• 한국의류산업학회지
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• 제20권4호
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• pp.379-388
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• 2018

The Hawaiian shirt, also known as the Aloha shirt, is a short-sleeved, colorful shirt with traditional Polynesian designs (e.g., hibiscus, fish) originating in Hawai'i. The shirt was selected for study because it is a unique garment that originated in the Hawaiian Islands in the late $19^{th}$ and $20^{th}$ centuries and marketed as a tourist product but was eventually adopted as appropriate residential clothing by the $mid-20^{th}$ century, however with different aesthetic details. Today, it is assumed by Hawaiian Island residents that tourists demonstrate poor taste when selecting a Hawaiian shirt. The purposes of this study are to examine the validity of the assumption that tourist taste and resident taste in Hawaiian shirts are different and to investigate the current Hawaiian shirt market change. For this study, 555 questionnaires were obtained from tourists and residents, and 10 Hawaiian shirt retailers/wholesalers participated in in-depth interviews. The results indicated that differences do exist between tourists' and residents' preferences for print designs and colorway. The market change of Hawaiian shirts was also recognizable in that an increasing number of tourists select Hawaiian shirts similar to resident customers, as part of their routine lives rather than as holiday or vacation garments. Other differences in Hawaiian shirt shopping behavior included the findings that tourists consider fabrication less important than resident customers who consider fabrication more (i.e., cotton 100%). By using both quantitative and qualitative methods, this study contributes to the fashion design and marketing field as well as help manufacturers and retailers with their merchandise and distribution plans.

• ALGAE
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• 제37권4호
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• pp.249-264
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• 2022

Two genera of the Rhodymeniales, Halopeltis and Leptofauchea, are here reported for the first time from the Hawaiian Islands and represent the deepest records for both genera. Molecular phylogenetic analyses of cytochrome oxidase subunit I (COI), rbcL, and large subunit ribosomal DNA (LSU) sequences for Hawaiian specimens of Leptofauchea revealed one well-supported clade of Hawaiian specimens and three additional lineages. One of these clades is described here as Leptofauchea huawelau sp. nov., and is thus far known only from mesophotic depths at Penguin Bank in the Main Hawaiian Islands. L. huawelau sp. nov. is up to 21 cm, and is the largest known species. An additional lineage identified in the LSU and rbcL analyses corresponds to the recently described L. lucida from Western Australia, and is a new record for Hawai'i. Hawaiian Halopeltis formed a well-supported clade along with H. adnata from Korea, the recently described H. tanakae from mesophotic depths in Japan, and H. willisii from North Carolina, and is here described as Halopeltis nuahilihilia sp. nov. H. nuahilihilia sp. nov. has a distinctive morphology of narrow vegetative axes that harbor constrictions along their length. The current distribution of H. nuahilihilia includes mesophotic depths around W. Maui, W. Moloka'i, and the island of Hawai'i in the Main Hawaiian Islands. Few reproductive characters were observed because of the small number of specimens available; however, both species are distinct based on phylogeny and morphology. These descriptions further emphasize the Hawaiian mesophotic zone as a location harboring many undescribed species of marine macroalgae.

• 한국의상디자인학회지
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• 제9권2호
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• pp.59-68
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• 2007

"Aloha" is the Hawaiian word that extends the warmth friendliness, and pride of the Hawaiian people to their island's visitors. The aloha shirt truly symbolizes aloha sprit to islanders and visitors alike. The earliest foreign settlers in the Hawaiian Islands were the Chinese and Japanese. They brought with them their myriad talents and trades, among them the art of tailoring. In July of 1936, a shirtmaker named Ellery J.Chun coined the term "Aloha Shirt" an apt characterization for such an eloquent garment. He was the first to make the shirt on a commercial basis. The shirt sold for as little as a dollar in Chun's own King-Smith store. The genuine aloha shirt is now regaled as a work of art and avidly sought out by collectors. When tourism came to Hawaii in the late 1930s, these unusal shirts were among the first thing that visitors had to have. Local designers and tailors worked quickly to meet the demand and began to expand the range of decoration to include palm trees and romantic beaches, tropical jungles and volcanoes, exotic flowers and scenes from polynesian legend. Therefore the aloha shirt had been born. The functional use of creative colors and amazing artistic renderings in these shirts certainly capture the simplicity and sprit of Hawaii. Aloha shirt is dress that display mystery and charm of Hawaii and cultural symbol of condensed Hawaiian mind. Furthermore, the innocence with which Hawaiians formerly translated their life and heritage onto fabric ranks these shirts with the finest of American folk art. Aloha shirt is made from cotton, silk, rayon in present and past. Most important design element of Aloha shirt is print pattern. Main print pattern of Aloha shirt are all over pattern, horizontal pattern, border pattern, Japanese pattern, picture pattern and back panel pattern. In this study I investigate the design characteristics and development process of aloha shirt.

