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Journal articles on the topic 'Mount Cook National Park'

Author: Grafiati

Published: 4 June 2021

Last updated: 12 February 2022

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1

Waterhouse, J. B. "Permian fossils in Malte Brun Range, Mount Cook National Park, New Zealand." New Zealand Journal of Geology and Geophysics 30, no. 1 (January 1987): 91–92. http://dx.doi.org/10.1080/00288306.1987.10422196.

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2

Warren, Charles R., and Martin P. Kirkbride. "Temperature and bathymetry of ice‐contact lakes in Mount Cook National Park, New Zealand." New Zealand Journal of Geology and Geophysics 41, no. 2 (June 1998): 133–43. http://dx.doi.org/10.1080/00288306.1998.9514797.

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3

Kirkbride, Martin P. "Relationships between temperature and ablation on the Tasman Glacier, Mount Cook National Park, New Zealand." New Zealand Journal of Geology and Geophysics 38, no. 1 (March 1995): 17–27. http://dx.doi.org/10.1080/00288306.1995.9514636.

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4

Blair, R. W. "Moraine and Valley Wall Collapse due to Rapid Deglaciation in Mount Cook National Park, New Zealand." Mountain Research and Development 14, no. 4 (November 1994): 347. http://dx.doi.org/10.2307/3673731.

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5

Robertson, Clare M., Douglas I. Benn, Martin S. Brook, lan C. Fuller, and Kat A. Holt. "Subaqueous calving margin morphology at Mueller, Hooker and Tasman glaciers in Aoraki/Mount Cook National Park, New Zealand." Journal of Glaciology 58, no. 212 (2012): 1037–46. http://dx.doi.org/10.3189/2012jog12j048.

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AbstractThe subaqueous margins of calving glaciers have the potential to make significant contributions to glacier mass loss. However, to date, very little is known about the morphology and development of subaqueous margins. A unique combination of sub-bottom profile and bathymetric data collected between 2008 and 2010 in proglacial lakes at Mueller, Hooker and Tasman glaciers in New Zealand’s Southern Alps reveal subaqueous ice ramps extending up to 510 m from the terminus of each glacier. Ice ramp surfaces are undulating and covered with a thick layer (up to 10 m) of unsorted sediment derived from supraglacial and englacial debris, lateral moraines and deltaic deposits. A cyclic calving pattern, relatively stable lake level and the debris cover appear to control the development and maintenance of these ice ramps. High subaerial retreat rates generally correspond to high subaqueous calving rates, although the highest subaerial retreat rates are not associated with the largest ice ramp. Debris mantling the subaqueous ice ramp surfaces insulates the ice from melting and also reduces buoyant forces acting on the terminus. Comparisons with previous studies show that the ice ramps evolve over time with changes in glacier dynamics and water-body properties.

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6

BRANCH, WILLIAM R., JENNIFER A. GUYTON, ANDREAS SCHMITZ, MICHAEL F. BAREJ, PIOTR NASKRECKI, HARITH FAROOQ, LUKE VERBURGT, and MARK-OLIVER RÖDEL. "Description of a new flat gecko (Squamata: Gekkonidae: Afroedura) from Mount Gorongosa, Mozambique." Zootaxa 4324, no. 1 (September 26, 2017): 142. http://dx.doi.org/10.11646/zootaxa.4324.1.8.

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A new species of flat gecko, Afroedura gorongosa sp. nov., is described from Gorongosa National Park, Sofala Province, central Mozambique. The new species is morphologically similar to A. transvaalica and A. loveridgei, from both of which it is genetically distinct (15–17% divergence; 400 bp of 16S rRNA). Morphologically it can be distinguished from both species by having fewer midbody scale rows (97–101) and a higher number of precloacal pores in males (8–13). The type series was collected on the western flanks of Mount Gorongosa (900 and 1100 m a.s.l.) in comparatively cool and moist microclimates, where it is threatened by illegal deforestation. Additional material was collected as low as 212 m a.s.l. on an inselberg near Mount Gorongosa. The new discovery adds to the growing number of endemic montane reptiles discovered in Mozambique in recent years, and highlights the need for a national conservation assessment of the country’s herpetofauna and continued protection of the Mount Gorongosa region.

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7

Rosenberg, Sandra M., Ian R. Walker, and Rolf W. Mathewes. "Postglacial spread of hemlock (Tsuga) and vegetation history in Mount Revelstoke National Park, British Columbia, Canada." Canadian Journal of Botany 81, no. 2 (February 1, 2003): 139–51. http://dx.doi.org/10.1139/b03-015.

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To investigate postglacial environmental changes in southeastern British Columbia, subfossil pollen was analyzed from Eagle Lake, Mount Revelstoke National Park. Palynological evidence suggests that during the early Holocene, Eagle Lake was surrounded by an open forest. The pollen assemblage indicates that climatic conditions were warmer and drier than at present with high alder pollen values. Spruce and fir were common in local forests throughout the Holocene. Western hemlock pollen first occurs at approximately 3500 14C years BP. The migration path of western hemlock into this region is currently unclear. Data from palynological records appear insufficient to resolve the migration pattern, although several routes are possible. The available data support northward migration into southeastern British Columbia. The arrival of this conifer may be in response to the late Holocene increase in precipitation, as inferred from many lower elevation and coastal sites. Mountain hemlock pollen does not appear until about 2100 14C years BP. Mountain hemlock's migration route into southeastern British Columbia is also unresolved. In the late Holocene, the presence of mountain hemlock, and increases of Ericales and Valeriana sitchensis pollen, suggest a shift to the more open, cool, and moist conditions characteristic of the modern-day subalpine parkland. These climatic inferences correspond closely to those derived from other palynological and geological evidence throughout southern British Columbia.Key words: pollen, vegetation, Tsuga, hemlock, British Columbia, Holocene, climate.

