Gotowe bibliografie tematyczne / Hills

Gotowa bibliografia na temat „Hills”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 20 lutego 2023

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Artykuły w czasopismach na temat "Hills"

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DEV, INDER, SUDESH RADOTRA, ASHA RAM, J. P. SINGH, D. DEB, M. M. ROY, M. SRIVASTAVA, PARDEEP KUMAR, SUHEEL AHMAD i R. S. CHAURASIA. "Species richness, productivity and quality assessment of grassland resources in hill agroecosystem of western Himalaya". Indian Journal of Animal Sciences 88, nr 10 (22.10.2018): 1167–75. http://dx.doi.org/10.56093/ijans.v88i10.84145.

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Livestock contribution in agricultural economy is significantly higher in hilly regions of India. A detailed study was carried out to assess the productivity, species richness and diversity of grasses of the grasslands in different hill agro-ecosystems of Kangra district of Himachal Pradesh in western Himalaya. Saccharum spontaneum (low hills), Chrysopogon echinulatus (mid hills) and Festuca spp. (high hills) were observed as the most dominant species in hill agro-ecosystems. Productivity assessment was done at five locations, viz. open forest area; enclosed forest area; community land; farmers’ field; and wasteland in each hill zone. High species richness and diversity was observed in mid hill zone as compared to low and high hills. The mean production level was recorded highest in low hills closely followed by mid hills; much less in high hills. Amongst the land-use systems, highest biomass production was recorded at farmers’ field followed by community land and least in wasteland situation. The average herbage production obtained through six cuts at periodic intervals (March to December) was 3,202 DM kg/ha, while in single harvest it was 2,249 DM kg/ha (low-hill conditions); 2,893 and 1,924 DM kg/ha (mid-hill conditions) and 1,399 and 850 DM kg/ha (high-hill conditions), respectively. Averaged over the different locations, 6.01, 6.64 and 10.87% crude protein (CP) was observed (in multicut situation) in low, mid and high hills respectively. Average herbage production obtained through six cuts at periodical intervals (March-December) was consistently higher as compared to single harvest in all the three zones.
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K, Arumugam. "The Legends and History of the Javadi Hills People". International Research Journal of Tamil 4, S-10 (10.08.2022): 1–6. http://dx.doi.org/10.34256/irjt22s101.

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Javadi Hills is the eastern chain of hills comprising Vellore district, Thiruvannamalai district, and Tirupattur district. The people living in these hills call themselves Malayalis. They have nothing to do with the Malayalis living in the state of Kerala. They live in the hills of Yelagiri Hill, Kolli Hills, Sitheri Hills, and Pachaimalai Hills in Tamil Nadu. But marriages happen between the people of these hill areas. They are the majority of the 37 tribes in Tamil Nadu. One hundred and four villages (184) in fourteen panchayats on this hill are the domains of this study. These Malayalis tell folktales as songs and stories. It can be seen that the custom of telling this as stories by men and songs by women can be seen. And they do not tell these stories all the time. It is noteworthy that they sing only during festivals or among researchers who conduct research on this community. Similarly, this review article explains that the songs narrating stories related to them are in circulation only among a few senior tribal people.
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Srinivasulu, B., C. Srinivasulu, T. A. Shah, G. Devender i H. Kaur. "First confirmed record of Calodactylodes aureus (Reptilia) from Karnataka, India". TAPROBANICA 6, nr 1 (29.06.2014): 53–54. http://dx.doi.org/10.47605/tapro.v6i1.129.

