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Journal articles on the topic 'Sandur'

Author: Grafiati

Published: 4 June 2021

Last updated: 8 February 2022

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1

Firdaus, Elvin Nuril, and Sony Sukmawan. "PERANAN SANDUR KEMBANG DESA DALAM PELESTARIAN KESENIAN SANDUR DI BOJONEGORO, JAWA TIMUR." HUMANIKA 28, no. 1 (May 1, 2021): 17–28. http://dx.doi.org/10.14710/humanika.v28i1.35771.

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Sandur merupakan seni pertunjukan tradisional yang tumbuh dan berkembang di wilayah masyarakat agraris, yaitu masyarakat yang memenuhi kebutuhan hidupnya bersumber dari produksi dan pemeliharaan tanaman dan pertanian. Sandur mengisahkan tentang kehidupan masyarakat agraris, interaksi antarmasyarakat, bercocok tanam, hingga transisi masyarakat agraris menuju masyarakat urban. Salah satu daerah tempt berkembangnya Sandur adalah Bojonegoro. Sandur pernah mencapai masa kejayaannya di Bojonegoro. Seiring berjalannya waktu, Sandur dianggap kurang relevan dengan kehidupan masyarakat modern karena tidak ada penyesuaian dengan perkembangan zaman dan tidak ada regenerasi. Hal tersebut ditambah dengan hantaman modernisasi yang semakin memperburuk keadaan. Penelitian ini bertujuan untuk menjelaskan upaya pelestarian Sandur melalui kelompok Sandur Kembang Desa, yaitu sekelompok pemuda yang mempertahankan kesenian Sandur dengan cara menginovasi cerita dalam Sandur agar dapat diterima masyarakat. Penelitian ini dilakukan di Desa Ledok Kulon, Kecamatan Bojonegoro, Kabupaten Bojonegoro. Pendekatan yang digunakan dalam penelitian ini adalah pendekatan kualitatif dengan desain studi kasus. Data dikumpulkan melalui teknik wawancara tidak terstruktur dan observasi nonpartisipan. Hasil penelitian menunjukkan bahwa eksistensi Sandur terancam punah karena tidak adanya regenerasi dan ceritanya yang dianggap kurang relevan dengan kehidupan masyarakat modern. Hal tersebut menjadikan minat masyarakat terhadap kesenian Sandur semakin berkurang. Sandur Kembang Desa merupakan kelompok kesenian yang menginovasi Sandur di tengah pola kehidupan masyarakat yang bergeser mengikuti arus modernisasi. Inovasi Sandur Kembang Desa terinspirasi dari gaya hidup masyarakat modern, sehingga pertunjukannya mampu menarik perhatian masyarakat. Nilai-nilai yang diangkat dalam cerita Sandur Kembang Desa merupakan nilai-nilai yang relevan dengan masyarakat modern, tanpa mengubah nilai-nilai tradisional Sandur. Adanya inovasi dari Sandur Kembang Desa diharapkan mampu mempertahankan eksistensi Sandur di tengah perkembangan budaya modern.

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2

Sumiyani, Hidayah, and Autar Abdillah. "Sistem Kreativitas Sandur Bojonegoro dalam Pertunjukan “Selendang Kuning”." Gondang: Jurnal Seni dan Budaya 5, no. 1 (May 8, 2021): 127. http://dx.doi.org/10.24114/gondang.v5i1.24551.

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Pertunjukan sandur Bojonegoro dipentaskan di tanah lapang dengan panggung arena dan dibatasi dengan belabar janur kuning. Pada masa pandemi Covid-19, seniman Sandur menciptakan pertunjukan “Selendang Kuning” dengan konsep sandur rumah yaitu sandur yang dipentaskan dalam rumah atau yang dapat disaksikan di rumah. Tujuan penelitian ini adalah mengetahui aspek-aspek kreatifitas yang mendukung penciptaan karya Sandur Bojonegoro dengan konsep rumah. Metode penelitian yang digunakan adalah deskiptif kualitatif, dengan pengumpulan data observasi, wawancara semi terstruktur dan studi kepustakaan. Hasil penelitian kemudian dianalasis menggunakan sistem kreatifitas Mihaly Csikzentmihalyi. Hasil penelitian yang telah dianalisis, ditemukan bahwa karya sandur “Selendang Kuning” yang berkonsep sandur rumah dapat tercipta karena beberapa aspek, yaitu (1)domain yang ditempuh telah mengalami titik fokus pada pengembangan Sandur Bojonegoro ke bentuk dan media yang baru dengan penuh kesadaran memilih untuk mempertimbangkan unsur kepakeman yang harus dipakai ataupun yang tidak digunakan dalam proses penciptaan karya tersebut; (2)ranah dalam pertunjukan mendapatkan dukungan, kolaborasi antar aspek yang memadai; dan (3)individu kreatif dalam karya berupa para pelaku sandur Bojonegoro yang terbuka dengan segala kemungkinan penciptaan.

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3

Krzyszkowski, Dariusz. "The Wartanian Siedlec Sandur (Zedlitzer Sandur) southwards the Trzebnica Hills, Silesian Lowland; Southwestern Poland: re-examination after fifty years." E&G Quaternary Science Journal 43, no. 1 (January 1, 1993): 53–66. http://dx.doi.org/10.3285/eg.43.1.05.