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8

Gore, Donald R. "Mount McKinley, Denali National Park, Alaska." Spine 27, no. 21 (November 2002): i. http://dx.doi.org/10.1097/00007632-200211010-00001.

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9

Amri, K., and A. S. Pungkas. "Commodification of Mount Gede Pangrango National Park." KnE Social Sciences 3, no. 11 (August 8, 2018): 1162. http://dx.doi.org/10.18502/kss.v3i11.2837.

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10

Siegel, Rodney B., Robert L. Wilkerson, Robert C. Kuntz, James F. Saracco, and Amanda L. Holmgren. "Elevation Ranges of Birds at Mount Rainier National Park, North Cascades National Park Complex, and Olympic National Park, Washington." Northwestern Naturalist 93, no. 1 (March 2012): 23–39. http://dx.doi.org/10.1898/11-08.1.

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11

Karakaş, Recep, and Murat Biricik. "Birds of Mount Nemrut National Park Area, Turkey." eco.mont (Journal on Protected Mountain Areas Research) 10, no. 1 (2018): 36–45. http://dx.doi.org/10.1553/eco.mont-10-1s36.

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12

Putri, I. R., L. R. W. Faida, C. Fandeli, and R. H. Purwanto. "TOURIST DECISION IN MOUNT MERBABU NATIONAL PARK, INDONESIA." Russian Journal of Agricultural and Socio-Economic Sciences 75, no. 3 (March 30, 2018): 24–35. http://dx.doi.org/10.18551/rjoas.2018-03.03.

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13

PERKINS, PHILIP D. "A revision of the Australian humicolous and hygropetric water beetle genus Tympanogaster Perkins, and comparative morphology of the Meropathina (Coleoptera: Hydraenidae)." Zootaxa 1346, no. 1 (October 30, 2006): 1. http://dx.doi.org/10.11646/zootaxa.1346.1.1.