• Ocean and Polar Research
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• 제23권1호
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• pp.23-34
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• 2001

Geochemical and Sr-Nd isotopic compositions and K-Ar ages are analyzed in volcanic rocks from Weno Island, Caroline Islands. Seven Weno lava samples of alkali basalt and basaltic trachyandesite are aphyric or sparsely phyric comprising olivine, plagioclase, and clinopyroxene phenocrysts. Whole-rock geochemical variation of Weno lavas reflects main fractional crystallization of olivine and Cr-spinel phenocrysts. Newly determined K-Ar ages of Weno lavas range from 6.7 to 11.3 Ma (late Miocene), indicating their formation during primary volcanic stage of Chuuk Islands. Trace element compositions of Weno lavas are very similar to those of typical ocean island basalts (OIBs), suggesting their formation during intra-plate mantle plume activity. The plume composition is isotopically very similar to that of Hawaiian hot spot. However, the age span of Chuuk volcanism is longer than that of the other individual volcanoes in the Pacific.

• 환경생물
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• 제41권1호
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• pp.54-59
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• 2023

Lovenia elongata is a member of the family Loveniidae and is one of the most common tropical echinoids. This species has a broad distribution range in the sub- and tropical regions of the Indo-Pacific Ocean, extending from the Mozambique to the Hawaiian Islands, and from southern Japan to northern Australia. It is commonly found in subtidal areas and on coral reefs within these regions. This species was for the first time recorded from the Ulleungdo Island, Korea. This species is characterized by a teardrop-shaped test that reaches up to 5 cm in length, with a deep groove at the front and tapered at the back end. The petaloid is not obvious, and the primary spines are long and banded. This study is the first to report the newly recorded L. elongata in Korea.

• 암석학회지
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• 제7권1호
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• pp.1-14
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• 1998

당산봉 화산은 제주도 서쪽 끝 해안에 위치하며, 응회구, 분석구, 용암대지 및 애추층 등으로 구성된다. 이들의 암상과 층서는 써제이언분출, 스트롬볼리언분출, 하와이언분출 순으로 전개되는 화산 과정과 외력쇄설 지표과정을 나타낸다. 당산봉 응회구는 마그마와 해수가 상호작용하여 스팀폭발함으로서 형성되는 써쩨이언분출에 의한 구조물이다. 이 분출은 초기에 습윤한 테프라수지상분사 활동상이었고, 중기에 보다 덜 습윤한 테프라의 연속분승 활동상과 테프라수지상분사 활동상이 교대로 진행되었으며, 후기에 보다 건조한 초써쩨이언분사 활동상으로 전환되었다. 분석구는 응회구의 축조로 외부 물의 완전한 제한으로 인해 써제이언분출이 종식되고 스트롬볼리안분출로 전환됨으로써 형성되었다. 이 분출은 초기에 분석 위주로 포출하였으며 후기에 스패터 위주로 포출하는 활동상으로 변화되었다. 용암대지는 화도내 마그마 개스의 고갈로 폭발력이 소진되어 하와이언분출로 전환되므로써 형성되었다. 이 분출은 초기에 용암분천 활동상 위주로 진행되었으나 후기에 용암분류 활동상으로 변화되었다.

• 동굴
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• 제4호
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• pp.41-50
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• 1996

The coastal plains of the Puna and Ka' u Districts of the island of Hawaii are a contradiction to the popular view that the island of Hawaii is a tropical rain forest or a vegetated landscape with abundant water sour This section of the island lies in the rain shadow of Mauna Loa a Kilauea Volcanoes and receives less than 30 inches of annual precipita When rain does come. it is in the form of sudden down pours. givi residents of the area little time to collect and conserve water. Due to porous nature of the rock. there is no standing surface water. In spite of these harsh climatic conditions. archeological evidence indic that an extensive agriculture complex existed not only along the coast. into the most remote parts of what is called the Ka'u Desert. Pass through these agricultural areas are historic and pre - historic t systems. These trail systems apparently played a significant suppor role for exchange between the ahupua's (classic land divisions of Haw and the geopolitical districts. The question arises as to how could vast agricultural complexes a heavy foot travel over miles of arid land exist without dependable wa sources\ulcorner While planting - pits and mounds were designed to make most efficient use of available water and conserve moisture(Carter 19 9). people involved in planting also needed potable water for surv Most publications and research papers dealing with the early population this area make only oblique reference to springs and wells which t populations depended upon. The Federal Cave Resource Protection Act(1988) has served as imprtus for the National Park Service to look closer at the lava tu caves and fault cracks within Hawaii Volcanoes National Park. P visitors to these underground areas found large volumes of standing wa in fault cracks. and abundant drip areas with the lava tubes. Re observes noted that in most cases. where the cracks and caves we located in the arid sections of the park. there has been extens modifiacation or utilization of these water sources by the early Hawaii and others. The variety of western containers used for collection indica that these water sources were used during historic times. William E described similar water sources in his narrative of his trip around island in 1823(Eills 1979), This report is directed at documenting recent observations and a stimulating further research into early Hawaiian water collection syst It also explores the implications that power and political influence of e chiefs in the arid portions of Hawaii could have been linked to the con of the water resources.

