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272:. The Honeycomb Hill Cave area was discovered in 1976 and in 1982 was given the status of a site of global significance in paleozoology due to discoveries of bones of several species that had gone extinct upon human settlement. In 1984, the first systematic discovery campaign led to finds of the bones of fifty birds, most of which were extinct species.
194:. As the logging areas progressed to be further away from the sawmill, it became necessary to build an access road into the rugged environment. Eventually, maintenance costs and extensions of this road escalated, and after changes of ownership and a belated attempt at reforestation, the sawmill went
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In 2008, the
Kahurangi National Park was expanded by an additional 10 hectares to complete the protection of the Honeycomb Hill Cave system. Honeycomb Hill Cave is in a restricted area, with access permitted by permit only. The Oparara Trust has a concession from the Department of Conservation
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The wealth of intact bones and skeletons is explained by the fact that the holes in the limestone could trap bones, protect them from heavy rains and preserve them for long periods of time due to constant thermal conditions and the chemical similarity of bones and limestone. Intact skeletons older
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The limestone layer has been extensively eroded by annual rainfall of up to 6m and the roots of the lush vegetation. Tectonic activity as well as changes in the level of the nearby sea have supported the appearance of unique geological formations. The basin currently contains many of the typical
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forest. The forest floor consists of a thick carpet of mosses, ferns, and understorey plants. Due to the sometimes shallow soil, these plants often have to squeeze their root systems through cracks in the limestone to gain a hold, furthering the erosion of the limestone layer.
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At the time of the bankruptcy, a major campaign was launched to ensure the protection and enhancement of the basin, as well as road maintenance, culminating in the founding of the Ōpārara Valley
Project Trust and the purchase of the area on 1 October 2004.
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Miners and deer hunters have often reported spectacular rock formations in the
Honeycomb Hill area, but it was not until an exploration of the Buller Caving Group in the 1980s that an inventory of the 70 entrances to 13 km of galleries located in the
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With its natural environment relatively closed and isolated, the Ōpārara Basin has long been protected from human influence. However, the locations of natural rock arches have been indicated in maps as early as from the 1880s.
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The Ōpārara Basin resides on a foundation of 350 million year old granite, which was covered with a 15-60m thin layer of limestone approximately 35 million years ago. The surface layer consists of blue-grey mudstone.
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have been found. The former species is strictly protected, with even the collection of empty shells prohibited, while the latter has only been found in areas around 700m from the Ōpārara River. The spiders
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A six-year project to complete a 30 km network of walkways and mountain biking tracks was completed in 2009, opening up more of the Ōpārara Basin to tourists who would have originally only visited the
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into the water upon the decomposition of their vegetation. This colours the waters of the streams and rivers in the area a brown to red tea-like hue, depending on season and rainfall.
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was named after the area and grows near the entrances of arches and caves in the Ōpārara Basin. Despite meticulous research, only 175 plants have been found near a
451:, Mirror Tarn, and the accessible caves Box Canyon Cave and Crazy Paving Cave. The Honeycomb Hill Caves are restricted to visitors on an authorised guided tour.
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system was compiled. These explorations revealed the scientific significance of the cave system by discovering the largest collection of
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features found in a karst landscape, as well as some impressive rock arches and caves, and sites rich in limestone fossils.
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Nowadays this basin is an important habitat of many endemic species, some of which are endangered or unique to the area.
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The Ōpārara Valley is a popular tourist destination, with relatively short walks to see the natural rock arches
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The Ōpārara Basin is the only place where the large carnivorous landsnails
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and for being the sole habitat of several plant and animal species.
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Report of
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West Coast locals open up native forest and caves to visitors
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180° panoramic view of the Ōpārara Basin from the access road
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The Ōpārara Basin is also famous for its unique remains in
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to the area, while the caves are home to the protected
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The Ōpārara Basin is famous for its unique remains in
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in
Wellington. Further finds included skeletons of
511:Fife, Allan J.; Knightbridge, Phil (October 2005).
59:. Unsourced material may be challenged and removed.
517:and recommendations for track upgrades at Oparara"
501:(from 3 News website. Accessed 16 September 2013.)
423:Several of the plant species in the area release
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225:Several placenames in the area are inspired by
159:, it is one of the most striking places of the
1562:Blackwater River (Little Grey River tributary)
1246:Proposals for a road through North-west Nelson
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371:The Ōpārara Basin is also a habitat of the
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1557:Blackwater River (Buller River tributary)
275:The first and most complete bones of the
119:Learn how and when to remove this message
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305:than 20,000 years have been discovered.
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279:were found here, now on display at the
139:at 20 kilometres (12 mi) north of
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1263:Westhaven (Te Tai Tapu) Marine Reserve
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398:Most of the area is covered in mixed
309:to provide guided tours of the area.