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The Australian endemic humicolous and hygropetric water beetle genus Tympanogaster Perkins, 1979, is revised, based on the study of 7,280 specimens. The genus is redescribed, and redescriptions are provided for T. cornuta (Janssens), T. costata (Deane), T. deanei Perkins, T. macrognatha (Lea), T. novicia (Blackburn), T. obcordata (Deane), T. schizolabra (Deane), and T. subcostata (Deane). Lectotypes are designated for Ochthebius labratus Deane, 1933, and Ochthebius macrognathus Lea, 1926. Ochthebius labratus Deane, 1933, is synonymized with Ochthebius novicius Blackburn, 1896. Three new subgenera are described: Hygrotympanogaster new subgenus (type species Tympanogaster (Hygrotympanogaster) maureenae new species; Topotympanogaster new subgenus (type species Tympanogaster (Topotympanogaster) crista new species; and Plesiotympanogaster new genus (type species Tympanogaster (Plesiotympanogaster) thayerae new species. Seventy-six new species are described, and keys to the subgenera, species groups, and species are given. High resolution digital images of all primary types are presented (online version in color), and geographic distributions are mapped. Male genitalia, representative spermathecae and representative mouthparts are illustrated. Scanning electron micrographs of external morphological characters of adults and larvae are presented. Selected morphological features of the other members of the subtribe Meropathina, Meropathus Enderlein and Tympallopatrum Perkins, are illustrated and compared with those of Tympanogaster. Species of Tympanogaster are typically found in the relict rainforest patches in eastern Australia. Most species have very limited distributions, and relict rainforest patches often have more than one endemic species. The only species currently known from the arid center of Australia, T. novicia, has the widest distribution pattern, ranging into eastern rainforest patches. There is a fairly close correspondence between subgenera and microhabitat preferences. Members of Tympanogaster (s. str.) live in the splash zone, usually on stream boulders, or on bedrock stream margins. The majority of T. (Hygrotympanogaster) species live in the hygropetric zone at the margins of waterfalls, or on steep rockfaces where water is continually trickling; a few rare species have been collected from moss in Nothofagus rainforests. Species of T. (Plesiotympanogaster) have been found in both hygropetric microhabitats and in streamside moss. The exact microhabitats of T. (Topotympanogaster) are unknown, but the morphology of most species suggests non-aquatic habits; most specimens have been collected in humicolous microhabitats, by sifting rainforest debris, or were taken in flight intercept traps. Larvae of hygropetric species are often collected with adults. These larvae have tube-like, dorsally positioned, mesothoracic spiracles that allow the larvae to breathe while under a thin film of water. The key morphological differences between larvae of Tympanogaster (s. str.) and those of Tympanogaster (Hygrotympanogaster) are illustrated. New species of Tympanogaster are: T. (s. str.) aldinga (New South Wales, Dorrigo National Park, Rosewood Creek), T. (s. str.) amaroo (New South Wales, Back Creek, downstream of Moffatt Falls), T. (s. str.) ambigua (Queensland, Cairns), T. (Hygrotympanogaster) arcuata (New South Wales, Kara Creek, 13 km NEbyE of Jindabyne), T. (Hygrotympanogaster) atroargenta (Victoria, Possum Hollow falls, West branch Tarwin River, 5.6 km SSW Allambee), T. (Hygrotympanogaster) barronensis (Queensland, Barron Falls, Kuranda), T. (s. str.) bluensis (New South Wales, Blue Mountains), T. (Hygrotympanogaster) bondi (New South Wales, Bondi Heights), T. (Hygrotympanogaster) bryosa (New South Wales, New England National Park), T. (Hygrotympanogaster) buffalo (Victoria, Mount Buffalo National Park), T. (Hygrotympanogaster) canobolas (New South Wales, Mount Canobolas Park), T. (s. str.) cardwellensis (Queensland, Cardwell Range, Goddard Creek), T. (Hygrotympanogaster) cascadensis (New South Wales, Cascades Campsite, on Tuross River), T. (Hygrotympanogaster) clandestina (Victoria, Grampians National Park, Golton Gorge, 7.0 km W Dadswells Bridge), T. (Hygrotympanogaster) clypeata (Victoria, Grampians National Park, Golton Gorge, 7.0 km W Dadswells Bridge), T. (s. str.) cooloogatta (New South Wales, New England National Park, Five Day Creek), T. (Hygrotympanogaster) coopacambra (Victoria, Beehive Falls, ~2 km E of Cann Valley Highway on 'WB Line'), T. (Topotympanogaster) crista (Queensland, Mount Cleveland summit), T. (Hygrotympanogaster) cudgee (New South Wales, New England National Park, 0.8 km S of Pk. Gate), T. (s. str.) cunninghamensis (Queensland, Main Range National Park, Cunningham's Gap, Gap Creek), T. (s. str.) darlingtoni (New South Wales, Barrington Tops), T. (Hygrotympanogaster) decepta (Victoria, Mount Buffalo National Park), T. (s. str.) dingabledinga (New South Wales, Dorrigo National Park, Rosewood Creek, upstream from Coachwood Falls), T. (s. str.) dorrigoensis (New South Wales, Dorrigo National Park, Rosewood Creek, upstream from Coachwood Falls), T. (Topotympanogaster) dorsa (Queensland, Windin Falls, NW Mount Bartle-Frere), T. (Hygrotympanogaster) duobifida (Victoria, 0.25 km E Binns, Hill Junction, adjacent to Jeeralang West Road, 4.0 km S Jeerelang), T. (s. str.) eungella (Queensland, Finch Hatton Gorge), T. (Topotympanogaster) finniganensis (Queensland, Mount Finnigan summit), T. (s. str.) foveova (New South Wales, Border Ranges National Park, Brindle Creek), T. (Hygrotympanogaster) grampians (Victoria, Grampians National Park, Epacris Falls, 2.5 km WNW Halls Gap), T. (Hygrotympanogaster) gushi (New South Wales, Mount Canobolas Park), T. (s. str.) hypipamee (Queensland, Mount Hypipamee National Park, Barron River headwaters below Dinner Falls), T. (s. str.) illawarra (New South Wales, Macquarie Rivulet Falls, near Wollongong), T. (Topotympanogaster) intricata (Queensland, Mossman Bluff Track, 5–10 km W Mossman), T. (s. str.) jaechi (Queensland, Running Creek, along road between Mount Chinghee National Park and Border Ranges National Park), T. (Topotympanogaster) juga (Queensland, Mount Lewis summit), T. kuranda (Queensland, Barron Falls, Kuranda), T. (s. str.) lamingtonensis (Queensland, Lamington National Park, Lightening Creek), T. (s. str.) magarra (New South Wales, Border Ranges National Park, Brindle Creek), T. (Hygrotympanogaster) maureenae (New South Wales, Back Creek, Moffatt Falls, ca. 5 km W New England National Park boundary), T. (Hygrotympanogaster) megamorpha (Victoria, Possum Hollow falls, W br. Tarwin River, 5.6 km SSW Allambee), T. (Hygrotympanogaster) merrijig (Victoria, Merrijig), T. (s. str.) millaamillaa (Queensland, Millaa Millaa), T. modulatrix (Victoria, Talbot Creek at Thomson Valley Road, 4.25 km WSW Beardmore), T. (Topotympanogaster) monteithi (Queensland, Mount Bartle Frere), T. moondarra (New South Wales, Border Ranges National Park, Brindle Creek), T. (s. str.) mysteriosa (Queensland), T. (Hygrotympanogaster) nargun (Victoria, Deadcock Den, on Den of Nargun Creek, Mitchell River National Park), T. (Hygrotympanogaster) newtoni (Victoria, Mount Buffalo National Park), T. (s. str.) ovipennis (New South Wales, Dorrigo National Park, Rosewood Creek, upstream from Coachwood Falls), T. (s. str.) pagetae (New South Wales, Back Creek, downstream of Moffatt Falls), T. (Topotympanogaster) parallela (Queensland, Mossman Bluff Track, 5–10 km W Mossman), T. (s. str.) perpendicula (Queensland, Mossman Bluff Track, 5–10 km W Mossman), T. plana (Queensland, Cape Tribulation), T. (Hygrotympanogaster) porchi (Victoria, Tarra-Bulga National Park, Tarra Valley Road, 1.5 km SE Tarra Falls), T. (s. str.) precariosa (New South Wales, Leycester Creek, 4 km. S of Border Ranges National Park), T. (s. str.) protecta (New South Wales, Leycester Creek, 4 km. S of Border Ranges National Park), T. (Hygrotympanogaster) punctata (Victoria, Mount Buffalo National Park, Eurobin Creek), T. (s. str.) ravenshoensis (Queensland, Ravenshoe State Forest, Charmillan Creek, 12 km SE Ravenshoe), T. (s. str.) robinae (New South Wales, Back Creek, downstream of Moffatt Falls), T. (s. str.) serrata (Queensland, Natural Bridge National Park, Cave Creek), T. (Hygrotympanogaster) spicerensis (Queensland, Spicer’s Peak summit), T. (Hygrotympanogaster) storeyi (Queensland, Windsor Tableland), T. (Topotympanogaster) summa (Queensland, Mount Elliott summit), T. (Hygrotympanogaster) tabula (New South Wales, Mount Canobolas Park), T. (Hygrotympanogaster) tallawarra (New South Wales, Dorrigo National Park, Rosewood Creek, Cedar Falls), T. (s. str.) tenax (New South Wales, Salisbury), T. (Plesiotympanogaster) thayerae (Tasmania, Liffey Forest Reserve at Liffey River), T. (s. str.) tora (Queensland, Palmerston National Park), T. trilineata (New South Wales, Sydney), T. (Hygrotympanogaster) truncata (Queensland, Tambourine Mountain), T. (s. str.) volata (Queensland, Palmerston National Park, Learmouth Creek, ca. 14 km SE Millaa Millaa), T. (Hygrotympanogaster) wahroonga (New South Wales, Wahroonga), T. (s. str.) wattsi (New South Wales, Blicks River near Dundurrabin), T. (s. str.) weiri (New South Wales, Allyn River, Chichester State Forest), T. (s. str.) wooloomgabba (New South Wales, New England National Park, Five Day Creek).

