Sar-qoflī in the Customs and Laws of Modern Iran: The Emergence of Haqq-e Kasb o Pīshe o Tejārat and the Evolution of the Shop-lease Contract System

In the shop-lease contract with sar-qoflī, which is a widely practiced form of lease contract in today's Iran, a lessor of a shop sells to a hirer a right called sar-qoflī which amounts to almost as much as the entire value of the shop's ownership, while obtaining a monthly rent of only small value. This peculiar form of contract was brought into existence based on a new right called “haqq-e kasb o pīshe o tejārat,” that emerged as a result of the blending of traditional customary practice relating to real estate leasing with Anglo-American value concepts. The adoption of this right, causing as it did the lessor's responsibility for compensation for the value of the usufructuary right, drastically changed the relationship between lessors and hirers in Iran.     

Geomorphic reconstruction of formation and recession processes of waterfalls of the Kaminokawa river basin on Osumi Peninsula,southern Kyushu,Japan

To assess the geomorphological importance of waterfall recession in volcanic bedrock, we examined recession rates of six waterfalls in the lower reaches of Kaminokawa river basin on the Osumi Peninsula in southern Kyushu. The examination was performed with an empirical equation that uses a dimensionless parameter obtained by dimensional analysis of relevant measured factors, including erosive force, size of waterfall, and bedrock resistance. Welded Ata ignimbrite, formed at approximately 110 ka, may have played an initiating role to maintain such waterfalls because it resists weathering more than other local rocks. Estimated recession rates for the six waterfalls range from 0.2 to 3.0 cm/y, which compare with estimated rates for waterfalls in another region characterised by welded ignimbrite. Comparison of equation‐derived recession rates of waterfalls with actual recession distances from confluences supports the idea that an original waterfall will subsequently split into two distinct waterfalls when it recesses past an upstream junction of two channels. Our findings revealed that all six waterfalls likely would have been at almost the same point lower in the watershed in the past, marking the general site of the original waterfall. Moreover, the ancestral original waterfall is highly likely to have started from a point between the caldera rim and present river mouth. There, a knickpoint was likely caused by the river dropping into an inner part of the caldera, possibly just after the eruption of the Ata ignimbrite. The waterfall erodes upstream away from the caldera basin, and this happens to be to the east.     

Transitions in Islamic plant-ash glass vessels: on-site chemical analyses conducted at the Raya/al-Tur area on the Sinai Peninsula in Egypt

This study focuses on the chemical composition of Islamic plant-ash glass (dated from the 9th to 11th centuries) excavated from the Raya/al-Tur area on the South Sinai in Egypt. Plant-ash glass objects from the Raya site were classified into three compositional types based on on-site chemical analyses with a portable X-ray fluorescence spectrometer. Based on typological characteristics and chemical composition comparisons with contemporary glass objects from other Islamic sites, one hypothesis holds that plant-ash glass objects produced in the Syria–Palestine or Mesopotamian regions could have been imported to Raya during the 9th to 10th centuries. In particular, some colorless glass vessels with a high magnesium/calcium ratio were noted to exhibit post-Sassanian cut decorations. Conversely, most of the bluish-green plant-ash glass objects from the Monastery of Wadi al-Tur near the Raya site exhibited relatively high levels of aluminum, titanium, iron, and lead. These pieces were likely produced during the Fatimid period (late 10th to 12th centuries), and based on their elemental composition, possibly originated in Egypt. The present work provides a greater understanding of chronological changes in post-9th century Islamic plant-ash glasses and the development of social and commercial networks within the Middle Eastern area.     

From Atomic Fragments to Memories of the Trinity Bomb: A Bridge of Oral History over the Pacific

This paper first introduces the background of the making ofMemories of the Trinity Bomb, a Japanese documentary film basedon the book Atomic Fragments: A Daughter's Questions, authoredby Mary Palevsky. Yoshihiko Muraki, an independent filmmaker,revealed his unique approach in filming the spiritual journeyof Mary, a daughter of the Manhattan Project scientists, inher search of the true meaning of the atomic bomb. While thedocumentary primarily focused on the narratives of Mary Palevskyand several Project scientists, this paper introduces Japaneseperspectives on the film through interviews with Japanese viewersvarying both in generation and background. Through this endeavor,the paper explores the meaning of this trans-media as well astransnational collaboration on the topic of the atomic bomb,which remains at the crossroads of history and personal memories.     

Reck,Christiane, Mitteliranische Handschriften Teil I: Berliner Turfanfragmente manichäischen Inhalts in soghdischer Schrift. [Verzeichnis der Orientalischen Handschriften in Deutschland Band XVIII, 1].

Indo-Iranian Journal -     

Long‐term stability of fracture systems and their behaviour as flow paths in uplifting granitic rocks from the Japanese orogenic field

In granitic rocks, fracture networks typically provide pathways for groundwater flow and solute transport that need to be understood to assess the long‐term performance of deep underground storage or disposal facilities such as radioactive waste repositories. However, relatively little is known about the long‐term processes of fracturing and/or the longevity of flow paths (FP) in granitic rocks distributed within orogenic belts. To clarify these issues, Japanese plutons of different ages and in situ fractures in granite at the Mizunami Underground Research Laboratory (MIU) located in central Japan were studied. Detailed structural characterization and geochemical analysis of in situ fracture fillings sampled from a depth of 300 m were carried out to clarify the relationship between fracturing and mineral infilling processes. Different plutons show identical episodes of fracturing and fracture filling, consisting of: brittle tensile fracturing, due to decreasing temperature through the ductile–brittle transition after plutonic intrusion (Stage I); relatively rapid uplifting (ca. a few mm/year) accompanied by hydrothermal water circulation, which produced uncrushed layered mineral fillings (Stage II); and a period of low‐temperature meteoric water circulation following exposure after uplift (Stage III). The parageneses of carbonate mineral fracture fillings and their carbon isotopic compositions (¹⁴C, δ¹³C) show that there were distinct episodes of carbonate mineral precipitation during the rapid uplifting of a pluton. The carbonate minerals that formed during each episode incorporated carbon from a distinct source. The evolution of fillings identified here enables development of a specific model of fracturing and persistence of fluid‐conducting systems in the plutons of the orogenic field.