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The Indian Golden Gecko Calodactylodes aureus (Beddome, 1870) was known originally from the Tirupati hills in the Seshachalam range and the Velikonda range. It is listed under Schedule I of the Indian Wildlife Protection Act (1972) as it was considered rare, being found at the time only in the Seshachalam range. Subsequently, researchers have revealed the presence of this species from the Papikonda Hills (Perantalapally) in Khammam District, Maredumilli in East Godavari District, Araku Valley and Ananthagiri Hills in Vishakhapatnam District and Kadapa Hills from Andhra Pradesh, Niyamgiri hill ranges of Rayagada, Kalahandi Districts in Odhisha and Vellore and Balmathi Hill, Tamil Nadu. Furthermore, this species was recently reported from Sathgar Hill, Kailasagiri Hill (Ambur) and Valli Malai in Vellore District, Sayed Basha Malai in Krishnagiri District, Nedumkunam Hill, Melthiruvadathanur (Morambu), Karadi Parai and Sathanur Dam in Tiruvanamalai District and the Gingee Hills in Villupuram District of Tamil Nadu. Reddy et al. (2013) reported the occurrence of this species from Nigidi reserve forest area in the Anantapur District of Andhra Pradesh and this is the westernmost locality record of this species to date.
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Devkota, P., i S. Mishra. "Comparative Study of Vegetable Biodiversity in Terai and Hilly Belts of Chitwan, Nepal". Nepal Journal of Science and Technology 19, nr 1 (28.06.2020): 1–8. http://dx.doi.org/10.3126/njst.v19i1.29731.

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The study was conducted to assess biodiversity and conservation aspects of vegetable crops in two different geographical areas of the Chitwan district. The household survey was carried out in Kailash (hill) and Nayabasti (terai) of Chitwan. Descriptive analysis, mean comparison, correlations, and biodiversity indices were used for data analysis. On the basis of biodiversity index, evenness, the adequate number of species, and Sorenson’s coefficient, open-pollinated (OP) (nonhybrid) vegetables were more diverse in hills than in terai, while hybrid vegetables are more diverse in terai than in hills. Hybrid vegetables were mostly grown in terai, where the use of chemical fertilizers and pesticides was also higher. OP vegetables dominated hilly areas. Gurung ethnic community had a significant role in the conservation of indigenous vegetable biodiversity. The primary source of seed was home storage in the case of OP vegetables in hills. However, in terai, agro-concerns were used as a significant source of seeds, followed by co-operatives. Co-operatives’ involvement was high in terai as compared to hills, but the role was not significant in vegetable farming. In contrast, assistance in vegetable farming from agriculture service provider organizations was higher in hills as compared to terai. The major problem in vegetable farming was lack of irrigation in both areas, followed by market inaccessibility in hills, whereas climate change was rising as a problem in terai. Markets of produced goods were farm gate, local markets, and distant markets. A middleman mostly did the price determination of the products. Off-season vegetable farming was not practiced in the study areas. However, off-farm vegetable production was typical in hilly areas. Indigenous and OP vegetable biodiversity has been facing various challenges despite their roles in nutrition, indigenous knowledge promotion, and food security. Hence, it is suggested to strengthen government policy toward irrigation facility development, gene bank establishment, marketing facilities, and technology transfer and develop on-farm community based intense organizations for sustainable vegetable diversity conservation.
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Naher, Habibon, Noor Jahan Sarker i Shawkat Imam Khan. "A comparison of the breeding biology of White-throated Kingfisher Halcyon smyrnensis Linnaeus, 1758 in plains and hilly areas of Bangladesh". Journal of Threatened Taxa 14, nr 10 (26.10.2022): 21936–45. http://dx.doi.org/10.11609/jott.7565.14.10.21936-21945.

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The breeding biology of White-throated Kingfisher Halcyon smyrnensis was studied in plains and hilly areas from September 2008 to August 2011. Four villages under Savar upazilla were selected for plains, and Chittagong University Campus, Chattagram for the hilly area. The breeding season started in February in hills and April on plain. Mean (SD) time required to build a new nest was 11.3 (3.9) days in plains and 15.3 (0.57) days in hills. Clutch size was 3–4 in hills and 3–7 in plains. Mean egg parameters (length, width, and weight) and mean egg volume and surface area were similar in both areas. The mean incubation period on plains was 16.4 (1.2) days, in hills 14.1 (0.7) days. On plains fledging success was 52%, compared to 57% in hills. Theft by local inhabitants was a major reason for fledgling loss in plains, hence increased public awareness may reduce nestling mortality and increase breeding success.
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P, Suresh. "Oral Customs of Javvaadhumalai Malayalis". International Research Journal of Tamil 4, S-17 (17.12.2022): 167–75. http://dx.doi.org/10.34256/irjt224s1728.