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14

Kurniawan, Windra, Cecep Kusmana, Sambas Basuni, Aris Munandar, and Kholil Kholil. "Landuse Conflicts Analysis at Mount Halimun Salak National Park." Journal of Natural Resources and Environmental Management 3, no. 1 (July 1, 2013): 23–30. http://dx.doi.org/10.19081/jpsl.2013.3.1.23.

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15

Ardy Priatama, R., Ernan Rustiadi, Setyardi P. Mulya, and Widiatmaka. "The Encroachment Dynamics in Mount Gede Pangrango National Park." IOP Conference Series: Earth and Environmental Science 556 (September 23, 2020): 012003. http://dx.doi.org/10.1088/1755-1315/556/1/012003.

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16

Rukmana, E., T. Chikmawati, and Sulistijorini. "The Diversity of Pteridaceae in Mount Ciremai National Park." IOP Conference Series: Earth and Environmental Science 197 (November 2, 2018): 012029. http://dx.doi.org/10.1088/1755-1315/197/1/012029.

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17

SETYAWAN, AHMAD DWI. "Possibilities of Mount Lawu to be a National Park." Biodiversitas, Journal of Biological Diversity 2, no. 2 (July 1, 2001): 166–71. http://dx.doi.org/10.13057/biodiv/d020207.

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18

Rahayuningsih, M., ES Rahayu, and AN Pratiwi. "Species richness of Pteridophyta in Mount Merbabu National Park." Journal of Physics: Conference Series 1918, no. 5 (June 1, 2021): 052020. http://dx.doi.org/10.1088/1742-6596/1918/5/052020.

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19

Baird, Kingsley W. "Naming Rights." Militaergeschichtliche Zeitschrift 78, no. 1 (May 8, 2019): 1–18. http://dx.doi.org/10.1515/mgzs-2019-0001.

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Abstract This paper explores the rich and dynamic history of a physically modest hill called Pukeahu Mount Cook, located on the southern outer edges of the central business district in New Zealand’s capital city, Wellington. The hill was named »Pukeahu« by Māori who originally settled in the area and renamed »Mount Cook« by British colonists soon after their arrival in the nineteenth century. The story of Pukeahu Mount Cook is one of Māori habitation, tribal tensions and migrations, of conflict between Māori and Pākehā and the assertion of British colonial rule, and of the official narrative of New Zealand’s national identity forged through overseas wars and reinforced by associated remembrance practices. The hill’s two names, the ascendency of one over the other, and finally their »peaceful coexistence« are a reflection of changing cultural dynamics, a recognition of the nation’s founding bicultural principles and a process of restoration.

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20

Mules, Trevor. "Economic Impacts of National Park Tourism on Gateway Communities: The Case of Kosciuszko National Park." Tourism Economics 11, no. 2 (June 2005): 247–59. http://dx.doi.org/10.5367/0000000054183513.

