Knowledge

Geography of Palau

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on the volcanic islands where poor drainage conditions exist. Distinctive forest communities are found on the atolls, the rock islands and on the platform islands. Included in these communities is the casuarina forest with the needle-bearing ironwood tree (ngas)." In addition to the forest associations on the volcanic islands are large areas of grasslands and savanna . The grassland/savanna association accounts for 16% of the total area of Palau (6,783 hectares out of a total of 41,619) and most (99%) of this association is found on Babeldaob Island . While some of this association is the result of human activity, at least a portion of the association is found on poor soils. In
1178: 502:, usually blowing from December to July bring frequent rains and often a slightly drier time from February through April. The southwest trade winds are often associated with more violent storms. Although the Palau Islands are outside of the main typhoon zone, several damaging typhoons have struck the islands. The mean annual temperature is 27 °C, with a range in variation of less than 4 °C from the coolest months, January and February, to the warmest month, April. The daily variation averages only 6 °C. The humidity is very high, averaging 82% annually. 1164: 1074: 1112: 1137: 1098: 307:
levels of natural terraced benches have been recognized. One bench is 1 m to 2 m above mean sea level, while a second, and much broader, bench is 5 to 10 m above mean sea level. Many villages on Babeldaob Island are built on this second bench. Geologic data indicate that Babeldaob Island has undergone a net uplift of land relative to sea level of about 2 m in the last 4000 years; thus, for most of the Palau coastline, submerged habitation sites in
1062: 1152: 1086: 26: 1451: 1430: 1406: 291:. Weathered material from exposed upper parts of the volcanic islands was eroded away and accumulated in shallow coastal waters forming deposits of clay. The substrata of the volcanic islands are volcanic breccias and tuffs, some flow material, conglomerates, and related sediments. The sediments are extensively lateritic clays and are strongly acid. The 986:, and the coconut plantation associations. These four forest communities include a wide variety of food producing species in tree gardens or kitchen gardens. Interspersed throughout these food producing forest associations are areas of cropland and urban development. The important resources of the food producing forest associations include 949:
The volcanic islands contain heavily eroded hills reaching heights of 250m above sea level, while the rock islands and atolls vary in elevation from sandy relict beaches a few meters above sea level to jagged limestone hills more than 200m high. The islands all are covered with dense stands of mixed
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range from 81 to 86 °F (27 to 30 °C) throughout the year. Subsurface temperatures to about 320 ft (100m) rarely fall below 79 °F (26 °C). Below this depth, the temperature drops quickly to less than 50 °F (10 °C) at approximately 590 ft - (180m). The constant heating of
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where the terrain is level, especially surrounding the volcanic islands but also including large portions of Beliliou Island. These forests serve to hold eroding soil from washing into the lagoon and thus provide a natural buffer to protect the lagoon. The swamp forest is also found in upland areas
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Island are made up of Palau limestone. The limestone is raised coralline reef structure which formed in the warm tropical waters during Miocene to Pleistocene times. Surrounding the volcanic islands are natural terraced benches resulting from sea level changes and uplifting of the Palau ridge. Two
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island soils are well-drained, limestone island soils excessively so. Upland volcanic island soils range from nearly level to very steep and are fine-textured, while bottom land soils are poorly drained or saturated. Limestone island soils may be either level, deep and sandy or steep, shallow and
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to low, coral islands usually fringed by large barrier reefs. Natural resources consist of forests, minerals (especially gold), marine products, and deep-seabed minerals. Current environmental issues include inadequate facilities for disposal of solid waste; threats to the
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the ocean surface in the tropics creates a highly-stratified temperature regime in the water column, with little mixing. This general regime may vary locally or seasonally, as in the case of the upwelling of cold subsurface waters along steep leeward islands slopes.