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Abstract. Der Zedlitzer Sander (Siedlec Sandur) in Schlesien, im südwestlichen Polen gelegen, wurde zuerst von M. Schwarzbach im Jahr 1942 beschrieben. Er wurde als ein warthezeitlicher Sander gedeutet, der am Südrand der Stauchmoräne (Trzebnica Hügel, Trzebnica Katzengebirge) entstanden war. Einige neuere Untersuchungen widersprechen dieser Interpretation und negieren das Auftreten warthezeitlichen Eises in Südwest-Polen. Der vorliegende Beitrag präsentiert neue sedimentologische Untersuchungen aus den Ablagerungen des Siedlec Sanders. Das wichtigste Ergebnis dieser Studien ist eine detaillierte Beschreibung einiger klassischer, schon von Schwarzbach beschriebener und einiger neuer Aufschlüsse. Aus diesen Aufschlüssen wurde geschlossen, daß der Siedlec Sander einen eiszeitlichen Schwemmfächer mit Sedimentstrukturen repräsentiere, wie sie auch in Schwemmfächern semiarider Klimate vorkommen. Das glaziofluviatile Material des Schwemmfächers legt nahe, daß seine Sedimentation in einer kalten Polarwüste erfolgte. Dieser Schluß spricht für Schwarzbachs Deutung und nicht für die seiner Opponenten, und er belegt indirekt das Auftreten warthezeitlichen Eises in Schlesien. Im vorliegenden Beitrag wird außerdem die mögliche Ausdehnung des Eises in das Trebnitzer Katzengebirge diskutiert.

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4

Angiel, Piotr. "Variability of Textural Characteristics of Sandur Deposits of Fláajökull and Falljökull (SE Iceland)." Miscellanea Geographica 12, no. 1 (December 1, 2006): 111–17. http://dx.doi.org/10.2478/mgrsd-2006-0013.

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Abstract Studies conducted on the sandurs of Fláajökull and Falljökull aimed at the reconstruction of the dynamics of braided rivers based on the grain size parameters of deposits. The goal of the project was to estimate the degree of deposit transformation and of changes of grain size characteristics as related to the length of transport in contemporary sandur rivers.

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5

Tyas, Galuh Haryanti Manunggaling, and Srihadi Srihadi. "BENTUK DAN FUNGSI SANDUR DI DESA SUKOREJO KECAMATAN PARENGAN KABUPATEN TUBAN." Greget: Jurnal Pengetahuan dan Penciptaan Tari 19, no. 2 (December 28, 2020): 125–41. http://dx.doi.org/10.33153/grt.v19i2.3459.

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Sandur in his show tells about the life of people who have a livelihood as a farmer. The problem in this research is how sandur shows form and how Sandur functions. Based on the object studied, this research uses qualitative method. To discuss the form using the concept of Sal Murgiyanto and I Made Bandem which discuss elements of traditional theater which includes dialogue, decorating, dance, accompaniment music, makeup, costumes and dance. Discussing the problem of function using the concept of SD Humardani which belongs to social functions including entertainment functions, educational functions, and solidarity functions. The results showed that Sandur is a folk art in the form of traditional theater. Sandur has 3 innings in the show, namely the opening section, the contents and the closing part. Sandur's performance form can be seen from the elements of the performance consisting of dialogue, decor, costumes, makeup, accompaniment music, singing, and dance. Sandur function is classified into social functions, namely as entertainment, as education, and as community solidarity. Keywords: Sandur, Shape, Function

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6

Eisendle, Ursula. "Description of Mononchus sandur n. sp. (Nematoda: Mononchidae) and remarks on M. truncatus Bastian, 1865 and M. aquaticus Coetzee, 1968 from a glacial floodplain reach (Großglockner region, Hohe Tauern, Austria)." Nematology 10, no. 6 (2008): 809–18. http://dx.doi.org/10.1163/156854108786161481.

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AbstractFemales and males of a new species of the genus Mononchus were found in an alpine, glacial floodplain reach (2073 m a.s.l.) in the Großglockner region (Hohe Tauern National Park; Austria). Females of Mononchus sandur n. sp. are medium sized (1.5-1.8 mm) with body diam. of 45-65 μm. The buccal cavity is 28-35 × 13-15 μm in size with the dorsal tooth located 65-77% from the buccal cavity base. The distinct amphid openings (4 μm) are located 11 μm posterior to the head and anterior to the dorsal tooth apex. The general appearance of the female is characterised by the shape of the tail with its combination of length and slenderness (224-306 μm; c′ = 7.2-10.8). Males of M. sandur n. sp. are very similar to females with the exception of a shorter tail (147-159 μm). Males have 16 and 18 preanal supplements, 57-68 μm long spicula and 11-14 μm long gubernaculum. Morphometric measurements and ratios were determined for 20 females of M. sandur n. sp., M. truncatus and M. aquaticus, all co-occurring in the floodplain reach. One-way analysis of variance revealed that M. aquaticus, M. truncatus and M. sandur n. sp. differ significantly in 18 out of 20 morphometric traits. A cluster analysis of ten morphometric traits was done to allocate and separate the measurements of the 60 females. Three distinctly separate clusters arose. By calculating the Kappa coefficient (K), it could be shown that the partitioning of individuals in these three clusters was in complete accordance with the species determination (K = 1; P < 0.0001).

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7

Salamon, Tomasz, and Tomasz Zieliński. "Unusual development of sandur sedimentary succession, an example from the Pleistocene of S Poland." Geologos 16, no. 2 (June 1, 2010): 83–99. http://dx.doi.org/10.2478/v10118-009-0007-9.