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Kosciuszko National Park (KNP) is a major tourist attraction for Australians, featuring the highest mountain on the Australian mainland (Mount Kosciuszko) and including popular ski resorts and wilderness. The region adjoining KNP includes townships with a total population of some 25,000 people, whose economic welfare is increasingly affected by tourism to KNP. This paper reports research that surveyed expenditure by visitors to KNP, which injects new activity into the adjoining regional economy. The paper uses the first round of an input–output process to model the impacts of such expenditure on the region, and also develops a spreadsheet model for allocating visitor expenditure between businesses within the park and businesses within the adjoining regional economy.

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21

Grasby, Stephen E., Robert O. van Everdingen, Jan Bednarski, and Dwayne AW Lepitzki. "Travertine mounds of the Cave and Basin National Historic Site, Banff National Park." Canadian Journal of Earth Sciences 40, no. 11 (November 1, 2003): 1501–13. http://dx.doi.org/10.1139/e03-058.

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The Cave and Basin National Historic Site is a fan-shaped travertine deposit associated with four thermal spring outlets. Tentative age dating of the travertine mound indicates growth initiated with onset of the late Holocene shift to more humid and cool climate conditions and suggests that the flow of thermal waters was limited during the Hypsithermal, which in turn places constraints on the evolutionary biology of endemic species in the spring system. Two large caves and one collapsed cave structure are developed within the deposit. Cave development is in response to both physical erosion of till underlying the travertine and acid gas attack of calcite that makes up the deposit. This process is buffered by formation of reaction crusts of gypsum on the interior cave walls. Only minor modern travertine growth occurs due to historic flow control measures. Understanding the flow of water through the historic site is critical for long-term preservation.

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22

Aho, Ken, and Janet Bala. "Vascular Alpine Flora of Mount Washburn, Yellowstone National Park, USA." Madroño 59, no. 1 (January 2012): 2–13. http://dx.doi.org/10.3120/0024-9637-59.1.2.

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23

Stone, Jennifer, Bao C. Lê, and John R. Moring. "FRESHWATER FISHES OF ACADIA NATIONAL PARK, MOUNT DESERT ISLAND, MAINE." Northeastern Naturalist 8, no. 3 (October 2001): 311–18. http://dx.doi.org/10.1656/1092-6194(2001)008[0311:ffoanp]2.0.co;2.

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Stone, Jennifer, Bao C. Le, and John R. Moring. "Freshwater Fishes of Acadia National Park, Mount Desert Island, Maine." Northeastern Naturalist 8, no. 3 (2001): 311. http://dx.doi.org/10.2307/3858487.

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25

Klingle, Matthew. "National Park, City Playground: Mount Rainier in the Twentieth Century." Western Historical Quarterly 39, no. 2 (May 2008): 223–24. http://dx.doi.org/10.1093/whq/39.2.223.

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26

Schilling, Tony. "Conservation in Nepal. IV: The Mount Everest (Sagarmatha) National Park." Curtis's Botanical Magazine 14, no. 3 (August 1997): 153–66. http://dx.doi.org/10.1111/1467-8748.00094.

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27

Sadikin, P. N., S. Mulatsih, B. Pramudya, and H. S. Arifin. "Dynamic model of ecotourism management in Mount Rinjani National Park." IOP Conference Series: Earth and Environmental Science 399 (December 31, 2019): 012041. http://dx.doi.org/10.1088/1755-1315/399/1/012041.

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28

Faida, Lies Rahayu Wijayanti, Denni Susanto, Kristiani Fajar Wianti, M. Danang Anggoro, and Marlianansari Putri. "Community Interactions in Sand Utilization within Mount Merapi National Park." Jurnal Ilmu Lingkungan 19, no. 3 (July 28, 2021): 525–30. http://dx.doi.org/10.14710/jil.19.3.525-530.