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According to the 1983 Soil Conservation Service survey (Smith, 1983), there are roughly 18 kinds of soils in Palau, exhibiting a wide variety of texture, drainage, depth and fertility characteristics. To paraphrase the survey's summary, upland volcanic and
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area of more than 1200 sq. km. Variations in soil type, elevation, and human activity have led to the development of distinctive plant communities. At present, only 75 % of the Palau Islands are forested, the rest being covered by
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tropical forest; in addition, the volcanic islands contain numerous areas of savanna and a broad belt of coastal mangrove swampland. An extensive barrier reef surrounds the central islands of the archipelago, forming a rich
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The relief of the country varies from the hilly main island of Babeldaob to the low, coral islands, usually bordered by large barrier reefs. Average altitude - no data available; the lowest point is the water level of the
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sand beaches, the rock island edges rise abruptly out of the water, forming steep cliffs. Distinctive geologic features of the rock islands are shear cliffs and a notch cut back into the cliff just above mean sea level.
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The Palau archipelago contains more than 250 islands and islets stretched along a 150 km north south trending arc in the western Pacific. Its center is located near 7° north latitude, some 650 km north of
336:(ECC, flowing west to east). The influence of the NEC is strongest between November and May, when the trade winds prevail, and the ECC predominates the rest of the year. The 498:(Tropical Rainforest Climate). It rains almost daily. Short but torrential storms provide over 3.8m annually. Prolonged dry spells or droughts are rare. The northeast 1381: 440: 1220: 261: 1202: 1213: 978:. On the lower slopes, especially around settlements, the upland forest association becomes mixed with four other forest communities including the 1923: 1177: 1891: 1244: 280:
The Palau Islands are composed chiefly of accumulated volcanic material and limestone. Geologists distinguish three geologic units of erupted
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Share of forest area in total land area, top countries (2021). Palau has the fifth highest percentage of forest cover in the world.
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This is a list of the extreme points of Palau, the points that are farther north, south, east or west than any other location.
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The climate of the Palau Islands is defined as being maritime tropical, characterized by little variation seasonally or
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are found on the volcanic islands' uplands and include a great diversity of species. The variety of trees includes
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and world-famous rock islands. The total land area is 459 km (177 sq mi). It has the 42nd largest
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consists of eight principal islands and more than 250 smaller ones lying roughly 500 miles southeast of the
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islands. These limestone islands, primarily situated in the archipelago center between
1286:"Australia - Oceania :: Palau — The World Factbook - Central Intelligence Agency" 2054: 2006: 1928: 1818: 1668: 1636: 1580: 1529: 1519: 883: 201: 1085: 1842: 1803: 1770: 1717: 1560: 1506: 1035: 463: 368: 281: 194: 1459: 1440: 1341: 1321: 1025:. Most cropland in Palau is divided into small garden areas. The swamp forest and 1788: 1698: 1026: 448: 308: 1858: 1808: 471: 452: 444: 1382:"Climatological Information for Palau Islands, Pacific Islands, United States" 1151: 2104: 1798: 1455: 1434: 1048: 963: 491: 467: 367:
The area of Palau is slightly more than 2.5 times the size of the US city of
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A preliminary wildlife management plan for the Republic of Palau vertebrates
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A preliminary wildlife management plan for the Republic of Palau vertebrates
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Terrain varies geologically from the high, mountainous main island of
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Most of the Republic of Palau lies within the influence of both the
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Important resources in the gardens include several species of targ
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This article incorporates text from this source, which is in the
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Snyder, David.; Adams, William Hampton; Butler, Brian M. (1997).
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Snyder, David.; Adams, William Hampton; Butler, Brian M. (1997).
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The rock islands, the platform islands and the eastern half of
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Several types of forest communities can be observed in Palau.
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loamy in areas where they are associated with rock outcrops.