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Unusual development of sandur sedimentary succession, an example from the Pleistocene of S PolandAn atypical lithological development of outwash deposits in the Carpathians Foreland (S Poland) shows lower and middle parts of the sedimentary succession that are characterized by sinuous palaeochannels. This channel facies consists of laterally accreted sands derived from side bars. The sedimentary environment was a proglacial system of anabranching channels, presumably of anastomosed type. The outwash channel pattern was most probably controlled by the raising base level of the fluvial system. Both proglacial and extraglacial waters were dammed by a sandur within a small upland valley. Aggradation and progradation of the glaciofluvial deposits resulted in progressive rising of the dammed lake level. The low hydraulic gradient of the outwash streams resulted in a sinuous planform as well as a low-energy style of deposition. Afterwards, the rising lake water was drained off through a low watershed and the entire valley became filled with outwash sediments. The bedrock morphology thus became buried and a typical unconfined sandur with a braided channel network developed during the last phase of the glaciomarginal sedimentation (upper part of the sedimentary succession under study).

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8

Loftsdóttir, Kristín, Auður Arna Arnardóttir, Már Wolfgang Mixa, and Guðbjörg Guðjónsdóttir. "Sól og sandur: Ferðir Íslendinga til Kanaríeyja." Tímarit um viðskipti og efnahagsmál 18, no. 1 (August 25, 2021): 45–66. http://dx.doi.org/10.24122/tve.a.2021.18.1.3.

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Rannsóknir á ferðamennsku til Íslands hafa verið í uppgangi síðastliðin ár, en verulega skortir á rannsóknir á utanlandsferðum Íslendinga. Hvort tveggja er þó hluti af þeim hnattræna veruleika sem Ísland er hluti af og vettvangur margvíslegra efnahagslegra gjörninga. Greinin fjallar um ferðir Íslendinga til Kanaríeyja og spyr hvað einkennir ferðir Íslendinga til Kanaríeyja síðasta áratuginn og hverskonar áfangastaður Kanaríeyjar er fyrir Íslendinga. Greiningin styðst við megindleg gögn, þ.e. niðurstöður spurningakönnunnar og greiningu á fyrirliggjandi gögnum frá Hagstofu Kanaríeyja og Ferðamálastofu Íslands. Rannsóknir erlendis endurspegla að spænsk yfirvöld hafa reynt að leggja áherslu á að Kanaríeyjar hafi upp á meira að bjóða en eingöngu sólarlandaferðir. Jafnframt sýna erlendar rannsóknir að mörk milli þeirra sem eru ferðamenn, aðfluttir, eða sem vinna á eyjunum eru oft óljós og flæðandi. Greining megindlegra gagna fyrir greinina sýnir að Kanaríeyjar hafa haft vaxandi mikilvægi sem áfangastaður fyrir ferðalanga frá Íslandi síðasta áratug og þá sérstaklega eyjan Tenerife. Aðdráttarafl Kanaríeyja sem áfangastaðar virðist út frá niðurstöðum könnunarinnar fyrst og fremst vera í tengslum við veðurfar eyjanna og afþreyingu, en bent er jafnframt á að rétt eins og annarstaðar getur hreyfanleiki til eyjanna falið í sér flæðandi hópa þar sem mörk ferðamanna, aðfluttra, eða vinnandi eru ekki alltaf skýr.

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9

Jacobsen, Jógvan í. Lon. "Unges dialektbrug i bygden Sandur på Færøerne." Oslo Studies in Language 11, no. 2 (January 21, 2021): 173–87. http://dx.doi.org/10.5617/osla.8497.

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In this article, dialect changes and variation among young schoolchildren in the island of Sandoy in the Faroe Islands are discussed. The fieldwork was made by a group of students at the University of the Faroe Islands in November 2019 under the guidance of this article’s author. The informants are two groups of 10 and 15 year old schoolchildren. By examining the young generation, we can get information about the ‘state of health’ of the dialect. Here three dialectal variables are examined: (i) The variation of definite and indefinite form of words for family members, for instance the dialectal form mamman ‘the mother’ and the Central Faroese form mamma ‘mother’; (ii) Personal and possessive pronouns in 1st and 2nd person plural in oblique case, for instance the dialect form [o:gʊn] ‘us’ and the Central Faroese form [ɔʰk:ʊn] ‘us’; (iii) The pronunciation of short ó with the dialectal variant [ɔ] and the Central Faroese form [œ], for instance [fɔlk] resp. [fœlk] ‘people’. The first variable shows clearly a tendency towards dialect change in the young generation: the indefinite forms are much more frequent than the dialect counterpart. The use of the pronouns shows a relatively high degree of variation: the dialect forms are more frequently used by the 10 than the 15 year old pupils. The pronunciation of short ó shows variation to a large extent. Here we see the same pattern as we saw for variable 2: the youngest pupils are more likely to use the dialect¬al form [ɔ] than the older ones. On the other hand, variation is much more common in the group of 15 year old pupils. This study shows both stability and change in the dialect of children in Sandoy: Stability in use of the dialectal forms of the personal and possessive pro¬nouns, and variation and change in the two other variables. In a couple of years an underwater tunnel will connect the island of Sandoy with the central part of the islands. In a future scenario this dialect study opens the possibility for comparative studies of the dialect of Sandoy before and after the opening of the tunnel.

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10

ZIELINSKI, TOMASZ, and ANTONIUS J. LOON. "Pleistocene sandur deposits represent braidplains, not alluvial fans." Boreas 32, no. 4 (June 28, 2008): 590–611. http://dx.doi.org/10.1111/j.1502-3885.2003.tb01238.x.