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Interaksi masyarakat dengan Taman Nasional Gunung Merapi sudah ada bahkan jauh sebelum taman nasional ditetapkan. Salah satu bentuk interaksi yang masih dilakukan oleh masyarakat adalah pemanfaatan pasir di kawasan Kali Putih. Tujuan penelitian ini adalah mengetahui interaksi masyarakat sekitar Taman Nasional Gunung Merapi dalam pemanfaatan pasir di kawasan Kali Putih Zona Khusus Rekonstruksi dan Mitigasi. Metode penelitian yang digunakan pada penelitian ini adalah metode survei. Wawancara dilakukan langsung dengan masyarakat yang melakukan aktivitas di kawasan Kali Putih, Zona Khusus Mitigasi dan Rekonstruksi Taman Nasional Gunung Merapi. Penentuan informan dilakukan dengan accidental sampling dimana informan ditentukan secara kebetulan di lapangan saat melakukan aktivitas pemanfaatan sumber daya pasir di kawasan Kali Putih. Hasil wawancara kemudian diolah menggunakan analisis deskriptif kualitatif. Berdasarkan hasil pengambilan informasi di lapangan, didapatkan beberapa informasi diantaranya aktivitas penambangan pasir sudah dilakukan pada tahun 1977. Interaksi masyarakat dalam pemanfaatan pasir di Kali Putih dipayungi hukum berupa kemitraan kawasan konservasi dengan dokumen PKS Nomor : PKS.34/BTNGM/TU/Kons/04/2018 dan 08/PMH/04/2018 Tentang Penguatan Fungsi Kawasan Taman Nasional Gunung Merapi Melalui Kerja Sama Pemberdayaan Masyarakat. Ketergantungan masyarakat sekitar akan pemanfaatan sumber daya pasir masih sangat tinggi. Selain pemanfaatan pasir, masyarakat juga melakukan aktivitas dalam mendukung pengelolaan Taman Nasional Gunung Merapi yaitu : patroli bersama petugas TNGM, penanaman di kawasan TNGM, dan terlibat dalam pemadaman kebakaran hutan dan pengembangan Obyek Wisata Alam (OWA) Jurang Jero.ABSTRACTCommunity interaction with Mount Merapi National Park existed long before the national park was established. One form of interaction that is still carried out by the community Ngablak Viilage is the utilization of sand in the Kali Putih area. The aim of this study was to determine the interaction of the community Ngablak Village in the utilization of sand in the Kali Putih area, the Special Reconstruction and Mitigation Zone. The research method used in this research was a survey method. Interviews were conducted directly with communities carrying out activities in the Kali Putih area, the Special Zone for Mitigation and Reconstruction of Mount Merapi National Park. The determination of informants was carried out by accidental sampling where the informants were determined by chance in the field while carrying out activities to exploit sand resources in the Kali Putih area. The results of the interviews were then processed using qualitative descriptive analysis. Based on the results of information retrieval in the field, some information was obtained including sand utilization activities that were carried out in 1977. Community interaction in the use of sand in Kali Putih is legally protected in the form of a conservation area partnership with the PKS document Number: PKS.34 / BTNGM / TU / Kons / 04 / 2018 and 08 / PMH / 04/2018 concerning Strengthening the Function of the Mount Merapi National Park Area through Community Empowerment Cooperation. The dependence of the surrounding community on the utilization of sand resources is still very high. In addition to the utilization of sand, the community also carries out activities in supporting the management of Mount Merapi National Park, namely: patrolling with MMNP officers, planting in the MMNP area, and being involved in extinguishing forest fires and developing the Jurang Jero Nature Tourism Object.

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Woodward, Josh. "Selling Mount Buffalo National Park: Victorian Railways, Harold Clapp and the Blueprint for National Park Promotion in Australia." Journal of Australian Studies 45, no. 3 (July 3, 2021): 371–84. http://dx.doi.org/10.1080/14443058.2021.1954683.

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Faizin and Bambang Azis Nur. "Landslides susceptibility mapping at Gunung Ciremai National Park." E3S Web of Conferences 31 (2018): 12010. http://dx.doi.org/10.1051/e3sconf/20183112010.

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In addition to agriculture, tourism became one of primary economic income for communities around Mount Ciremai, West, Java. Unfortunately, the landscape of West Java has many potential causes to disasters, mainly landslides. Mapping of disaster susceptibility area is needed as a consideration of tourism planning. The study was conducted in Gunung Ciremai National Park, West Java. This paper propose a methodology to map landslides susceptibilities based on spatial data. Using Geographic Information System tools, several environmental parameters such as slope, land use, elevation, and lithology are scored to build a landslide susceptibility map. Then, susceptibility map is overlaid with Utilization Zone.

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Noviati Sadikin, Pipin, Sri Mulatsih, Hadi Susilo Arifin, and Bambang Pramudya Noorachmat. "ANALYSIS OF SUSTAINABILITY STATUS OF ECOTOURISM IN MOUNT RINJANI NATIONAL PARK." Jurnal Analisis Kebijakan Kehutanan 17, no. 1 (May 29, 2020): 33–51. http://dx.doi.org/10.20886/jakk.2020.17.1.33-51.

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Rees, Andrew B. H., and Les C. Cwynar. "Evidence for early postglacial warming in Mount Field National Park, Tasmania." Quaternary Science Reviews 29, no. 3-4 (February 2010): 443–54. http://dx.doi.org/10.1016/j.quascirev.2009.10.003.

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Cameron, Nigel G., Peter A. Tyler, Neil L. Rose, Simon Hutchinson, and Peter G. Appleby. "The recent palaeolimnology of Lake Nicholls, Mount Field National Park, Tasmania." Hydrobiologia 269-270, no. 1 (October 1993): 361–70. http://dx.doi.org/10.1007/bf00028035.

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Mar’atusholihah, Euis Rahmah, E. K. S. Harini Muntasib, and Siti Badriyah Rushayati. "Tourism Hazard Mitigation in Mount Rinjani National Park, West Nusa Tenggara." Social Science, Humanities and Sustainability Research 2, no. 2 (June 18, 2021): p5. http://dx.doi.org/10.22158/sshsr.v2n2p5.