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Tamil Nadu consists of the Eastern and Western Ghats. There are thirty-six tribal people living in these hills including "Adiyaan, Aranaadan, Eravaalan, Irular, Oorali, and Kaniyan." The Eastern Ghats have Javvaadhumalai, Yelagirimalai, Kalvarayanmalai, Servarayanmalai, Chitherimalai, Pachaimalai, Paalamalai, Vattalmalai, Neyyaamalai, Jarugumalai, Parukkurmalai, Kaalimalai, Kadakadalai, and Kollimalai hills. The divisions of the population living in the Western Ghats cannot be seen in these hills. The hills are mainly inhabited by Malayali tribes. The life of these javvaadhu hill people is a simple life. They are also preserving the arts according to the environment in which they live. The oral literature in their case helps to know the life and culture of the hill people.
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Kalaimani, A., i A. Nath. "The Indian Golden Gecko, Calodactylodes aureus (Beddome, 1870) in Tamil Nadu, India". TAPROBANICA 5, nr 1 (15.06.2013): 81–84. http://dx.doi.org/10.47605/tapro.v5i1.98.

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The gekkonid lizard genus Calodactylodes Strand, 1926 is endemic to peninsular India and Sri Lanka. Calodactylodes aureus (Beddome, 1870), the first described species in the genus, was originally recorded from the Tirupati Hills, Andhra Pradesh state in India. In Andhra Pradesh, in addition to the type locality, it is recorded from the Araku Valley and the Ananthagiri Hills both in the Visakhapatnam District, from Perantalapally in the Khammam District, from Maredumilli in the East Godavari District, the Seshachalam Hills in Chittoor and Kadapa Districts and the Tirumala Hills in Chittoor District. In Orissa state the species has been reported from Rayagada and Kalahandi Districts in the Niyamgiri Hills. Finally, in the state of Tamil Nadu the species has been recorded from the Balamathi, Valli Malai and Sathgar Hills in Vellore District, Nedumkunam Hill in Tiruvannamalai District and Shyed Basha Malai in Krishnagiri District.
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Daniel Anderson. "The Hills, Beautiful Hills". Missouri Review 32, nr 4 (2009): 60–62. http://dx.doi.org/10.1353/mis.0.0200.

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Fadjarajani, S., i R. As’ari. "Disaster mitigation-based environmental management model: a study on ten thousand hills, Tasikmalaya City, West Java". IOP Conference Series: Earth and Environmental Science 986, nr 1 (1.02.2022): 012020. http://dx.doi.org/10.1088/1755-1315/986/1/012020.

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Abstract Tasikmalaya seen from the physiographical aspect has its own uniqueness because it has many hills known as the ten thousand hills. The Ten thousand has functions, namely: geological, ecological, hydrological, aesthetic, economic, micro-climatological, natural defense/fortress (buffer zone), as well as education and tourism functions. The method used in this research is descriptive with field observation data collection techniques based on Satellite Imagery analysis.. The method used in this research is descriptive with field observation data collection techniques based on Satellite Imagery analysis. Data analysis is based on satellite imagery data processing with ArcGIS which was developed. The facts on the ground show that the extinction rate of the hill reaches 70%. One of the driving factors for the extinction of the hill was the mining of mineral. The distribution pattern and factual conditions in the field showed that 41.67% of the hills experienced extinction and 58.33% of the hills were heavily damaged by sand mining. This disaster mitigation-based environmental management model includes: 1) Zoning of hill areas based on conservation functions, 2) community participation based on economic improvement. Ten thousand hill zoning and community participation based on economic improvement can be used as role models for environmental management based on disaster mitigation in Tasikmalaya which is located in the ten thousand hill area.
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Alfin, A. S., H. E. Wibowo i A. Harijoko. "Morphometric Characteristic and Distribution of Hummocky Hills in Debris Avalanche Deposit of Galunggung Volcano, West Java, Indonesia". IOP Conference Series: Earth and Environmental Science 1071, nr 1 (1.08.2022): 012012. http://dx.doi.org/10.1088/1755-1315/1071/1/012012.