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11

Zielinski, Tomasz, and Antonius Van Loon. "Pleistocene sandur deposits represent braidplains, not alluvial fans." Boreas 32, no. 4 (December 1, 2003): 590–611. http://dx.doi.org/10.1080/03009480310004170.

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12

Heim, Dieter. "Glacier drainage and sandur formation at Kötlujökull, South Iceland." Polar Geography and Geology 9, no. 2 (April 1985): 91–107. http://dx.doi.org/10.1080/10889378509377242.

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13

MARREN, PHILIP M. "Glacier margin fluctuations, Skaftafellsjökull, Iceland: implications for sandur evolution." Boreas 31, no. 1 (June 28, 2008): 75–81. http://dx.doi.org/10.1111/j.1502-3885.2002.tb01057.x.

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14

Marren, Philip M. "Fluvial–lacustrine interaction on Skeiðarársandur, Iceland: implications for sandur evolution." Sedimentary Geology 149, no. 1-3 (May 2002): 43–58. http://dx.doi.org/10.1016/s0037-0738(01)00243-3.

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15

Marren, Philip M., Andrew J. Russell, and E. Lucy Rushmer. "Sedimentology of a sandur formed by multiple jökulhlaups, Kverkfjöll, Iceland." Sedimentary Geology 213, no. 3-4 (January 2009): 77–88. http://dx.doi.org/10.1016/j.sedgeo.2008.11.006.

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16

Marren, Philip M. "Glacier margin fluctuations, Skaftafellsjo¨kull, Iceland: implications for sandur evolution." Boreas 31, no. 1 (March 1, 2002): 75–81. http://dx.doi.org/10.1080/03009480210653.

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17

Kasprzak, Marek, Michał Łopuch, Tadeusz Głowacki, and Wojciech Milczarek. "Evolution of Near-Shore Outwash Fans and Permafrost Spreading Under Their Surface: A Case Study from Svalbard." Remote Sensing 12, no. 3 (February 3, 2020): 482. http://dx.doi.org/10.3390/rs12030482.

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The article presents geomorphological analysis results for two outwash fans (sandurs), Elveflya and Nottingham, in the marginal zone of the Werenskiold Glacier in the south-west part of the Spitsbergen. The main goal of this study was to reconstruct the morphological evolution of these landforms and to identify the permafrost zone under their surface. For this purpose, age data of fossils were compiled and compared with newly exposed and dated fossil tundra in the layer glaciotectonically deformed by the forming glacier end moraine. Using this method, a time frame was identified for the glacier advance and for the simultaneous formation of the outwash plains. It was concluded that the Elveflya surface has been built-up with deposits since the Little Ice Age. Sediment deposition ended in the late 1960s, due to hydrographic changes and the redirection of all proglacial waters towards the Nottingham bay. A photointerpretation analysis based on two orthophotomaps and LANDSAT scenes allowed the identification of five microfans in Elveflya, of which two youngest fans have a twice shorter range than the other three. The sixth microfan is currently shaped by deposits washed from the slope of the end moraine. An additional focus was placed on a currently active sandur, which fills the Nottingham bay, in order to identify its growth rate. The average growth rate of this surface increased from 5700 m2·year−1 over the period of 1985–2000 to 24,900 m2·year−1 over the period of 2010–2017. Electromagnetic measurements carried out on the surfaces of the sandurs demonstrated that the electrical resistivity of the ground is high in the apex of the Elveflya fan (ρ ≥ 1 kΩ.m) and low in its toe (typically ρ < 200 Ω.m), as in the case of the Nottingham fan ground. In the interpretation advanced here, permafrost developed in the proximal part of the Elveflya sandur, which continues to be supplied by fresh groundwaters flowing from the glacier direction. Low electrical resistivity of the ground in the distal part of the outwash fan suggests the absence of ground ice in this zone, which is subjected to the intrusion of salty and comparatively warm seawater, reaching approximately 1 km inland under the surface of the low-elevated marine terrace. The identified zones additionally display different tendencies for vertical movements of the terrain surface, as identified with the Small Baseline Subset (SBAS) method. The proximal part of the Elveflya outwash fan is relatively stable, while its distal part lowers in the summer period by a maximum of 5 cm. The resulting morphological changes include linear cracks having lengths up to 580 m and an arc line consistent with the coastline.

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18

Kumar, R. V. Vinayak, M. R. Patel, B. P. Ravi, and Guruprasad Jagalur. "Pelletisation studies of manganese ore fines from sandur schist belt, Karnataka." Asian Journal of Multidimensional Research (AJMR) 8, no. 4 (2019): 51. http://dx.doi.org/10.5958/2278-4853.2019.00134.4.

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19

MOHAPATRA, B. K., D. S. RAO, B. D. NAYAK, and R. K. SAHOO. "Mineralogical and chemical characteristics of ferromanganese ores from Sandur, Karnataka, India." JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY 91, no. 2 (1996): 48–61. http://dx.doi.org/10.2465/ganko.91.48.

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20

Weyhe, Eivind. "Akrinatjørn, Mølbursvatn and Mølheyggjarnir – three place-names by Sandur on Sandoy." Fróðskaparrit - Faroese Scientific Journal, no. 61 (July 19, 2015): 84. http://dx.doi.org/10.18602/fsj.v0i61.14.