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Mountaineering tourism in Mount Rinjani National Park has various potential natural hazards and requires improved mitigation to ensure tourism security and sustainability. The purpose of this research is to identify the perceptions of tourism actors on the tourism hazards, inventory the types of tourism hazards that occur and mitigate the hazards that have been carried out, and develop tourism hazard mitigation. The methods used in this research are interviews, field observations, and literature studies. Public perceptions of the mountaineering tourism hazard are included in the good category, which means people already know and understand the type and risk of hazard tourism. The types of tourism hazards that have occurred are earthquakes, landslides, volcanic activity, fires, ravines, slippery ravines, cold temperatures, fog, wildlife, and plant hazard. The mitigation that has been carried out consists of mitigation before the hazard event and after the hazard event. Mitigation efforts are divided into regulations, facilities and infrastructure, education, and awareness programs. It is necessary to improve mitigation through addition and improvement of climbing procedures and hazard management procedures, improvement of hiking hazard maps, improvement quality of facilities to minimize damage, making secure infrastructure as a means of warning, security, and emergency response, and socialization/education-related hazard mitigation and how to deal with it.

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Haryadi, Haryadi, Sunarto Sunarto, and Sugiyarto Sugiyarto. "Vegetation Analysis of the Secondary Forest Area of Mount Merapi National Park." Jurnal Biodjati 4, no. 1 (May 28, 2019): 50–57. http://dx.doi.org/10.15575/biodjati.v4i1.4239.

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Mount Merapi National Park (MMNP) is a natural con-servation area with the main function of preserving the diversity of plants, animals and their ecosystems. In 2010, Mount Merapi suffered a large eruption which caused damage to the forest ecosystem inside. One of the locations that suffered severe damage was at Cangkrin-gan Resort. After the eruption, the affected vegetation began to grow again. The purpose of this study is to monitor and determine the di-versity of secondary forest plants in the MMNP area. The method used was a method of path and use a point-intercept transect as the sam-pling unit. The results showed that after the eruption, the Acacia de-curens dominated at each level starting from sapling, poles and trees. Based on the results of the study showed that the eruption of Mount Merapi that occurred in 2010 resulted in a change in vegetation struc-ture in the area with the Shannon-Weiner diversity index which is still low, amounting to 1.86 for seedling, 1.32 for the sapling and 0.22 for poles. At the tree level 100% is still dominated by Acacia decurens.

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Herrero, Hannah, Peter Waylen, Jane Southworth, Reza Khatami, Di Yang, and Brian Child. "A Healthy Park Needs Healthy Vegetation: The Story of Gorongosa National Park in the 21st Century." Remote Sensing 12, no. 3 (February 3, 2020): 476. http://dx.doi.org/10.3390/rs12030476.

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Understanding trends or changes in biomass and biodiversity around conservation areas in Africa is important and has economic and societal impacts on the surrounding communities. Gorongosa National Park, Mozambique was established under unique conditions due to its complex history. In this study, we used a time-series of Normalized Difference Vegetation Index (NDVI) to explore seasonal trends in biomass between 2000 and 2016. In addition, vegetation directional persistence was created. This product is derived from the seasonal NDVI time series-based analysis and represents the accumulation of directional change in NDVI relative to a fixed benchmark (2000–2004). Trends in precipitation from Climate Hazards Group InfraRed Precipitation with Station data (CHIRPS) was explored from 2000–2016. Different vegetation covers are also considered across various landscapes, including a comparison between the Lower Gorongosa (savanna), Mount Gorongosa (rainforest), and surrounding buffer zones. Important findings include a decline in precipitation over the time of study, which most likely drives the observed decrease in NDVI. In terms of vegetation persistence, Lower Gorongosa had stronger positive trends than the buffer zone, and Mount Gorongosa had higher negative persistence overall. Directional persistence also varied by vegetation type. These are valuable findings for park managers and conservationists across the world.

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Fasandra, Fernando, Adhi Trirachmadi Mumin, and Nurbaeti Nurbaeti. "Analysis of Potential Mountaineering Tourism in Mount Gede Pangrango National Park in West Java." TRJ Tourism Research Journal 3, no. 1 (April 30, 2019): 47. http://dx.doi.org/10.30647/trj.v3i1.48.

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This study aims to determine the dominant factors in potential mountaineering tourism and analyze potential strategies in terms of SWOT. This research was using a combination of qualitative and quantitative methods. The strategy was analyzed using Strengths, Weaknesses, Opportunities, and Threats (SWOT) methods on indicators of natural tourist attraction in the form of land, accessibility, management and service, climate, facilities / infrastructure, availability of clean water, security, and marketing. Quantitative data was collected using a questionnaire with a Likert scale, while qualitative data was collected through observation, interviews, and documentation. Respondents for quantitative data were 100 tourists, and those for qualitative data were 21 informants consisting of technical field managers, communities, community climbers, and traveler. The results of the study showed an analysis of the potential of mountain climbing tourism in Mount Gede Pangrango National Park is quite potential and development strategy is needed. The findings in this study show SWOT matrix analysis of policy strategies for potential mountain climbing tourism in Mount Gede Pangrango National Park has the power and opportunity to develop more Progressive Strategy by making Mount Gede Pangrango National Park excellent mountain climbing tourism with its natural beauty and uniqueness.

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Nebasifu, Ayonghe Akonwi, and Ngoindong Majory Atong. "Discourses of Cultural Continuity among the Bakweri of Mount Cameroon National Park." Culture and Local Governance 6, no. 2 (July 9, 2020): 103–21. http://dx.doi.org/10.18192/clg-cgl.v6i2.4754.