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The geologically diverse archipelago is dominated by
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603,978 km (233,197 sq mi) (200 nmi)
1340:Freifeld, Holly.; Otobed, Demei O.; Palau. (1997). 229:, and near 134° east latitude, some 900 km east of 1438: 1319: 340:lie more deeply within the influence of the ECC. 2102: 1442:Archaeology and historic preservation in Palau 1323:Archaeology and historic preservation in Palau 212:of 603,978 km (233,197 sq mi). 1885: 1479: 1183:Map including most of the islands of Palau ( 272:(Tobi), some distance southwest of Angaur. 1243:Note: if submerged reefs are included then 1892: 1878: 1486: 1472: 24: 295:clay deposit covers much of southeastern 256:." The limestone islands of Beliliou and 167:603,978 km (233,197 sq mi) 1899: 940: 406:242 meters (794 ft) (on Babeldaob) 177:Map of Palau and its location in Oceania 172: 1384:. Hong Kong Observatory. Archived from 430:Environment - international agreements: 2103: 1535:Trust Territory of the Pacific Islands 1873: 1467: 1335: 1333: 1315: 1313: 1311: 1309: 1307: 1305: 1280: 1278: 1276: 1274: 332:(NEC, flowing east to west) and the 315:areas are unlikely. Excepting a few 509:Climate data for Palau (Köppen Af) 13: 1493: 1029:associations are found on coastal 14: 2122: 1330: 1302: 1271: 1259:Map of main island chain of Palau 1252: 1192: 103:459 km (177 sq mi) 1449: 1433: This article incorporates 1428: 1409: This article incorporates 1404: 1176: 1162: 1150: 1135: 1110: 1096: 1084: 1072: 1060: 197:chain. The country includes the 323: 299:Island and exceeds 45 m thick. 1924:Federated States of Micronesia 1374: 1350: 929:Source: Hong Kong Observatory 1: 1264: 1247:is Palau's northernmost point 936: 768:Average rainfall mm (inches) 362: 1051:(0 m); The highest point is 7: 1649:Compact of Free Association 698:Mean daily minimum °C (°F) 558:Mean daily maximum °C (°F) 252:islands, are known as the " 215: 127:1,519 km (944 mi) 10: 2127: 1125: 928: 508: 485: 275: 2015: 1992: 1911: 1836: 1769: 1756: 1747: 1725: 1716: 1644: 1635: 1601: 1556: 1552: 1543: 1505: 1041: 881: 837: 767: 697: 627: 557: 552: 549: 546: 543: 540: 537: 534: 531: 528: 525: 522: 519: 516: 513: 334:Equatorial Countercurrent 163: 151: 139: 131: 123: 115: 107: 99: 89: 52: 42: 32: 23: 2075:Northern Mariana Islands 348: 342:Sea surface temperatures 330:North Equatorial Current 147:242 metres (794 ft) 2040:Cocos (Keeling) Islands 982:, the palm forest, the 384:exclusive economic zone 380:12 nautical miles 210:Exclusive Economic Zone 164:Exclusive economic zone 1435:public domain material 1411:public domain material 946: 178: 2018:and other territories 1219:Southernmost point – 1201:Northernmost point – 944: 176: 1234:Westernmost point - 1212:Easternmost point – 957:secondary vegetation 404:Mount Ngerchelchauus 1515:Spanish East Indies 1104:Mount Ngerchelchuus 1091:Palau geography map 1079:Ulong Island, Palau 1053:Mount Ngerchelchuus 838:Average rainy days 628:Daily mean °C (°F) 