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Three place-names near the village of Sandur are discussed, and suggestions made as to their interpretation. The first element of <em>Akrinatjørn </em>‘Akrinatarn’ is explained as the plant-name <em>akurull </em>(Eriophorum angustifolium). The <em>Mølbur</em>- of <em>Mølbursvatn </em>‘Mølburswater’ is seen as a reflex of *<em>Melberði</em>, compounded of ON <em>melr </em>m. ‘gravel-bank’ and *<em>berði </em>n., a derivative of <em>barð </em>n. ‘edge, rim’; the original name of this lake was thus probably *<em>Melberðisvatn</em>. It is further suggested that the first element of the name <em>Mølheyggjarnir </em>‘the Møl heights’ also comes from an original <em>melr </em>rather than <em>møl </em>f. The confusion of <em>e </em>and <em>ø </em>in <em>Mølbursvatn </em>and <em>Mølheyggjarnir </em>is to be seen in the light of the delabialisation that characterises the dialect of this area.

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21

LANDVIK, JON Y., and JAN MANGERUD. "A Pleistocene sandur in western Norway: facies relationships and sedimentological characteristics." Boreas 14, no. 2 (January 16, 2008): 161–74. http://dx.doi.org/10.1111/j.1502-3885.1985.tb00911.x.

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22

Olsen, Henrik, and Frank Andreasen. "Sedimentology and ground-penetrating radar characteristics of a Pleistocene sandur deposit." Sedimentary Geology 99, no. 1 (September 1995): 1–15. http://dx.doi.org/10.1016/0037-0738(94)00136-i.

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23

Kumar, B. V. Suresh, R. K. Sunil Kumar, and K. N. Prakash Narasimha. "Water Quality Assessment in and Around Sandur Taluk, Bellary District, South India." International Journal of Advanced Earth Science and Engineering 5, no. 1 (March 15, 2016): 325–32. http://dx.doi.org/10.23953/cloud.ijaese.203.

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24

Lüthgens, Christopher, Matthias Krbetschek, Margot Böse, and Margret C. Fuchs. "Optically stimulated luminescence dating of fluvioglacial (sandur) sediments from north-eastern Germany." Quaternary Geochronology 5, no. 2-3 (April 2010): 237–43. http://dx.doi.org/10.1016/j.quageo.2009.06.007.

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25

Kerur, B. R., T. Rajeshwari, S. Anilkumar, K. Narayani, and A. K. Rekha. "Gamma spectrometric analysis of ore samples from Sandur of Bellary, Karnataka, India." Journal of Radioanalytical and Nuclear Chemistry 294, no. 2 (January 4, 2012): 191–96. http://dx.doi.org/10.1007/s10967-011-1599-4.

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26

Hanáček, Martin, Daniel Nývlt, Jan Flašar, Václav Stacke, Peter Mida, Jiří Lehejček, Gabriela Tóthová, et al. "New methods to reconstruct clast transport history in different glacial sedimentary environments: Case study for Old Red sandstone clasts from polythermal Hrbyebreen and Bertilbreen valley glaciers, Central Svalbard." Czech Polar Reports 3, no. 2 (June 1, 2013): 107–29. http://dx.doi.org/10.5817/cpr2013-2-13.

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The objective of this study were Little Ice Age (LIA) to recent subglacial tills, glaciofluvial sediments of proglacial sandur, esker sediments and sediments of moraine-mound complexes of Hrbyebreen polythermal valley glacier and LIA to recent sediments of lateral moraine, frontal moraine, ice-cored moraine and glaciofluvial sediments of proglacial sandur of Bertilbreen polythermal valley glacier. Fossil (probably early Holocene) subglacial and supraglacial tills and sediments of coarse-grained glaciomarginal delta of Bertilbreen have also been studied. The research focused on Old Red sandstone clasts, for which roundness, shape and striation presence have been investigated. The results from this research led to the proposal of new methodological approaches. It is mainly the covariant plot of striations and RA (the share of striated clasts versus the share of very angular and angular clasts), which effectively differentiate subglacial tills from glaciofluvial sediments and allows for identification of the source material of moraine-mound complexes, especially the oldest, more degraded parts near the maximum LIA glacier extent. The second is the covariant plot of distance and RS index (the distance from the starting point versus the share of subangular and subrounded clasts) to present downstream roundness trends in proglacial glaciofluvial sediments. The research confirmed the crucial role of lithological properties of thinly bedded rocks on the shape of these rock clasts in sediment and a minimum impact of passive and active transport on the clast shape modification.

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Manikyamba, C., and S. M. Naqvi. "Late Archaean Mantle Fertility : Constraints from Metavolcanics of the Sandur Schist Belt, India." Gondwana Research 1, no. 1 (October 1997): 69–89. http://dx.doi.org/10.1016/s1342-937x(05)70006-x.

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Pisarska-Jamroży, Małgorzata, and Tomasz Zieliński. "Pleistocene sandur rhythms, cycles and megacycles: Interpretation of depositional scenarios and palaeoenvironmental conditions." Boreas 43, no. 2 (September 4, 2013): 330–48. http://dx.doi.org/10.1111/bor.12041.

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Satish Kumar, K., K. N. S. S. S. Srinivas, V. Pradeep Kumar, P. Prabhakara Prasad, and T. Seshunarayana. "Magnetic Mapping of Banded Iron Formation of Sandur Schist Belt, Dharwar Craton, India." Journal of the Geological Society of India 91, no. 2 (February 2018): 174–80. http://dx.doi.org/10.1007/s12594-018-0831-z.

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Angiel, Piotr. "Geographical Research of the 30th Polish Antarctic Expedition at Arctowski Polish Station (King George Island, South Shetland Islands, Antarctica)." Miscellanea Geographica 13, no. 1 (December 1, 2008): 51–56. http://dx.doi.org/10.2478/mgrsd-2008-0005.

