The current article starts by studying the viewpoints of religious scholars and clerics about art and particularly theatre due to the fact that religion and religious beliefs play an important role in our society. It then discusses theatrical activities in the city of Qom. This part of the article is divided into 5 historical periods: 1- Before 1975 Theatrical activities were mainly restricted to performances in schools for special occasions. 2- 1975 to 1978- The theatre of Qom gained a special position in the country with the establishment of theatre groups outside schools and the participation of these groups in theatre festivals. 3-1978 to 1981- Various active groups interested in the art of theatre were established and held performances in the city. 4-1981 to 1996- Various art and culture organizations including the Institution for Culture and Islamic Guidance, the Qom Seminary Office for Information Dissemination and the Arts Assembly of the Islamic Information Dissemination Organization embarked on theatrical activities. During this period the theatre of Qom became active in various festivals. 5-1996 to 2003- A provincial theatre festival was held in Qom. The performances found their way to 10festivals outside the country and the number of theatre graduates reached a total of 51. In the end the article presents statistics of theatrical activities in Qom as a means to reach a conclusion.

Since Qom is one of the historic cities of Iran and the center of the world of Shiate, recognition of its historic structure and the conditions of its creation as a model both for a city in ancient Iran and for an Islamic city is of prime significance.Despite the valuable researches conducted by Engineer Ahmad Saeednia and Marcelle Bazen about Qom, there have remained some obscurities in its historic survey. This article tries to clarify the ambigeous points about the cration of Qom referring to historic noble resources. Therefore, regarding the refutation of Marcelle Bazen and Ahmad Saeednia’s theory about creation of Qom, a short survey on different periods of the history of Qom is necessary. The writer believes that Qom was a big and thrivingcity and was ruined several times due to historic events during the history.

This research has described for determinate of Oligo-Miocene Foraminifers at the Do Baradar section. The main aim project was scrutiny age of this Formation and Paleoecology distribution lot of basins have created with big streams between Zagros andAlborz with Central Iran. Final transgressive sea on the Rupelian to Late Miocene have created the continue sediments consist low depth Lime stone and Marls. These sediments have complete different colors and lithology have named Lower Red Formation and Upper Red Formation and total Qom Formation. In this section the thickness of Qom Formation is 830 Meters that 8 units can separate of Marls and Limestone. From the Limestone have collected a lot of Samples and on Marls have samples isolate Foraminifers. The result of this research have been showing: The Central Iran Sediments on the Rupelian to Burdigalian have a warm climate (Tropical) to sub warm (Subtropical) climate with restrict marine environment but continue to open sea. The depth on Oligo-Miocene was different and have swing.

Because of neighborhood with Tehran as capital city, Qom was as a shelter and sanctuary for the various political personalities of Qajar period and however had no importance for political situation but held prominent station because of the presence of the hazrat-e Ma'soumah holy shrine (salamollah alayha) and centrality of shia clergymen. Thereupon, Qom changed to main point against Qajar autarchy, during Constitutional Revolution and migration of clergymen to this city.The presence of clergy scholars in Qom due to coming and going of the political figures and remit of variant telegraphs between Tehran and Qom and increased people's complaint against residential landlords and influentials significant injustice and the people's confrontation against these cruel dictators of whom one was "Motawallibashi". Also implementation of oration against the Qajar reign in the hazrat-e Ma'soumah holy shrine was the most important event at that time that played an effective role for development of Iranian people in contrast to obsolutism and the establishment of Constitutional (Mashrooteh) system.After distributing of constitutional ordinance Qom people continued to their political participation like too many of the country provinces and they formed multiple of syndicates and political societies that had many effects on social and political evolutions of this city after their own deputy selection in the assembly.

The intracotinental Qom- Aran depression basin is located in the central Iran zone and correlated with its tectonic environment. Some of the depression basins such as Qom- Aran, Aredstan- Yazd and Rafsanjan- Zarand basins show NW-SE trend and are located between two subordinate uplifted subzones of the central Iran zone (mid triangle subzone in the north and Urumiyeh-Dokhtar volcanic belt in the south). From Urumiyeh- Dokhtar magmatic subzone toward middle parts of central Iran zone, There are various subordinate trends and morphostructures, Probably due to the affected stress and the reflection of brittle behaviour of the central Iranian crystalline basement, that have produced faulted and rotated blocks with different forms and dimensions as well as the compexity of the morphostructures. Therefore, In the Qom-Aran depression basin, there are three structural trends, NW-SE, SW (Davazdah Emam-Narreh khar kuh fault) NNW- SSE (Qom-Raband Zefreh - fault) and NE-SW (Maranjab fault) .During the Neogene, spreading of the Red Sea and movement of Arabian Plate to the north produced compressional stress in the Iranian platform. Strike- slip movenents of Central Iranian blocks caused some local extensional movements, such as a long the bended part of Qom- Zefreh fault, and as a result the Qom- Aran pull - a part basin was formed. In the later phases a huge amount of continental facies sediments of the Upper Red Formation and related M1, M2 and M3 members deposited in this basin. The above mentioned deposits are originated by erosion of surrounding uplifted areas. The latter form reliefs which bounded mainly with reverse fault are located in the margin of the Qom-Aran depression basin. In the late Neogene the continuation of the Red Sea spreading and related compressional stress to the north, caused an anticlock rotational movement of the Qom-Aran block. According to this structural evolution some NE-SW trends (Maranjab Fault) are activated so that, the trend of Maranjab Fault shows 75 degree divergence to the Qom-Ravand - Zefreh faults ternd. All structural evidences indicate an extentional movement along the bended parts of the Qom-Ravand - Zefreh strike - slip fault and consequently the formation of the Qom-Aran pull- apart basin. On the other hand, the folding of Upper Red Formation deposits with axial NW-SE (Alborz and Sarajeh anticline) and E-W trends (Qaleh Sadar Anticline) in the border of Qom- Aran depression indicate the limitation of basin dimension due to the oblique convcergence of southern sub- block in eastern part of the depression which has proouced a narrow folded area in the Qaleh Sardar area. The above mentioned rotational movements are in agreement with geophysical and microseismic data, and resulted the structural subdivisions of the area into active (Maranjab) - Passive (Yakhab), captured (Daryacheh-ye -Namak) and isolated (daryacheh-ye - Hozsoltan) blocks.