392:Elevation extremes: 242:coralline limestone 144:Mount Ngerchelchuus 70: /  20: 2111:Geography of Palau 1730:Telecommunications 1704:Traditional chiefs 1576:Towns and villages 1525:South Seas Mandate 1417:The World Factbook 947: 398:Pacific Ocean 0 m 179: 116: • Water 100: • Total 19:Geography of Palau 18: 2098: 2097: 2090:Wallis and Futuna 2035:Clipperton Island 1993:Associated states 1867: 1866: 1832: 1831: 1743: 1742: 1712: 1711: 1679:Political parties 1674:National Congress 1659:Foreign relations 1631: 1630: 1627: 1626: 1530:Battle of Peleliu 1520:German New Guinea 1388:on 1 October 2018 1238:, Hatohobei state 980:plantation forest 933: 932: 443:, Climate Change- 338:Southwest Islands 225:on the island of 171: 170: 108: • Land 74:7.500°N 134.500°E 2118: 2080:Pitcairn Islands 2050:French Polynesia 2030:Christmas Island 1959:Papua New Guinea 1939:Marshall Islands 1912:Sovereign states 1894: 1887: 1880: 1871: 1870: 1852: 1845: 1754: 1753: 1723: 1722: 1642: 1641: 1554: 1553: 1550: 1549: 1488: 1481: 1474: 1465: 1464: 1453: 1452: 1446: 1432: 1431: 1425: 1408: 1407: 1398: 1397: 1395: 1393: 1378: 1372: 1371: 1369: 1368: 1354: 1348: 1347: 1337: 1328: 1327: 1317: 1300: 1299: 1297: 1296: 1282: 1216:, Kayangel state 1180: 1166: 1154: 1139: 1114: 1100: 1088: 1076: 1064: 506: 505: 464:marine ecosystem 419:permanent crops: 378:territorial sea: 374:Maritime claims: 282:volcanic breccia 262:platform islands 195:Caroline Islands 181:The Republic of 85: 84: 82: 81: 80: 75: 71: 68: 67: 66: 63: 28: 21: 17: 2126: 2125: 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Retrieved 1289: 1245:Velasco reef 1242: 1196: 1045: 1012: 961: 948: 495: 489: 456: 437:Biodiversity 433: 429: 428: 423: 418: 414:arable land: 413: 409: 408: 400: 395: 391: 390: 382: 377: 373: 372: 366: 352: 327: 324:Oceanography 311:and coastal 301: 279: 254:rock islands 235: 219: 202:battleground 199:World War II 180: 152:Lowest point 94:Ranked 179th 15: 1949:New Zealand 1761:LGBT rights 1566:Environment 1362:Weatherbase 1290:www.cia.gov 1236:Tobi Island 500:trade winds 480:overfishing 286:interbedded 187:Philippines 77: / 53:Coordinates 1614:Chelbacheb 1367:2019-03-28 1295:2019-03-27 1265:References 1225:Helen Reef 1221:Round Rock 1170:Mecherchar 992:breadfruit 984:agroforest 968:hard woods 937:Vegetation 363:Statistics 317:calcareous 309:intertidal 227:New Guinea 1919:Australia 1901:Geography 1735:Transport 1684:President 1654:Elections 1619:Ioueldaob 1609:Babeldaob 1545:Geography 1229:Hatohobei 1119:Babeldaob 1055:(242 m). 1019:pineapple 833:(147.97) 492:diurnally 459:Babeldaob 434:party to: 410:Land use: 356:limestone 297:Babeldaob 260:, called 238:Babeldaob 124:Coastline 33:Continent 2105:Category 1934:Kiribati 1859:Category 1819:Religion 1804:Language 1669:Military 1637:Politics 1581:Wildlife 1499:articles 1207:Kayangel 1031:lowlands 1008:betelnut 976:pandanus 924:2,357.4 828:(11.98) 823:(11.32) 818:(13.87) 813:(11.86) 808:(14.95) 803:(18.04) 798:(17.27) 793:(11.99) 773:(10.70) 270:Tochobei 266:Sonsorol 