
Child labour in Pakistan on the rise a year after devastating floods - Asia, World The 2010 monsoon floods submerged Pakistan on an unprecedented scale, with 10 years' worth of rain falling in the space of a week. Two thousand people were killed and another 20 million affected. Two million homes and 10,000 schools were destroyed. In a report released today, the UK-based charity Save the Children warns that the number of children forced to work has risen by up to a third in areas worst hit by the floods. "A year on from the floods and many of the children caught up in the disaster are struggling to survive," said David Wright, Save the Children's country director for Pakistan. The spike in child labour comes as families have watched their incomes fall by up to 70 per cent over the past year, the report said, drawing on a survey of over 2,300 households in the worst flood-affected areas. With incomes at perilous lows, the 10 million children in flood-affected areas are also being denied the food they need to survive. "Pakistan needs to act now.
Indo-European languages The Indo-European languages are a family of several hundred related languages and dialects. There are about 439 languages and dialects, according to the 2009 Ethnologue estimate, about half (221) belonging to the Indo-Aryan subbranch.[2] It includes most major current languages of Europe, the Iranian plateau, and the Indian Subcontinent, and was also predominant in ancient Anatolia. With written attestations appearing since the Bronze Age in the form of the Anatolian languages and Mycenaean Greek, the Indo-European family is significant to the field of historical linguistics as possessing the second-longest recorded history, after the Afro-Asiatic family. Indo-European languages are spoken by almost 3 billion native speakers,[3] the largest number by far for any recognised language family. Etymology[edit] History of Indo-European linguistics[edit] Franz Bopp, pioneer in the field of comparative linguistic studies. Gaston Coeurdoux and others made observations of the same type.