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In recent years, the separation of people from their land through protected areas and conservation initiatives of local governance has been at the core of criticism in the people–park discourse. However, vital questions remain as to how people maintain cultural relations to parks and their peripheral zones. This paper explores circumstances where people are not entirely disconnected from their culture despite the state management of Mount Cameroon National Park (MCNP) in West Africa. In this example, people uphold subsistence activities and spiritual interaction with ancestors and deities steered under the umbrella of ritual beliefs. Based on an ethnographic inquiry among the Bakweri in the southwest region of Cameroon, we found that factors of remote settlement, an urge for collective assurances among people, and a sense of belonging in an ethnic group enhance a reciprocal attachment between people and place. This observation helps bridge gaps in people–park relations through cultural continuity.

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Kondratieff, B. C., R. A. Lechleitner, and R. E. Zuellig. "ADDITIONS TO THE STONEFLIES (PLECOPTERA) OF MOUNT RAINIER NATIONAL PARK, WASHINGTON, U.S.A." Entomological News 117, no. 4 (September 2006): 461–63. http://dx.doi.org/10.3157/0013-872x(2006)117[461:attspo]2.0.co;2.

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Parson, Robert E., and Arthur D. Martinson. "The Wilderness above The Sound: The Story of Mount Rainier National Park." Western Historical Quarterly 19, no. 1 (January 1988): 67. http://dx.doi.org/10.2307/969800.

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Larashati, Inge. "COMPOSITION OF UNDER-SHRUBS SPECIES IN MOUNT SALAK NATIONAL PARK, WEST JAVA." Berkala Penelitian Hayati 17, no. 1 (December 31, 2011): 5–8. http://dx.doi.org/10.23869/bphjbr.17.1.20112.

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Lund, Christian, and Noer Fauzi Rachman. "Indirect Recognition. Frontiers and Territorialization around Mount Halimun-Salak National Park, Indonesia." World Development 101 (January 2018): 417–28. http://dx.doi.org/10.1016/j.worlddev.2017.04.003.

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Caroli, Aolo, Daniele Panzeri, and Barry Haack. "Sagarmatha National Park (Mount Everest) Visitor Survey and Analysis (Everest Visitor Survey)." Tourism Review International 17, no. 2 (October 15, 2013): 115–29. http://dx.doi.org/10.3727/154427213x13728688260956.

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44

Larson, Gary L. "Sunrise to Paradise: The Story of Mount Rainier National Park. Ruth Kirk." Quarterly Review of Biology 74, no. 4 (December 1999): 459–60. http://dx.doi.org/10.1086/394131.

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45

Kings, Stephen J. "A comparative study of the forest avifauna in Mount Elgon National Park." Bulletin of the African Bird Club 4, no. 2 (September 1997): 99–102. http://dx.doi.org/10.5962/p.308936.

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46

Hafizhasando, R., M. Rahayuningsih, and S. Saptono Parmin. "Fungi in Selo hiking trail of mount Merbabu national park Central Java." Journal of Physics: Conference Series 1918, no. 5 (June 1, 2021): 052033. http://dx.doi.org/10.1088/1742-6596/1918/5/052033.

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47

Fitriani, A. A., M. Rahayuningsih, and E. S. Rahayu. "Species richness of mosses in selo hiking trails mount merbabu national park." Journal of Physics: Conference Series 1918, no. 5 (June 1, 2021): 052031. http://dx.doi.org/10.1088/1742-6596/1918/5/052031.

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Denny, T. Setyawati, T. Kalima, M. Wardani, Zuraida, R. A. Fambayun, and Adi Susilo. "The association among dominant tree species in mount Halimun Salak National Park." IOP Conference Series: Earth and Environmental Science 743, no. 1 (May 1, 2021): 012014. http://dx.doi.org/10.1088/1755-1315/743/1/012014.

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Nurlaila, Ai, Ika Karyaningsih, Nina Herlina, Iing Nasihin, and Bambang Yudayana. "Diversity of insect pollinator on farmland near to mount Ciremai National Park." IOP Conference Series: Earth and Environmental Science 819, no. 1 (July 1, 2021): 012062. http://dx.doi.org/10.1088/1755-1315/819/1/012062.

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50

Purwanto, Sulis. "ECOLOGICAL RESTORATION IN NATURAL CONSERVATION TOURISM AREA." International Journal of Tourism, Heritage and Recreation Sport 1, no. 1 (June 26, 2019): 27–31. http://dx.doi.org/10.24036/ijthrs.v1i1.7.

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Ecotourism is a concept of tourism development that pays attention to the physical, economic and sociocultural environment and provides positive benefits to local communities and tourist experience. The concept of ecotourism that can be applied in national park areas is ecological restoration. This study aims to determine the application of ecological restoration in nature-based tourism areas. The method used is descriptive qualitative by conducting observations, interviews and literature studies. The results show that ecological restoration is part of the concept of ecotourism that can be applied in the national park area. Ecological restoration is the most important part of ecotourism development. Examples of the application of ecological restoration in the area of Mount Merapi is by replanting trees after eruption and conservation of water. Ecological restoration is carried out to improve the quality of the damaged nature in accordance with its original state and can also support tourism areas around the National Park of Mount Merapi such as Tlogo Muncar, Goa Japan and Plawangan Turgo Hill.

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