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Abstract Sector collapse of a volcanic body produces topography of horseshoe-shaped caldera incisions and a widespread hummocky hill resembling debris avalanche deposit. The study of morphometry, distribution, and the alignment of the hummocky hills is necessary to understand the source and deposition process of the debris-avalanche deposit. Galunggung volcano is, one of the volcanoes in Java Island, attributed with 7 km wide of caldera opens towards the east direction (N 135° E) where hummocky hills cover an area of ~32 km2. Morphometry of the hummocky hills is 500-700,000 m2 in size, elongation ratio of 1.3-3.9. Hummocky hills are distributed 0.5 to 20 km distance from the summit of the Galunggung volcano. The elongation orientation of the hummocky hills is deviated from the main flow direction forming various angles. We divide the deviation angle into parallel (0-45°) and perpendicular orientation (45-90°). The maximum size of the hummocky hills generally decreases towards increasing distance from the summit. These hills also show changes in alignment from perpendicular to parallel, suggesting a typical free flow pattern of debris-avalanche deposits.
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Rozprawy doktorskie na temat "Hills"

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Dunning, Jennifer C. "Far Hills". Ohio University / OhioLINK, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1149620129.

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Slasha, Unathi. "Jah Hills". Thesis, Rhodes University, 2017. http://hdl.handle.net/10962/7157.

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Jah Hills is alone in Kwaf Indoda bush, waiting for elders to come, burn ibhuma and deliver him home. Two weeks before he departs from his initiation period, he is seduced by igqwirha. When he fails to satisfy her appetite, he gets ‘abducted and turned into isithunzela. One night, he narrowly escapes and finds his way back. But the experience at home is gruesome; they drive him away and want his death. My novel is fast paced, accumulating speed as it proceeds. It is formally experimental, drawing on forms that have gone before and trying to usher in a new manner of writing and looking at the world. It is told through the eyes of isithunzela that Jah Hills has become. It makes use of Nguni folklore, reimagined and subverted so it fits the character’s unearthly vision. Certain characters and moments from Nguni folktales are borrowed and appear throughout the text. Stylistically I draw extensively from the work of Sony Lab’ou Tansi, Taban Lo Liyong, Dambudzo Marechera, D.O. Fagunwa and Amos Tutuola.
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Cates, Joel. "Beyond The Hills". Digital Archive @ GSU, 2009. http://digitalarchive.gsu.edu/english_hontheses/5.

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A couple travels through Spain in order to obtain an abortion for an unwanted pregnancy. The couple, an unnamed American man and a woman known only by the nickname Jig, has a much more complicated relationship than first seems and must navigate through complex emotions and gender roles. This story, and elaboration on Hemingway’s well known “Hills Like White Elephants”, attempts to give the characters introduced by Hemingway more depth and back story than the original short story.
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Newley, Trevor Michael Jeremy. "Turbulent air flow over hills". Thesis, University of Cambridge, 1986. https://www.repository.cam.ac.uk/handle/1810/250880.

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Lea, Adam Stuart Robert. "Boundary layer flow over hills". Thesis, University of Leeds, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.400175.

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Carlson, Chelsea. "Real Tweets of Beverly Hills". Scholarship @ Claremont, 2014. http://scholarship.claremont.edu/scripps_theses/344.

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Presbitero, Alan Ludovice, i n/a. "Soil Erosion Studies on Steep Slopes of Humid-Tropic Philippines". Griffith University. Australian School of Environmental Studies, 2003. http://www4.gu.edu.au:8080/adt-root/public/adt-QGU20040906.151808.