513:"Distribution of the very rare moss
366:New Zealand greater short-tailed bat
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57:adding citations to reliable sources
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524:DOC Research and Development Series
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1896:Landforms of the West Coast Region
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297:, and nine different species of
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44:needs additional citations for
1901:Drainage basins of New Zealand
1227:Nelson Coast temperate forests
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281:National Museum of New Zealand
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153:its large natural rock arches
480:History of the Oparara Basin
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1768:Pancake Rocks and Blowholes
1617:Metro Cave / Te Ananui Cave
1233:Opacuincola gretathunbergae
214:ever found in New Zealand.
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1691:Facilities and attractions
552:41.1508695°S 172.1908772°E
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289:New Zealand owlet-nightjar
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135:is a basin drained by the
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1743:Karamea Centennial Museum
1718:Granity Community Library
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1798:Stillwater–Ngākawau Line
1778:Punakaiki Marine Reserve
1733:Kahurangi Marine Reserve
1682:Wharepapa / Arthur Range
1210:Kahurangi Marine Reserve
654:Wharepapa / Arthur Range
557:-41.1508695; 172.1908772
1906:Kahurangi National Park
1738:Kahurangi National Park
1252:Pseudowintera traversii
691:Ellis Basin cave system
609:Kahurangi National Park
515:Epipterygium opararense
413:Epipterygium opararense
329:Powelliphanta annectens
323:Powelliphanta marchanti
313:Today's fauna and flora
161:Kahurangi National Park
1758:Ngakawau Hydro Project
1703:Charming Creek Tramway
1677:Waitakere / Nile River
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1870:Ngāti Apa ki te Rā Tō
1773:Paparoa National Park
1137:Little Wanganui River
909:Little Waingaro River
899:Little Pokororo River
485:26 March 2014 at the
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362:Arachnocampa luminosa
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228:The Lord of the Rings
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157:temperate rainforests
151:of New Zealand. With
1813:Victoria Forest Park
1642:Ōpārara Basin Arches
1029:Te Waikoropupū River
884:Little Boulder River
736:Lakes and reservoirs
701:Ōpārara Basin Arches
573:Oparara Valley Trust
294:Aptornis otidiformis
53:improve this article
1662:Perpendicular Point
1525:Geographic features
894:Little Ōnahau River
696:Honeycomb Hill Cave
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410:The very rare moss
262:Honeycomb Hill Cave
235:Geology and climate
208:Honeycomb Hill Cave
1793:Seddonville Branch
1708:Conns Creek Branch
1365:Inangahua Junction
1240:Pittosporum dallii
1164:Roaring Lion River
944:Pariwhakaoho River
904:Little Slate River
889:Little Devil River
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389:New Zealand falcon
377:great spotted kiwi
351:Nelson cave spider
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1728:Inland Pack Track
1647:Ōtūmahana Estuary
1582:Denniston Plateau
1547:Ballroom Overhang
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1132:Little Crow River
393:paradise shelduck
248:Fauna of the past
145:West Coast Region
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16:(Redirected from
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1849:Regional Council
1839:District Council
1823:Westport Airport
1783:Reefton Hospital
1385:Springs Junction
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1203:Related articles
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964:Puremāhaia River
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1191:
1188:
1187:
1185:
1181:
1175:
1172:
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1167:
1165:
1162:
1160:
1157:
1153:
1150:
1149:
1148:
1147:Ōpārara River
1145:
1143:
1140:
1138:
1135:
1133:
1130:
1128:
1125:
1123:
1120:
1118:
1115:
1113:
1112:Karamea River
1110:
1108:
1105:
1103:
1100:
1098:
1097:Johnson River
1095:
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1083:
1080:
1078:
1075:
1073:
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1040:
1037:
1035:
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1027:
