Context: Death from laughter is a rare form of death, usually resulting from cardiac arrest or asphyxiation, caused by a fit of laughter. Instances of death by laughter have been recorded from the times of ancient Greece to the modern day.
 Question: can you have a heart attack from laughing Context: A deed in lieu of foreclosure is a deed instrument in which a mortgagor (i.e. the borrower) conveys all interest in a real property to the mortgagee (i.e. the lender) to satisfy a loan that is in default and avoid foreclosure proceedings.
 Question: is a deed in lieu the same as foreclosure Context: Several paleontologists suggest the possibility of two separate brown bear migrations: inland brown bears, also known as grizzlies, are thought to stem from narrow-skulled bears which migrated from northern Siberia to central Alaska and the rest of the continent, while Kodiak bears descend from broad-skulled bears from Kamchatka, which colonized the Alaskan peninsula. Brown bear fossils discovered in Ontario, Ohio, Kentucky and Labrador show the species occurred farther east than indicated in historic records. In North America, two types of the subspecies Ursus arctos horribilis are generally recognized--the coastal brown bear and the inland grizzly bear; these two types broadly define the range of sizes of all brown bear subspecies.
 Question: is a grizzly the same as a brown bear Context: In the original novel and Jackson's adaptation, it is implied that Saruman promised her to Gríma as payment for his services as a spy. In one scene, while mourning for her dead cousin, she is subjected to Gríma's obnoxious affections, which she spurns. She sings the dirge at Théodred's funeral. In the extended edition of The Two Towers, Éowyn is shown discovering, to her astonishment, that Aragorn is a long-lived Dúnadan. In the original theatrical release of The Lord of the Rings: The Return of the King, Éowyn plays a much larger role in the Battle of Pelennor Fields than in the book, where the only fighting mentioned is her conflict with the Witch-king and also Gothmog. Her speech revealing her identity is cut, replaced with the simple declaration ``I am no man!'' She also replaces Merry as the person to sit with Théoden as he dies. In the Extended Edition of the film, Éowyn is portrayed as being near death following her fight with the Witch-King; her brother finds her and screams in anguish because he fears that she is dead. She is later seen being healed by Aragorn, and meeting Faramir in the Houses of Healing.
 Question: does eowyn die in return of the king Context: The femoral artery is a large artery in the thigh and the main arterial supply to the leg. It enters the thigh from behind the inguinal ligament as the common femoral artery, a continuation of the external iliac artery. Injuries to the femoral artery can require reattachment surgery.
 Question: are there any main arteries in your thigh Context: In the late Cretaceous, approximately 100 million years ago and subsequent to the splitting off from Gondwana of conjoined Madagascar and India, the Indian Plate split from Madagascar. It began moving north, at about 20 centimetres (7.9 in) per year, and is believed to have begun colliding with Asia as early as 55 million years ago, in the Eocene epoch of the Cenozoic. However, some authors suggest that the collision between India and Eurasia occurred much later, around 35 million years ago. If the collision occurred between 55 and 50 Mya, the Indian Plate would have covered a distance of 3,000 to 2,000 kilometres (1,900 to 1,200 mi), moving faster than any other known plate. In 2012, paleomagnetic data from the Greater Himalaya was used to propose two collisions to reconcile the discrepancy between the amount of crustal shortening in the Himalaya (~1300 km) and the amount of convergence between India and Asia (~3600 km). These authors propose a continental fragment of northern Gondwana rifted from India, traveled northward, and initiated the ``soft collision'' between the Greater Himalaya and Asia at ~50 Ma. This was followed by the ``hard collision'' between India and Asia occurred at ~25 Ma. Subduction of the resulting ocean basin that formed between the Greater Himalayan fragment and India explains the apparent discrepancy between the crustal shortening estimates in the Himalaya and paleomagnetic data from India and Asia.
 Question: did any subduction occur during the collision of india and asia
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