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An in-situ water-induced soil erosion study of two years duration was conducted at a low slope of about 10%, and also on steep slopes of about 50%, 60% and 70% at the experimental site located at a soil and water research area contiguous to the Department of Agricultural Engineering and Applied Mathematics of the Visayas State College of Agriculture (ViSCA). ViSCA is located in the town of Baybay at the island of Leyte in humid tropical Philippines (latitude of 10 degrees 44' north and longitude of 124 degrees 48' east). The study has the following aims, namely: 1) to investigate the effect of local farming practices on soil erosion, particularly at steep slopes; 2) to study the hydrology and soil erosion processes in steep slope conditions in humid tropical climate; and 3) to apply and determine the limitations of a physical process-oriented sediment transport model for water-induced soil erosion model (Griffith University Erosion System Template, GUEST) to a very permeable soil under very high rainfall conditions. In the context of the steep slope experiments at ViSCA: a) across the slope planting of corn is equally effective in controlling soil loss as hedged farming alone or in combination with peanut intercrop; b) across the slope planting of corn in hedged runoff plots is as effective in controlling soil loss as when combined with peanut intercrop; c) farmer’s practice of planting a rowcrop like corn along the slope (providing ready-made downslope pathways for runoff water thus, encouraging flow-driven soil erosion) produces significant soil loss, often larger than from a bare runoff plot; d) hedgerows significantly reduced sediment concentration provided they remain intact; e) "failure" in hedgerows, often results in massive soil loss, being even greater than that in a comparable bare runoff plot. (Failure is manifested by runoff breaching the litter barrier at the base of the hedgerow in a localized position, leading to concentrated flow and extension of rills upslope from base of hedgerow) of hedged runoff plot (even though contour planted) and f) application of stubble in combination with across slope planting in hedged runoff plots (with or without a closely growing intercrop) provided both maximum surface cover (aerial and contact) and protection against soil loss in steep slopes. These conclusions are likely to apply to crops similar to corn, with an intercrop similar to peanut in morphology and root system. These conclusions might also be expected to apply to low slopes, though the effect of such protection might not be as pronounced as in steep slope runoff plots. Soil erosion mechanisms in steep slopes are dominated mainly by the runoff-driven processes of entrainment and re-entrainment. Average sediment concentration c and total soil loss M are shown to be functions of positive coefficient runoff related regressors and a parameter that measures rills formed and permanently imprinted on soil surface, and of negative coefficient regressors related to surface contact cover, at least for the steep slopes considered in this study. The relatively high streampower associated with overland flow on steep slopes suggests that overland flow dominates over rainfall impact as a source of soil sediment concentration. This was confirmed by the low value of the measured ratio of soil sediment concentration shed by net-rainfall detachment trays to that lost from the bare runoff plots. On the effect of surface contact cover on average sediment concentration c, the following findings were made, namely: a) surface contact cover of only about 20% to 30% is sufficient to reduce c to low levels, assuming the cover is well distributed; b) an "exponential-decay" form of relationship existed between surface contact cover and the average sediment concentration from the non-bare soil without normalizing with respect to sediment concentration from a reference bare soil runoff plot; and c) such nonlinear relationship is indicative of the dominating runoff processes of entrainment and re-entrainment compared to the linear form of relationships if rainfall –driven processes of detachment and re-detachment dominate. In runoff dominated soil erosion processes, surface contact cover (including both living and dead vegetative cover close enough to the soil surface to impede overland flow) is more significant in curtailing soil erosion than aerial surface cover. ...continued.
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Presbitero, Alan Ludovice. "Soil Erosion Studies on Steep Slopes of Humid-Tropic Philippines". Thesis, Griffith University, 2003. http://hdl.handle.net/10072/366622.