1025:
1022:
1020:
1017:
1015:
1014:Stanley River
1012:
1010:
1007:
1005:
1002:
1000:
997:
995:
992:
990:
987:
985:
982:
980:
979:Rolling River
977:
975:
972:
970:
969:Riuwaka River
967:
965:
962:
960:
957:
955:
952:
950:
949:Paturau River
947:
945:
942:
940:
937:
935:
932:
930:
927:
925:
924:Onekaka River
922:
920:
917:
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912:
910:
907:
905:
902:
900:
897:
895:
892:
890:
887:
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880:
879:Kaituna River
877:
875:
872:
870:
867:
865:
862:
860:
857:
855:
852:
850:
847:
845:
842:
840:
837:
835:
832:
830:
829:Boulder River
827:
825:
822:
820:
817:
815:
812:
810:
809:Anatoki River
807:
806:
804:
802:
798:
795:
791:
785:
782:
780:
777:
775:
772:
770:
767:
765:
764:Big Rimu Walk
762:
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755:
749:
746:
744:
741:
740:
738:
734:
728:
725:
723:
720:
719:
717:
713:
707:
704:
702:
699:
697:
694:
692:
689:
687:
686:Bulmer Cavern
684:
683:
681:
677:
671:
668:
667:
665:
661:
655:
652:
650:
649:Glasgow Range
647:
646:
644:
640:
634:
631:
629:
628:Mount Burnett
626:
624:
621:
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589:
584:
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318:
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300:
296:
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278:
277:Haast's eagle
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258:
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188:
175:
171:
169:
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158:
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146:
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138:
137:Ōpārara River
134:
133:Ōpārara Basin
123:
120:
112:
101:
98:
94:
91:
87:
84:
80:
77:
73:
70: –
69:
65:
64:Find sources:
58:
54:
48:
47:
42:This article
40:
36:
31:
30:
27:
19:
18:Oparara Basin
1808:Truman Track
1723:Heaphy Track
1713:Fenian Track
1672:Scotts Beach
1636:
1572:Buller River
1567:Buller Gorge
1542:Awarau River
1345:Blacks Point
1250:
1238:
1231:
1190:Buller River
1159:Postal River
1151:
1122:Leslie River
1107:Kākāpō River
1082:Heaphy River
1077:Gunner River
1024:Tākaka River
1019:Tadmor River
989:Sherry River
954:Pearse River
919:Ōnahau River
914:Matiri River
844:Clarke River
814:Aorere River
774:Heaphy Track
769:Fenian Track
748:Lake Sparrow
743:Boulder Lake
727:Scotts Beach
670:Granity Pass
623:Mount Arthur
533:
523:
514:
506:
494:
475:
463:
449:Oparara Arch
442:
422:
411:
409:
397:
370:
361:
353:
340:
334:
327:
321:
319:
316:
307:
303:
292:
285:Lyall's wren
274:
270:paleozoology
267:
260:
259:skeleton in
242:
238:
226:
224:
220:Heaphy Track
216:
212:bird fossils
204:
200:
189:
185:
168:paleozoology
165:
149:South Island
132:
130:
115:
106:
96:
89:
82:
75:
63:
51:Please help
46:verification
43:
26:
1627:Mount Haast
1532:Allen River
1466:Waimangaroa
1451:Seddonville
1399:Seddon Ward
1355:Crushington
1215:Lake Matiri
1169:Taipō River
1127:Lewis River
1062:Allen River
999:Slate River
994:Skeet River
984:Saxon River
974:Rocky River
929:Ōtere River
864:Ellis River
859:Devil River
839:Clark River
834:Brown River
819:Baton River
555: /
543:172°11′27″E
439:Mirror Tarn
364:), and the
1885:Categories
1832:Government
1612:Lewis Pass
1492:Charleston
1174:Ugly River
1092:Huia River
1072:Crow River
1009:Spey River
1004:Snow River
934:Owen River
874:Hope River
869:Fyfe River
854:Dart River
849:Cobb River
633:Mount Owen
540:41°09′03″S
455:References
445:Moria Gate
354:Spelungula
109:April 2022
79:newspapers
1865:Ngāi Tahu
1587:Fox River
1497:Punakaiki
1461:Summerlea
1441:Mokihinui
1436:Millerton
1411:Denniston
1340:Big River
824:Big River
616:Mountains
373:blue duck
358:glowworms
345:are also
143:, at the
1512:Westport
1456:Stockton
1446:Ngakawau
1360:Ikamatua
1350:Cronadun
1319:Westport
483:Archived
447:and the
418:tramping
404:podocarp
196:bankrupt
1507:Te Kuha
1426:Karamea
1416:Granity
1406:Arapito
1380:Reefton
1258:Pūponga
431:Tourism
425:tannins
347:endemic
192:sawmill
182:History
147:of the
141:Karamea
93:scholar
1421:Hector
1390:Waiuta
1375:Maruia
793:Rivers
526:(221).
420:path.
391:, and
95:
88:
81:
74:
66:
1844:Mayor
1370:Lyell
1152:Basin
679:Caves
520:(PDF)
400:beech
100:JSTOR
86:books
1315:Seat
402:and
385:weka
339:and
326:and
131:The
72:news
1858:Iwi
381:kea
299:moa
257:Moa
55:by
1887::
1317::
522:.
395:.
387:,
383:,
375:,
368:.
356:,
291:,
287:,
222:.
163:.
1297:e
1290:t
1283:v
601:e
594:t
587:v
360:(
122:)
116:(
111:)
107:(
97:·
90:·
83:·
76:·
49:.
20:)
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