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Geography is the science that studies the lands, the features, the inhabitants, and the phenomena of the Earth. A literal translation would be "to describe or write about the Earth". The first person to use the word "geography" was Eratosthenes (276–194 BC). Four historical traditions in geographical research are the spatial analysis of the natural and the human phenomena (geography as the study of distribution), the area studies (places and regions), the study of the human-land relationship, and research in the Earth sciences. Modern geography is an all-encompassing discipline that foremost seeks to understand the Earth and all of its human and natural complexities—not merely where objects are, but how they have changed and come to be. Geography has been called "the world discipline" and "the bridge between the human and the physical science". Geography is divided into two main branches: human geography and physical geography.

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Surtsey eruption 1963.jpg
Surtsey ( Icelandic, meaning " Surtr's island") is a volcanic island off the southern coast of Iceland. At 63°18′11″N 20°36′17″W / 63°18′11″N 20°36′17″W / 63.303; -20.6047 Surtsey is the southernmost point of Iceland. It was formed in a volcanic eruption which began 130 metres (426 ft) below sea level, and reached the surface on 15 November 1963. The eruption lasted until 5 June 1967, when the island reached its maximum size of 2.7 km2 (1.0 sq mi). Since then, wind and wave erosion have caused the island to steadily diminish in size: as of 2002, its surface area was 1.4 km2 (0.54 sq mi). The new island was named after Surtr, a fire jötunn or giant from Norse mythology. It was intensively studied by volcanologists during its eruption, and afterwards by botanists and biologists as life forms gradually colonised the originally barren island. The undersea vents that produced Surtsey are part of the Vestmannaeyjar (Westmann Isles) submarine volcanic system, part of the fissure of the sea floor called the Mid-Atlantic Ridge. Vestmannaeyjar also produced the famous eruption of Eldfell on the island of Heimaey in 1973. The eruption that created Surtsey also created a few other small islands along this volcanic chain, such as Jólnir and other, unnamed peaks. Most of these eroded away fairly quickly.

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Albert Stanley, 1st Baron Ashfield
Albert Stanley, 1st Baron Ashfield was managing director, then chairman of the Underground Electric Railways Company of London (UERL) from 1910 to 1933 and chairman of the London Passenger Transport Board (LPTB) from 1933 to 1947. At a young age, he held senior positions in the developing tramway systems of Detroit and New Jersey. In 1907, his management skills led to his recruitment by the UERL, which was struggling through a financial crisis. He quickly integrated the company's management and used advertising and public relations to improve profits. As managing director of the UERL from 1910, he led the take-over of competing underground railway companies and bus and tram operations to form an integrated transport operation known as the Combine. He was Member of Parliament for Ashton-under-Lyne from December 1916 to January 1920 and was President of the Board of Trade between December 1916 and May 1919. He returned to the UERL and then chaired it and its successor the LPTB during the organisation's greatest period of expansion between the two World Wars, making it a world-respected organisation considered an exemplar of the best form of public administration.

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Nile Delta
Credit: Jacques Descloitres, MODIS Rapid Response Team, NASA/ GSFC

The Nile Delta is the delta formed in Northern Egypt where the Nile River spreads out and drains into the Mediterranean Sea. It is one of the world's largest river deltas—from Alexandria in the west to Port Said in the east, it covers 240 km of Mediterranean coastline—and is a rich agricultural region. From north to south the delta is approximately 160 km in length. The Delta begins slightly down-river from Cairo.

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