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An in-situ water-induced soil erosion study of two years duration was conducted at a low slope of about 10%, and also on steep slopes of about 50%, 60% and 70% at the experimental site located at a soil and water research area contiguous to the Department of Agricultural Engineering and Applied Mathematics of the Visayas State College of Agriculture (ViSCA). ViSCA is located in the town of Baybay at the island of Leyte in humid tropical Philippines (latitude of 10 degrees 44' north and longitude of 124 degrees 48' east). The study has the following aims, namely: 1) to investigate the effect of local farming practices on soil erosion, particularly at steep slopes; 2) to study the hydrology and soil erosion processes in steep slope conditions in humid tropical climate; and 3) to apply and determine the limitations of a physical process-oriented sediment transport model for water-induced soil erosion model (Griffith University Erosion System Template, GUEST) to a very permeable soil under very high rainfall conditions. In the context of the steep slope experiments at ViSCA: a) across the slope planting of corn is equally effective in controlling soil loss as hedged farming alone or in combination with peanut intercrop; b) across the slope planting of corn in hedged runoff plots is as effective in controlling soil loss as when combined with peanut intercrop; c) farmer’s practice of planting a rowcrop like corn along the slope (providing ready-made downslope pathways for runoff water thus, encouraging flow-driven soil erosion) produces significant soil loss, often larger than from a bare runoff plot; d) hedgerows significantly reduced sediment concentration provided they remain intact; e) "failure" in hedgerows, often results in massive soil loss, being even greater than that in a comparable bare runoff plot. (Failure is manifested by runoff breaching the litter barrier at the base of the hedgerow in a localized position, leading to concentrated flow and extension of rills upslope from base of hedgerow) of hedged runoff plot (even though contour planted) and f) application of stubble in combination with across slope planting in hedged runoff plots (with or without a closely growing intercrop) provided both maximum surface cover (aerial and contact) and protection against soil loss in steep slopes. These conclusions are likely to apply to crops similar to corn, with an intercrop similar to peanut in morphology and root system. These conclusions might also be expected to apply to low slopes, though the effect of such protection might not be as pronounced as in steep slope runoff plots. Soil erosion mechanisms in steep slopes are dominated mainly by the runoff-driven processes of entrainment and re-entrainment. Average sediment concentration c and total soil loss M are shown to be functions of positive coefficient runoff related regressors and a parameter that measures rills formed and permanently imprinted on soil surface, and of negative coefficient regressors related to surface contact cover, at least for the steep slopes considered in this study. The relatively high streampower associated with overland flow on steep slopes suggests that overland flow dominates over rainfall impact as a source of soil sediment concentration. This was confirmed by the low value of the measured ratio of soil sediment concentration shed by net-rainfall detachment trays to that lost from the bare runoff plots. On the effect of surface contact cover on average sediment concentration c, the following findings were made, namely: a) surface contact cover of only about 20% to 30% is sufficient to reduce c to low levels, assuming the cover is well distributed; b) an "exponential-decay" form of relationship existed between surface contact cover and the average sediment concentration from the non-bare soil without normalizing with respect to sediment concentration from a reference bare soil runoff plot; and c) such nonlinear relationship is indicative of the dominating runoff processes of entrainment and re-entrainment compared to the linear form of relationships if rainfall –driven processes of detachment and re-detachment dominate. In runoff dominated soil erosion processes, surface contact cover (including both living and dead vegetative cover close enough to the soil surface to impede overland flow) is more significant in curtailing soil erosion than aerial surface cover. ... [continued].
Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
Australian School of Environmental Studies
Faculty of Environmental Sciences
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Mitchell, Aaron C. "Camp Wood : experience the Flint Hills". Manhattan, Kan. : Kansas State University, 2010. http://hdl.handle.net/2097/4155.

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Stringer, Marc Alexander. "Separation of air flow over hills". Thesis, University of Reading, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.269964.

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Książki na temat "Hills"

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Eagle, Tom Charging. Black Hills, sacred hills. Wyd. 2. Chamberlain, S.D: Tipi Press, 1992.

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Hills. Mankato, Minn: Capstone Press, 2005.

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Berne, Emma Carlson. Hills. New York: PowerKids, 2008.

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Hills like white hills: Stories. Dallas: Southern Methodist University Press, 2009.

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Seven hills. Toronto, Ont: Chartres Books, 1988.

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Marie, Robertson Eleanor. Black Hills. New York: G.P. Putnam's Sons, 2009.

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Kraft, Gabrielle. Hollywood hills. New York: Pocket Books, 1993.

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Copyright Paperback Collection (Library of Congress), red. Bloody hills. New York: Signet, 2004.

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Simmons, Dan. Black Hills. New York: Little, Brown and Company, 2010.

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Booth, Pat. Beverley Hills. London: Guild, 1989.

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Części książek na temat "Hills"

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Aber, James S., David G. Croot i Mark M. Fenton. "Cupola-Hills". W Glaciotectonic Landforms and Structures, 71–90. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-015-6841-8_5.

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Gravil, Richard. "‘Indignant Hills’". W Wordsworth’s Bardic Vocation, 1787–1842, 51–72. London: Palgrave Macmillan UK, 2003. http://dx.doi.org/10.1057/9780230510333_4.

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Archer, W. G. "Twin Hills". W Love Songs of Vidyāpati, 55. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003104216-17.

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Michaux, Bernard. "Malvern Hills". W Tewkesbury Walks, 77–89. Cham: Springer International Publishing, 2013. http://dx.doi.org/10.1007/978-3-319-01544-6_7.

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Wilde, Simon A. "Jack Hills Zircon". W Encyclopedia of Scientific Dating Methods, 1–2. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-6326-5_95-2.

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Wilde, Simon A. "Jack Hills Zircon". W Encyclopedia of Scientific Dating Methods, 359. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_95.

