between 2005 and 2010, an annual population growth of 7.9%. All villages are listed in the following table, with the preliminary census results of 2005, counterclockwise around the perimeter of the atoll, starting in the northeast with Abaiang and ending in the southeast with Onauea. Tangkore is near the westernmost point of Teraina: Teraina has an unusual age structure; nearly half the population (44%) is aged under 15 and one in five people (19%) are children under five years. There are more males than females in almost all age groups except the elderly. Physical geography As regards its physical characteristics, this is one of the most interesting islands in the Pacific. It is a raised coral atoll, but it has not filled up with sand and soil, yet still retains a significant remnant of the former lagoon. The lake, however, is only just barely perceptibly brackish, as its only significant source is the plentiful rain. The lake is only a few feet (around 1–2 meters) deep for the most part, though the supposed maximum depth is nearly . Being only about away from the equator, Teeraina is inside the ITCZ; its climate is thus extremely humid, making it one of the "wet" Pacific islands. The western inland is made up by peat bog, which is still flooded after heavy rains, and constitutes infilled former lakebed. It is not clear in what way the western lake or lakes – there are now 2 main areas of bogland, which may correspond to former lake basins – were connected to the remaining waterbody. One bog is immediately adjacent to the lake's western end, the other is halfway between that and the island's northwest tip. Canals have been cut into the bogs, for punting, rowing and motor boats transporting people and produce. There is some removal of peat and sediments to stem the lake's ongoing infilling; in addition it seems that in recent times, the lake's level is slowly rising again so that the eastern bog's area has receded somewhat. The peat reaches thicknesses of about , much of which is located above sea level. It is also not precisely known where the last connection of the inland waters to the ocean were, and when they closed. The southeast end is more likely however, as the island is in the Equatorial Counter Current which runs west to east, and drifting coral and other reef-builder