Did the maya perform exhumation in jaina island?4 answersThe Maya did perform exhumation in Jaina Island. The site of Jaina Island is unique due to its specially developed burial culture involving ceramic figurines. These figurines are found in graves, unlike other Maya sites where they are mostly found in domestic contexts. The exhumation process in Jaina Island is believed to have been performed by the formation of a D2 extrusion wedge made up of metamorphic rocks. This wedge had a subduction thrust as its base and a detachment fault as its roof. The exhumation was related to the Eocene ridge subduction, which caused a high thermal gradient during ridge subduction and resulted in the exhumation of the metamorphic rocks.
Where do people exhume the bones of their ancesters?5 answersPeople exhume the bones of their ancestors in various locations such as burial grounds, home courtyards, open land, ditches, rubbish dumps, and even during excavations for new constructions.
Where in the americas people exhume the bones of their ancesters?4 answersExhumation of ancestral bones is practiced in several countries in the Americas. In Latin America, exhumation processes have been carried out in Guatemala, El Salvador, Colombia, Peru, Chile, Argentina, Uruguay, Brazil, Paraguay, Venezuela, Mexico, Panama, Ecuador, and Honduras. These exhumations are a result of various events such as collective massacres, state policies leading to disappearances, collective violence, and selective deaths under democratic regimes. The exhumation process in Latin America is seen as a part of transitional justice and has implications for the social and political life of these exhumed corpses in post-conflict societies. In North America, repatriation of American Indian bones from museums, universities, and historical societies is a major concern for tribal groups. The repatriation issue arises due to differing cultural concepts of the body and has gained prominence recently.
How can we automate the discovery of metamorphic relations?5 answersAutomating the discovery of metamorphic relations can be achieved by extracting and generalizing encoded metamorphic relations from existing test cases in open-source software projects. This approach has been proposed in papers by Xu et al.and Müller et al.. The proposed method, called MR-Extractor, identifies test cases that encode metamorphic relations in open-source software and then generalizes these relations into parameterized methods for metamorphic testing. The reusability of these codified metamorphic relations for new test generation is validated. Experimental results show that MR-Extractor can identify a significant number of metamorphic relation-encoded test cases and that test cases constructed from these relations can effectively improve test coverage. The approach has been evaluated in various domains, including computational material scienceand query-based systems.
How fast can we search ?5 answersThe speed at which we can search depends on various factors such as the efficiency of the search algorithm, the size of the dataset, and the computational resources available. Efficient search algorithms, such as binary search or hash-based search, can significantly reduce the search time by quickly narrowing down the search space. Additionally, parallel processing techniques can be employed to distribute the search workload across multiple processors or machines, further improving search speed. The size of the dataset also plays a crucial role, as larger datasets require more time to search through. Finally, the computational resources available, such as processing power and memory, can impact search speed. With more powerful hardware, searches can be performed faster. Overall, the speed of searching is a complex interplay between algorithm efficiency, dataset size, and available computational resources.
What is the rate of plate tectonics movement?4 answersThe rate of plate tectonics movement is steady and can be measured over several years or several million years. Recent studies of the motion of the Pacific and North American plates suggest that plate tectonic motion averaged over these time scales is consistent. The speed of plate movement can be deduced through analysis of magnetic anomalies above mid-ocean ridges, where the direction of the geomagnetic field is frozen into the crust formed by cooling magma. Rates of motion are determined by the spacing between dated magnetic highs and lows. Additionally, plate tectonic reconstruction approaches can extract time-dependent plate velocities and geometries, providing a median root mean square (RMS) plate speed of approximately 4 cm/yr over 200 million years. The motion of oceanic plates tends to be 2-3 times faster than continental plates, and plates with large continental fractions have slower RMS velocities.