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Wilcox, Alison, i Adam Bushnell. "Hills and mountains". W Descriptosaurus Story Writing, 9–13. Subjects: LCSH: Creative writing (Elementary education) | Description (Rhetoric)–Study and teaching (Elementary) | Vocabulary–Study and teaching (Elementary): Routledge, 2020. http://dx.doi.org/10.4324/9781003095675-5.

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Archer, W. G. "Hills of Gold". W Love Songs of Vidyāpati, 84. London: Routledge, 2021. http://dx.doi.org/10.4324/9781003104216-46.

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Kaimal, J. C., i J. J. Finnigan. "Flow Over Hills". W Atmospheric Boundary Layer Flows. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195062397.003.0008.

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Streszczenie:
We now move on to the next obstacle to understanding how the boundary layer behaves in general through the study of flow over ridges and hills. In Chapter 4 we examined simple changes in surface conditions and showed how their effects extend upwards with increasing downwind distance. The distinguishing features of the flow over those changes were a small perturbation in the pressure field and an internal boundary layer, the depth of which was controlled by turbulent diffusion from the new surface. Here, we confront not a change in surface properties but a change in surface elevation that forces large-scale changes in the pressure field. The response to this forcing is more complicated than any we have tackled so far, but the work of many scientists over the past 25 years gives us a measure of understanding of the processes involved. In addition to extending to hillsides the kind of analyses of wind and turbulence we have already presented, there are new questions that only arise in the context of hill flows. One, with ramifications for large-scale prediction of the weather and climate, is how much drag hills exert on the atmosphere flowing over them. For large hills and mountains this problem is dominated by the behavior of the internal gravity waves initiated by hills; over lower topography, however, it involves a subtle balance between changes in the surface stress distribution and the pressure field. In questions of wind turbine siting, understanding the position and magnitude of accelerations in the mean wind becomes crucial, whereas changes to both the mean wind and turbulence are important when predicting the fate of atmospheric pollutants in hilly terrain or estimating wind loads on buildings. The pattern of airflow around a hill is determined not only by the hill shape but also by its size. A characteristic feature of the atmosphere as a whole is its static stability, extending all the way to the ground at night-time and down to zi during the day. As a result, the vertical movement of air parcels that must occur as the wind flows over a hill is accompanied by a gravitational restoring force.
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Dhar Dwivedi, Rama, i Abhay Kumar Soni. "Ecofriendly Hill Mining by Tunneling Method". W Mining Techniques - Past, Present and Future. IntechOpen, 2021. http://dx.doi.org/10.5772/intechopen.95918.

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Mostly, hills are mined by ‘Strip mining’ i.e. removing the hills from top. This conventional approach destroys the landscape and defaces the beauty of the hill. Besides, a large amount of dust generated at source disturbs the villagers and nearby human settlements during the excavation operation or related activities. To eliminate this, and remove the ‘out yard dumping of material’, except at initial stage i.e. during developmental phase, if tunneling methods of civil construction work is applied, ‘the conventional hill mining’ can be turned into an eco-friendly hill mining with very little planning efforts. This chapter highlights the abovementioned aspects of ‘hill mining’ covering overviews about the ‘hill mining by tunneling method’. In this technique, the extraction of mineral deposits is done by driving tunnels at the bottom (or other accessible higher level of the hills) and combining it with cross-cuts and adits, to protect the green cover and the serene hill environment. A case study of limestone mining in hilly Meghalaya region of India forms a part of the description where its feasibility exists.
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Streszczenia konferencji na temat "Hills"

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Sun, Weizhao, Zhongfan Wang, Yaliang Xia, Gang Chen i Suhong Zhang. "Application of Fracture Prediction Research Based on OVT Gather in Granite Buried Hills". W International Petroleum Technology Conference. IPTC, 2021. http://dx.doi.org/10.2523/iptc-21500-ms.

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Abstract The space of fracture reservoir in granite buried hills varies sharply with strong heterogeneity and very difficult to predict. Conventional fracture prediction methods based on narrow-azimuth post-stack seismic data have low prediction accuracy. OVT pre-stack gather retains the information of offset and azimuth, reflects the anisotropic characteristics of fractures and can be effectively used to predict the strength and strike of fracture in granite buried hills. In this paper, based on the analysis of anisotropy of OVT gather data, according to the geological characteristics of granite fractures, optimizes the sensitive offset and azimuth OVT gather data, uses the P-wave azimuth anisotropy technique to predict the strength and strike of fractures. The prediction coincides well with the drilling results, which can provide an important guidance for the exploration and development of granite buried hill in the research area.
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Boon Kong, Tan. "Limestone Hills, Rockfalls and the Developers". W First EAGE South-East Asia Regional Geology Workshop - Workshop on Palaeozoic Limestones of South-East Asia and South China. Netherlands: EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20144034.