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Abstract This paper presents the scope of geographical research conducted at Arctowski Station during the 30th Polish Antarctic Expedition. The research included meteorological, climatological, geomorphological and glaciological issues. During the expedition, research was conducted on sandur sediments on the outwash plain of Sphinx Glacier, the size of the aeolian transport, intensity of periglacial phenomena, and the way in which environmental conditions are recorded on quartz grains collected on the Admiralty Bay beaches. Detailed measurements of the basic meteorological components were made, geomorphological maps of the outwash plains of Sphinx, Baranowski, and Windy Glaciers were also completed.

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Dietrich, Pierre, Jean-François Ghienne, Alexandre Normandeau, and Patrick Lajeunesse. "Upslope-Migrating Bedforms In A Proglacial Sandur Delta: Cyclic Steps From River-Derived Underflows?" Journal of Sedimentary Research 86, no. 2 (February 2016): 113–23. http://dx.doi.org/10.2110/jsr.2016.4.

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Szafraniec, Joanna E. "Paleoflood marks in sandur morphometry as the result of the glacier surge (NW Poland)." Hydrology Research 44, no. 2 (December 4, 2012): 264–80. http://dx.doi.org/10.2166/nh.2012.151.

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In the Pomeranian marginal zone of the last Pleistocene glaciation specific morphometric features are found. They represent indicators of surging events affecting the individual outlet glacier lobes of the Scandinavian Ice Sheet margin. They are assumed to have been active during the climate warming of the Weichselian glaciation decay. Many tunnel valleys deep-rooted in the proximal slopes of the terminal moraine ridge with incised gorges and wide extramarginal sandur fans spread from the mouths to the forefield. The relatively low relief intensity factor, the fluvioglacial sediments covering distal slopes of the terminal moraines and ‘washed out’ older forms may be considered as indirect evidence of outburst floods caused by a re-canalization of the subglacial drainage system. The morphometry of the palaeochannels in the gorge profiles are used to calculate estimates of extreme discharges (c. 5 × 103–105m3s–1).

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Thomas, G. S. P., M. Connaughton, and R. V. Dackombe. "Facies variation in a Late Pleistocene supraglacial outwash sandur from the Isle of Man." Geological Journal 20, no. 3 (April 30, 2007): 193–213. http://dx.doi.org/10.1002/gj.3350200302.

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Rajendran, N., and K. V. Krishnamurthy. "Report on the National Field Workshop on Iron Ore Deposits of Hospet-Sandur Sector." Journal of the Geological Society of India 95, no. 2 (February 2020): 212–13. http://dx.doi.org/10.1007/s12594-020-1412-5.

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Magilligan, F. J., B. Gomez, L. A. K. Mertes, L. C. Smith, N. D. Smith, D. Finnegan, and J. B. Garvin. "Geomorphic effectiveness, sandur development, and the pattern of landscape response during jökulhlaups: Skeiðarársandur, southeastern Iceland." Geomorphology 44, no. 1-2 (April 2002): 95–113. http://dx.doi.org/10.1016/s0169-555x(01)00147-7.

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Flindt, Anne-Cécile, Ívar Örn Benediktsson, Helena Alexanderson, and Per Möller. "A pre-LGM sandur at Fiskarheden in NW Dalarna, central Sweden - sedimentology and glaciotectonic deformation." Boreas 47, no. 3 (January 11, 2018): 711–37. http://dx.doi.org/10.1111/bor.12301.

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Manikyamba, C., S. M. Naqvi, S. Moeen, T. Gnaneshwar Rao, V. Balaram, S. L. Ramesh, and G. L. N. Reddy. "Geochemical heterogeneities of metagraywackes from the Sandur schist belt: implications for active plate margin processes." Precambrian Research 84, no. 3-4 (October 1997): 117–38. http://dx.doi.org/10.1016/s0301-9268(97)00022-3.

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Kumar, R. V. Vinayak, M. R. Patil, and B. P. Ravi. "Amenability to beneficiation of a low grade Manganese ore fines from Sandur Region, Karnataka, India." Research Journal of Science and Technology 10, no. 4 (2018): 291. http://dx.doi.org/10.5958/2349-2988.2018.00041.4.

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Laute, Katja, and Achim A. Beylich. "Characteristics of floodplain deposits within a braided sandur system in upper erdalen (nordfjord, western norway)." Geografiska Annaler: Series A, Physical Geography 92, no. 2 (June 2010): 211–23. http://dx.doi.org/10.1111/j.1468-0459.2010.00390.x.

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Syvitski, James P. M. "Marine Geology of Baie des Chaleurs." Géographie physique et Quaternaire 46, no. 3 (November 29, 2007): 331–48. http://dx.doi.org/10.7202/032918ar.