• 지질공학
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• 제24권4호
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• pp.597-608
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• 2014

전 세계적으로 해안지방에서의 지하수자원 이용은 점차 증가하고 있다. 또한 해수침투와 같은 자연재해로 인한 피해는 점차 가중될 것으로 예상되며 기후변화와 같은 환경의 변화는 재해의 속도를 가속화시키고 세계 곳곳에서 상당히 큰 대규모 재해의 형태까지 속출하고 있다. 해안 지하수 및 관련 재해 관련 연구개발은 각국의 대표적 실증 부지 중심으로 기술을 시험하고 검증하는 추세이다. 본 논문에서는 전세계적인 해안 지하수 및 관련 재해 연구의 추세를 파악하고 질적, 양적 성장을 확인하였으며 향후 발전방향을 전망하였다. 또한 해안 지하수의 해석기술을 간략하게 소개하였다. 현재 우리나라 실증 부지 중 제주도의 수문지질학적 특징에 대해 살펴보고 국지적인 해수침투 발생 현황을 파악하였다. 마지막으로 제주도와 규모와 형태가 비슷한 화산섬인 하와이 Oahu 지역의 대수층을 대상으로 해외 연구 동향 및 연구 내용에 대해 소개함으로써 앞으로 제주 지역 및 국내 해안 대수층의 지하수 유동 및 오염에 관한 연구에 접목할 수 있는 연구 방식에 대해 고찰하였다.

• 자원환경지질
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• 제26권1호
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• pp.55-65
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• 1993

Udo Island, some 3 km off the coast of Sungsan Peninsula at the eastern promontory of Cheju Island, occurs in such a regular pattern on the sequences which reprent an excellent example of an eruptive cycle. The island comprises a horseshoe-shaped tuff cone, a nested cinder cone on the crater floor, and a lava delta which extends over northwest from the moat between two cones. The volcanic sequences suggest volcanic processes that start with emergent Surtseyan eruption, progress through Strombolian eruption and end with lava effusion followed by reworking of smooth tephra on the tuff cone. Eruptive environment and hydrology of vent area in the Udo tuff cone are poorly constrained because the stratigraphic units under the tuff cone are unknown. It is thoughl, however, that the tuff cone could be mainly emergent because the present cone deposits show no evidence of marine reworking, and standing body of sea water could play a great role. The emergent volcano is characterized by distinctive steam-explosivity that results primarily from a bulk interaction between rapidly ascending magma and a highly mobile slurry. The sea water gets into the vent by flooding accross or through the top or breach of tephra cone. Udo tuff cone was constructed from Surtseyan eruption which went into with tephra finger jetting activities in the early stage, late interspersed with continuous uprush activities and proceeded to only continuous uprush activities in the last. When the enclosure of the vent by a long-lived tephra barrier would prevent the flooding and thus allow the vent to dry out, the Surtseyan eruption ceased to transmit into Strombolian activities, which constructed a cinder cone on the crater floor of the tuff cone. The Strombolian eruption ceased when magma in the conduit gradually became depleted in gas. In the case of Udo, the last magmatic activity was Hawaiian-type (and/or fountain) which accumulated basalt lava delta. And then the loose tephra of the tuff cone reworked over the moat lava and the northeastern flank.

• 한국어류학회지
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• 제35권1호
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• pp.44-49
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• 2023

둥글넙치과, 별목탁가자미속에 속하는 Bothus pantherinus 1개체가 제주도 서귀포시 대정읍 모슬포항 조간대에서 2022년 8월 14일 처음 채집되었다. 본 개체는 가슴지느러미와 눈주위에 검은 점과 고리 모양의 무늬, 유안측 측선 중앙에 하나의 뚜렷한 반점을 가지는 점, 75개의 측선비늘과 7개의 모래시계 모양의 등지느러미 담기골을 가지는 점 등에서 B. pantherinus로 동정되었다. 미토콘드리아 DNA의 COI 영역 603 bp를 분석한 결과 NCBI에 등록된 B. pantherinus와 잘 일치하였다. 본 종은 인도양, 호주, 일본, 하와이 등 북위 32도에서 남위 32도 사이에 분포하는 것으로 알려져 왔으나 이번 연구를 통해 본 종의 분포역이 한국의 제주도 해역(북위 33도)까지 확장되었다. 국내에 처음 보고되는 본 종의 새로운 국명으로 "벚꽃무늬둥글넙치"를 제안한다.