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Jones, Hugh. "The Metamorphism of Dumps into Hills". W First International Seminar on the Management of Rock Dumps, Stockpiles and Heap Leach Pads. Australian Centre for Geomechanics, Perth, 2008. http://dx.doi.org/10.36487/acg_repo/802_23.

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McJannet, George S. "General Overview of the Elk Hills Field". W SPE Western Regional Meeting. Society of Petroleum Engineers, 1996. http://dx.doi.org/10.2118/35670-ms.

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Graue, D. J., W. N. Larsen, M. Carazas, M. Gorriti i A. Guzman. "Development Of Boomerang Hills Area Of Bolivia". W SPE Latin America Petroleum Engineering Conference. Society of Petroleum Engineers, 1992. http://dx.doi.org/10.2118/23735-ms.

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Jones, P. W., i R. O. Baker. "Profile Control in Virginia Hills EOR Injectors". W SPE/DOE Enhanced Oil Recovery Symposium. Society of Petroleum Engineers, 1992. http://dx.doi.org/10.2118/24193-ms.

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Herd, Larry. "Seismic acquisition in the Loess Hills of China". W SEG Technical Program Expanded Abstracts 1990. Society of Exploration Geophysicists, 1990. http://dx.doi.org/10.1190/1.1890398.

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Huang, Gang, Catherine Le Ribault, Serge Simoëns, Ivana Vinkovic i J. M. Vignon. "LARGE EDDY SIMULATION OF SALTATION OVER GAUSSIAN HILLS". W VII European Congress on Computational Methods in Applied Sciences and Engineering. Athens: Institute of Structural Analysis and Antiseismic Research School of Civil Engineering National Technical University of Athens (NTUA) Greece, 2016. http://dx.doi.org/10.7712/100016.2319.9914.

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Scipioni, A., A. Mazzi, F. Zuliani, A. Morelli i M. Mason. "Environmental Management Systems in Euganean Hills Regional Park". W SUSTAINABLE TOURISM 2006. Southampton, UK: WIT Press, 2006. http://dx.doi.org/10.2495/st060151.

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Han, Haochen, Yongliang Wen, Tingyu Wang i Xiaorong Lv. "Exterior design of Southwest hills multifunctional mini-chassis". W 5th International Conference on Civil Engineering and Transportation. Paris, France: Atlantis Press, 2015. http://dx.doi.org/10.2991/iccet-15.2015.373.

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Raporty organizacyjne na temat "Hills"

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Sandeman, H. A. I. Geology, Ellice Hills, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215615.

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Sandeman, H. A. I., T. Skulski i M. Sanborn-Barrie. Geology, Ellice Hills, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215703.

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Carr, Adrianne E., Kelsey K. Wuthrich, Angela M. Ziech, Esther E. Bowen i John Quinn. Stormwater Management Plan for the Arden Hills Army Training Site, Arden Hills, Minnesota. Office of Scientific and Technical Information (OSTI), marzec 2013. http://dx.doi.org/10.2172/1170215.

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Linn, Johnathan. Geologic Map of Kramer Hills. Geological Society of America, 1992. http://dx.doi.org/10.1130/1992-linn-kramerhills.

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Dixon, J. Isopach map: Smoking Hills Sequence. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207679.

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Dyke, A. S., i J. M. Savelle. Surficial geology, Innirit Hills, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/213216.

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Fletcher, John, i Mark Martin. Geologic Map of the Hinkley Hills. Geological Society of America, 1998. http://dx.doi.org/10.1130/1998-fletcher-hinkleyhills.

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Gower, C. F. Geology, Double Mer White Hills, Labrador. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120621.

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Wetherup, S. Bedrock geology, Nulki Hills, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/209927.

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Little, E. C. Surficial geology, Ellice Hills (north), Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/222142.

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