250:Beliliou 231:Mindanao 223:Jayapura 216:Landform 65:134°30′E 2085:Tokelau 1984:Vanuatu 1905:Oceania 1843:Outline 1789:Cuisine 1771:Culture 1749:Society 1718:Economy 1602:Regions 1591:Mammals 1561:Climate 1507:History 1187:, 1991) 1157:Peleliu 1126:Islands 1036:Palauan 1023:tobacco 1015:cassava 988:coconut 831:3,758.3 788:(8.67) 783:(8.20) 778:(9.12) 763:(75.6) 758:(75.6) 753:(75.9) 748:(75.9) 743:(76.1) 738:(75.7) 733:(75.4) 728:(75.6) 723:(76.1) 718:(75.9) 713:(75.4) 708:(75.0) 703:(75.0) 693:(81.7) 688:(81.9) 683:(82.2) 678:(81.9) 673:(81.9) 668:(81.5) 663:(81.3) 658:(81.7) 653:(82.4) 648:(82.2) 643:(81.5) 638:(81.0) 633:(81.1) 623:(87.7) 618:(88.0) 613:(88.5) 608:(88.0) 603:(87.6) 598:(87.3) 593:(87.1) 588:(87.8) 583:(88.5) 578:(88.3) 573:(87.6) 568:(87.1) 563:(87.1) 486:Climate 276:Geology 206:Peleliu 191:Oceania 132:Borders 47:Oceania 2060:Hawaii 1979:Tuvalu 1824:Sports 1779:Anthem 1699:States 1571:Rivers 1497:  1458:: 1392:20 May 1209:state* 1145:Island 1143:Angaur 1042:Relief 1021:, and 1006:, and 1004:almond 1000:banana 974:, and 952:lagoon 921:182.9 918:183.0 915:179.8 912:198.0 909:176.7 906:186.0 903:168.0 900:210.8 897:234.0 894:244.9 891:194.9 888:198.4 877:224.6 514:Month 424:other: 421:4.35% 416:2.17% 258:Angaur 62:7°30′N 43:Region 1974:Tonga 1964:Samoa 1954:Palau 1944:Nauru 1850:Index 1809:Music 1586:Birds 1495:Palau 1437:from 1413:from 1231:state 996:mango 972:palms 874:19.9 871:18.7 868:20.1 865:16.8 862:19.8 859:21.0 856:21.9 853:20.0 850:14.8 847:16.7 844:15.9 841:19.0 826:304.3 821:287.5 816:352.3 811:301.2 806:379.7 801:458.2 796:438.7 791:304.5 786:220.2 781:208.3 776:231.6 771:271.8 553:Year 466:from 349:Soils 313:swamp 304:Oreor 293:Airai 246:Oreor 189:, in 183:Palau 2055:Guam 2007:Niue 1929:Fiji 1799:Flag 1394:2011 761:24.2 756:24.2 751:24.4 746:24.4 741:24.5 736:24.3 731:24.1 726:24.2 721:24.5 716:24.4 711:24.1 706:23.9 701:23.9 691:27.6 686:27.7 681:27.9 676:27.7 671:27.7 666:27.5 661:27.4 656:27.6 651:28.0 646:27.9 641:27.5 636:27.2 631:27.3 621:31.0 616:31.1 611:31.4 606:31.1 601:30.9 596:30.7 591:30.6 586:31.0 581:31.4 576:31.3 571:30.9 566:30.6 561:30.6 550:Dec 547:Nov 544:Oct 541:Sep 538:Aug 535:Jul 532:Jun 529:May 526:Apr 523:Mar 520:Feb 517:Jan 470:and 468:sand 289:tuff 284:and 268:and 248:and 135:None 90:Area 1903:of 1422:CIA 1185:DMA 204:of 159:0 m 111:99% 2107:: 1420:. 1360:. 1332:^ 1304:^ 1288:. 1273:^ 1227:, 1223:, 1205:, 1017:, 1010:. 1002:, 998:, 994:, 990:, 970:, 496:Af 482:. 474:, 451:, 447:, 439:, 119:1% 1893:e 1886:t 1879:v 1487:e 1480:t 1473:v 1424:. 1396:. 1370:. 1298:. 1241:* 386::

Index


Pacific Ocean
Oceania
7°30′N 134°30′E / 7.500°N 134.500°E / 7.500; 134.500
Ranked 179th
Mount Ngerchelchuus
Pacific Ocean

Palau
Philippines
Oceania
Caroline Islands
World War II
battleground
Peleliu
Exclusive Economic Zone
Jayapura
New Guinea
Mindanao
Babeldaob
coralline limestone
Oreor
Beliliou
rock islands
Angaur
platform islands
Sonsorol
Tochobei
volcanic breccia
interbedded

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