کی حفاظت کرتے ہوئے دشمنوں کی توپوں کا نشانہ بنتے ہیں اور جامِ شہادت نوش کر لیتے ہیں۔شہید کوقرآنِ پاک میں بھی زندہ فرمایا گیا ہے بلکہ یہاں تک فرمانِ باری تعالیٰ ہے کہ انہیں مردہ گمان بھی نہ کرو، خودتو زندہ ہیں ہی لیکن موت کا ظاہری لبادہ اوڑھ کر اور نظروں سے دائمی اوجھل ہو کر قوم و ملت کو حیات ِنو کی نوید سنا جاتے ہیں ، شہید کی زندگی قوم کی حیات ہے۔ شہید بحثیت مجاہد سرحدوں کی حفاظت کرتا ہے، سرحدوں پر پہرہ دیتاہے، اقوام خوابِ خرگوش کے مزے لے رہی ہوتی ہے اور شہید توپوں کی گھن گرج میں رات کی ساعتیں گزار رہا ہوتا ہے۔ شہادت ایک زیور ہے، جس کے زیب تن کرنے سے جسمانی خدوخال کے علاوہ روحانی نکھار بھی آجاتا ہے۔ شہید اپنی قوم کے عروج میں کلیدی کردار ادا کرتا ہے۔
قوم اس وقت اپنے مستقبل کی درخشندگی کے لیے مستعد ہوتی ہے جب وہ ذہنی طور پر آسودہ ہو، فکری اعتبار سے توانا ہو اور اس قسم کے ماحول کی تشکیل کے لیے شہید کا وجود...

پاکستان میں جبری شادیوں كے اسباب و محرکات

Before the advent of Islam, a woman was considered as property, with no rights at all. They did not have the right to choose a husband. Islam liberated women and gave them the basic rights. Unfortunately, in Pakistan many parents and legal guardians misinterpret and misuse the guardianship of their children, especially with reference to marriage. They deny some religious rights to their children because of local traditions, customs and taboos. Forcing children to marry against their wishes, does not conform to the Islamic code. Forced marriages are considered illegle in Shariah. Even in the case of marriage of a minor arranged, by a father or a grandfather, the girl has the right to cancal it on reaching Puberty. According to Shariah the boy and the girls has the right to turn to a court for a settlement of the issue.

Geophysical Characterization of Late Quaternary Basin Deposits and Hydrogeophysical Modelling of Lakki Marwat and Domail Plains, Khyber Pakhutunkhwa, Pakistan

The understanding of depositional setting, the aquifer properties and the groundwater flow within an intermontane basinis of great significance for groundwater abstraction and monitoring. Among different intermontane basins developed in northwestern Himalaya, Pakistan, the Bannu Basin is very important and is filled with Quaternary sediments. The electrical resistivity data was acquired, processed and interpreted in two separate plains of the Bannu Basin, i.e. the Lakki Marwat Plain and the Domail Plain. The Domail Plain lies in the eastern section of the Bannu Basin whereas the Lakki Marwat Plain is located in the western half. Through a combination of geostatistical analysis, geophysical inversion and visualization techniques it is possible to re-model and visualizes the single dimension resistivity data into 2D and 3D spaces. Variogram models are utilized to extend the interpretation of the data and to distinguish individual lithological units, as well as the occurrence of saline water within the subsurface. As such the alluvial system of the intermontane basin has formed during episodes of local tectonic activity with fluvial erosion and deposition yielding coarse sediments with characteristically high electrical resistivities near to the mountain ranges and finer sediments of medium to low electrical resistivities towards the basin center. The regional and local tectonic activity has caused a considerable amount of faulting in the rocks as well as depressions which over time, have been filled with clay-silt sediments typical of lacustrine and flood plain environments. Streams arising in the adjacent mountains have eroded these sediments leaving gravel–sand deposits in channels. It is concluded that these sediments have been deposited in several different depositional settings including prograding fan shaped bodies, flood plains, sandy plain and lacustrine deposits. The depositional setting of the sediments influences the groundwater flow movements within the plains. The work was further extended to estimate the aquifer properties utilizing vertical electrical sounding (VES) and pumping test data sets acquired in the Lakki Marwat and Domail Plains of Bannu basin. The sediments in the alluvial fan zones are characterized by low gamma ray values which suggest low levels of fine sediments. This is in contrast to the sandy plain and lacustrine zones where higher gamma ray values suggest higher contents of the finer material. The alluvial fan zones have the maximum transmissivity in the area, while the sandy plain and lacustrine zones exhibit very low transmissivities. This indicates a higher concentration of finer material within the sandy plain and lacustrine zones with the absence of the recharge boundaries, thus reducing the effective water transmission. The steady state groundwater flow pattern roughly follows the resistivity patterns within the aquifer system and generally flow towards the Gambila River within the Lakki Marwat Plain. The water flow is regular and uniform within the higher resistivity zones, whereas the flow patterns in the lower resistivity zone representing the lacustrine environment is generally retarded. The water table has a steady rise in the lacustrine zone due to the less transmission of water in the lacustrine zone. The correlation between resistivity zones and the groundwater flow in Domail Plain is difficult to establish, because a considerable portion of the subsurface has been masked by saline water. In this plain groundwater flows steadily towards the Kurram River roughly follow the topography of the plain. The regional trends in the depositional systems in conjunction with the groundwater flow patterns identify the prospective groundwater development zones within the subsurface. The prospective zones identified within the basin when evaluated further would help in management of the important groundwater resource within the region. The regional scale interpretation of seismic, well logs and electrical resistivity data sets highlight the tectonic activity in the region resulted in the formation of northwestern Himalayan fold and thrust belt and the associated intermontane basins.
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