ARCHIVE // PW // TIME-SERIES
Terrain
Palau — 33 years of data
Historical Values
| Year | Value |
|---|---|
| 1993 | about 200 islands varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 1994 | about 200 islands varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 1995 | about 200 islands varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 1996 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs lowest point: Pacific Ocean 0 m highest point: Mount Ngerchelchauus 242 m |
| 1997 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 1998 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 1999 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2000 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2001 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2002 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2003 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2004 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2005 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2006 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2007 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2008 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2009 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2010 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2011 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2012 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2013 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2014 | varying geologically from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2015 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2016 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2017 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2018 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2019 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2020 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2021 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2022 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2023 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2024 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |
| 2025 | varying topography from the high, mountainous main island of Babelthuap to low, coral islands usually fringed by large barrier reefs |