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RÉSUMÉ La baie des Chaleurs, quatrième estuaire en importance de l’est du Canada, est un large bassin peu profond rempli de sédiments non consolidés d'une épaisseur allant jusqu'à 50 m. La répartition de cette masse sédimentaire est en partie imposée par le réseau de drainage datant du Cénozoïque (Tertiaire ou Quaternaire), qui suit les principaux éléments structuraux du socle sédimentaire sous-jacent. Les dépôts de contact glaciaire pleistocenes, y compris le till, sont généralement minces ou absents. Toutefois, au centre et vers l’extérieur de la baie, les chenaux cénozoïques renferment les accumulations morainiques linéaires, jusqu'à 30 m d'épaisseur, qui pourraient signaler l'emplacement final du dôme de la Gaspésie. Six grands cônes glaciomarins identifient les exutoires en fonction pendant la phase de retrait des calottes régionales. Ces dépôts pléistocènes ont en partie été érodes par des chenaux de drainage fluvioglaciaires pendant une phase de bas niveau marin (-90 m), vers 9000 BP. Par la suite, au cours de la transgression marine de l'Holocène inférieur à moyen, les sédiments glaciaires ont été soumis à l’érosion par les vagues. Les dépôts s'amincissent donc en eaux peu profondes et sont caractérisés par la présence de terrasses parallèles à la rive et des surfaces de sédiments grossiers le long des marges de la baie. À 7000 BP, le complexe de sandur qui occupait le fond peu profond de la baie a aussi été atteint par la transgression marine. La surface du delta était protégée par une barrière morainique. Les sédiments de l'Holocène inférieur ont d'abord été déposés dans les eaux plus profondes du centre et de l'entrée de la baie et ont subséquemment formé une pellicule sur le sandur du fond de la baie à mesure que le niveau marin montait. Ces sédiments montrent une progression dans la stratification et la granulométrie en relation avec les fluctuations du niveau marin et des sources sédimentaires. Les conditions océanographiques modernes se sont établies il y a environ 5000 ans.

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Worsley, Peter. "Esmark's End Moraine and the Glacial Theory from a British Perspective." Earth Sciences History 27, no. 1 (January 1, 2008): 12–30. http://dx.doi.org/10.17704/eshi.27.1.6184m4v727vg0403.

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An end moraine (Vassryggen) and associated sandur, described by Jens Esmark as early as 1824, was the first pre-Neoglacial glacigenic landform association to be recognised as such. It formed the most important element of a range of evidence used by Esmark in support of his continental-scale glaciation hypothesis. The career of Esmark, who became a foundation professor of the Royal Frederick University in Christiania (Oslo), is outlined and his influence on the development of the glacial theory in Britain is appraised, as is the role of his associate Robert Jameson in Edinburgh. A sketch of the glacial geology of the Forsand area of southwest Norway examines the Vassryggen and allied landforms in the context of deglaciation and sea level change at the close of the Younger Dryas stadial.

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Kazakova, A. I., A. A. Semikolennykh, A. V. Gornov, M. V. Gornova, and N. V. Lukina. "Influence of Vegetation on the Lability Characteristics of Sandur Areas of the Bryansky Les Nature Reserve." Moscow University Soil Science Bulletin 73, no. 3 (July 2018): 100–106. http://dx.doi.org/10.3103/s0147687418030055.

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Maizels, Judith. "Lithofacies variations within sandur deposits: the role of runoff regime, flow dynamics and sediment supply characteristics." Sedimentary Geology 85, no. 1-4 (May 1993): 299–325. http://dx.doi.org/10.1016/0037-0738(93)90090-r.

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Vandenberghe, Jef, and Ming-ko Woo. "Modern and ancient periglacial river types." Progress in Physical Geography: Earth and Environment 26, no. 4 (December 2002): 479–506. http://dx.doi.org/10.1191/0309133302pp349ra.

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Climate has been proposed conventionally as the primary factor that determines periglacial river activity (aggradation) and pattern (braided). This concept does not explain the rich diversity in river patterns and morphological processes in both the present and past periglacial environments: besides braided rivers and sandur, meandering, anabranching, transitional and deltaic rivers also occur. A first attempt is made to combine past and present periglacial river types with regard to their morphology, processes and environments. The processes that control river energy and morphology are discussed especially for periglacial conditions. This approach permits an assessment of the responses of periglacial rivers to climatic conditions and the modulation of the responses due to changes in the basin properties. Examples drawn from palaeo- and present-day periglacial rivers and environments demonstrate that there is no unique type of periglacial river but rather an azonal fluvial system with a number of periglacial variants.

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Beylich, Achim A., Katja Laute, Susan Liermann, Louise Hansen, Valentin Burki, Geir Vatne, Ola Fredin, Dorothea Gintz, and Ivar Berthling. "Subrecent sediment dynamics and sediment budget of the braided sandur system at Sandane, Erdalen (Nordfjord, Western Norway)." Norsk Geografisk Tidsskrift - Norwegian Journal of Geography 63, no. 2 (June 2009): 123–31. http://dx.doi.org/10.1080/00291950902907934.

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., A. Jaswanth Gowda. "CONCENTRATION AND DISTRIBUTION OF PARTICULATE MATTER IN SUBBARAYANAHALLI IRON ORE MINE, SANDUR, KARNATAKA, INDIA - A CASE STUDY." International Journal of Research in Engineering and Technology 04, no. 05 (May 25, 2015): 219–23. http://dx.doi.org/10.15623/ijret.2015.0405042.

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47

Veyret, Yvette. "Essai sur la terminologie glaciaire." Géographie physique et Quaternaire 33, no. 2 (December 9, 2010): 205–22. http://dx.doi.org/10.7202/1000069ar.

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Un travail récent (VEYRET, 1978) portant sur les phénomènes glaciaires dans le massif central français a obligé à une mise au point terminologique. Les notions de cirque glaciaire, de drift, till, moraine, de drumlin, de kame et esker, de sandur et de valley-train, de glacier noir ont été envisagées. Dans chaque cas, on a tenté de retrouver le premier sens du mot évoqué, puis on a voulu dégager d’une bibliographie très volumineuse la définition couramment admise des différentes notions étudiées. Dans le détail, la genèse des formes analysées fait l’objet de beaucoup de divergences entre les auteurs et bien des points qu’il convenait de rappeler demeurent incomplètement éclairés. Cette étude n’avait pas pour but de discuter l’appelation des formes et des dépôts considérés et elle n’a pas cherché à suggérer de nouveaux termes français pour les substituer à ceux d’origine étrangère déjà existants et souvent bien introduits dans la littérature scientifique.

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48

Khotimah, Khusnul, Ahmad Jami’ul Amil, Abdul Rosid, and Mixghan Norman Antono. "Inovasi Pembelajaran Karakter Humanis Melalui Sanggar Sastra dengan Pendekatan CRS (Consideration Research Student) dalam Matakuliah Apresiasi dan Kritik Sastra." Stilistika: Jurnal Pendidikan Bahasa dan Sastra 12, no. 1 (January 28, 2019): 1. http://dx.doi.org/10.30651/st.v12i1.2437.

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Penelitian ini adalah penelitian kualitatif deskriptif dengan kajian pembelajaran sastra, peneletian ini mengkaji tentang pembelajaran sastra dan pendidikan karakter pada materi perkuliahan apresiasi dan kritik sastra. Pada penelitian ini instrumen yang digunakan adalah instrumen peneliti sendiri, instrumen proses pembelajaran, dan instrumen pendidikan karakter. Proses pembelajaran apresiasi dan kritik sastra diketahui dari hasil pengamatan dan penilaian penilaian kinerja mahasiswa selama mengikuti pembelajaran sastra. Proses pembelajaran setelah dilakukan tindakan ternyata sudah sesuai dengan landasan kualitas proses yang dibuat yaitu, ada lima jenis variabel yang menentukan keberhasilan belajar mahasiswa yaitu sebagai berikut: a) melibatkan mahasiswa secara aktif, b) Menarik minat dan perhatian mahasiswa, c) membangkitkan motivasi mahasiswa, d) Peragaan dalam pembelajaran Sastra melalui pementasan sandur. Nilai-nilai humanis yang diterapkan yaitu; menghargai pendapat orang lain (kebebasan menngeluarkan pendapat), Kerjasama, rela berkorban, peduli terhadap orang lain, dan tolong menolong, dan Solidaritas. pembelajaran apresiasi dan kritik sastra menekankan pada nilai-nilai humanis sehingga menciptakan keragaman yang harmonis dalam bingkai sastra.

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Mukhopadhyay, Dhruba, and Abdul Matin. "The structural anatomy of the Sandur schist belt—a greenstone belt in the Dharwar craton of South India." Journal of Structural Geology 15, no. 3-5 (March 1993): 309–22. http://dx.doi.org/10.1016/0191-8141(93)90128-w.

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50

Pisarska-Jamroży, Małgorzata. "Factors controlling sedimentation in the Toruń-Eberswalde ice-marginal valley during the Pomeranian phase of the Weichselian glaciation: an overview." Geologos 21, no. 1 (March 1, 2015): 1–29. http://dx.doi.org/10.1515/logos-2015-0001.

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Abstract During the Pleistocene the Scandinavian ice sheet drained huge quantities of sediment-laden meltwaters. These meltwaters supplied ice-marginal valleys that formed parallel to the front of the ice sheet. Not without significance was the supply of ice-marginal valleys from extraglacial rivers in the south. Moreover, periglacial conditions during and after sedimentation in ice-marginal valleys, the morphology of valley bedrocks, and erosion of older sediments played important roles in the depositional scenarios, and in the mineralogical composition of the sediments. The mechanisms that controlled the supply and deposition in ice-marginal valleys were analysed on the basis of a Pleistocene ice-marginal valley that was supplied by northern and southern source areas in the immediate vicinity. Investigations were conducted in one of the largest ice-marginal valleys of the Polish-German lowlands, i.e., the Toruń-Eberswalde ice-marginal valley, in sandurs (Drawa and Gwda) supplied sediments and waters from the north into this valley, and on extraglacial river terraces (pre-Noteć and pre-Warta rivers), formed simultaneously with the sandurs and ice-marginal valley (Pomeranian phase of Weichselian glaciation) supplied sediments and waters from the south into this valley. A much debated question is how similar, or different, depositional processes and sediments were that contributed to the formation of the Toruń-Eberswalde ice-marginal valley, and whether or not it is possible to differentiate mostly rapidly aggraded sandur sediments from ice-marginal valley sediments. Another question addresses the contribution of extraglacial feeding of the Toruń-Eberswalde ice-marginal valley. These matters were addressed by a wide range of analyses: sediment texture and structure, architectural elements of sediments, frequency of sedimentary successions, heavy-mineral analysis (both transparent and opaque heavy minerals), analysis of rounding and frosting of quartz grains, and palaeohydrological calculations. Additionally, a statistical analysis was used. The specific depositional conditions of distribution of sediments in ice-marginal valley allow to distinguish new environment of ice-marginal valley braided river. The spectrum of depositional conditions in the Toruń-Eberswalde ice-marginal valley and their specific palaeohydraulic parameters allow to distinguish three coexisting zones in the ice-marginal valley braided-river system: (1) deep gravel-bed braided channel zone with extensive scours, (2) deep sand-bed braided channel zone with transverse bars, and (3) marginal sand-bed and gravel-bed braided channel zone with diamicton and breccia deposition, which were characterised in detail. Some of the results have been published previously, which is why they are discussed in the present paper within the context of new data

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