Relevant bibliographies by topics / Region Quaternary

Academic literature on the topic 'Region Quaternary'

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Published: 10 December 2022
Last updated: 29 January 2023

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Journal articles on the topic "Region Quaternary"

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Mitusio, Taikou, and Hideo Kagami. "Quaternary Strata in Shikoku Region." Quaternary Research (Daiyonki-Kenkyu) 31, no. 5 (1992): 297–311. http://dx.doi.org/10.4116/jaqua.31.297.

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Zolnikov, I. D., A. V. Shpansky, and M. V. Mikharevich. "PROBLEMS OF THE QUATERNARY STRATIGRAPHY OF THE SIBERIAN REGION." Geology and mineral resources of Siberia, no. 10s (December 2021): 3–6. http://dx.doi.org/10.20403/2078-0575-2021-10c-3-6.

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This special issue of the journal is devoted to modern controversial subjects arising during the research of the Siberian Quaternary system. The initiative to discuss these problems and new factual material that requires rethinking outdated stratigraphic constructions belonged to the section of the Quaternary system of SIBRMSK and was supported by leading experts actively working in the region. It should be noted that this issue does not cover all the unresolved issues on the geology, stratigraphy and paleogeography of the Quaternary period of Siberia.
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Prado, José Luis, and María Teresa Alberdi. "Quaternary mammalian faunas of the Pampean Region." Quaternary International 212, no. 2 (February 2010): 176–86. http://dx.doi.org/10.1016/j.quaint.2009.03.010.

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Dam, R. A. C., S. van der Kaars, and A. P. Kershaw. "Quaternary environmental change in the Indonesian region." Palaeogeography, Palaeoclimatology, Palaeoecology 171, no. 3-4 (July 2001): 91–95. http://dx.doi.org/10.1016/s0031-0182(01)00241-3.

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Makeev, V. M., E. A. Pikulik, E. A. Karfidova, and A. O. Agibalov. "Quaternary tectonics and geodynamics of Moscow region." Moscow University Bulletin. Series 4. Geology, no. 2 (December 16, 2022): 19–26. http://dx.doi.org/10.33623/0579-9406-2022-2-19-26.

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In the Moscow region, Eopleistocene deformations (1,8 million years) were studied for the first time. The activity of modern geological processes is associated with them. The qualitative and quantitative characteristics of deformations were carried out on the basis of the structural-geodynamic method and morphometric analysis of a large array of GIS data. The stage-by-stage amplitudes and velocities of neotectonic uplifts have been estimated. And the gradient of the strain rate of the Moskvoretskaya zone was calculated.
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Deodoro, Sandra Cristina, William Zanete Bertolini, and Plinio da Costa Temba. "Quaternary formations mapping in the region of Volta Grande do Rio Uruguai (Brazil)." Geography Department University of Sao Paulo 41 (June 11, 2021): e174174. http://dx.doi.org/10.11606/eissn.2236-2878.rdg.2021.174174.

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Quaternary formations (detrital and weathered materials) are an important natural resource for different areas of scientific investigation, from understanding their relation to erosive processes and morphodynamic processes that create landforms or to understanding the history of the first human settlements (geoarcheology). Quaternary coverings can be formed in situ or be transported by external geologic agents. Regarding soils, Quaternary formations are related to landscape topography and are transformed according to the characteristics of this topography. Hence, classifying and mapping these soils is not always easy. The present article aims to map the Quaternary formations along a stretch of the Uruguay River basin known as Volta Grande (SC/RS-Brazil), by using topographic attributes derived from the SRTM GL1-Up Sampled digital elevation model, soil particle-size analysis, and a generated Multiresolution Index of Valley Bottom Flatness (MRVBF) index . The results of the analysis show that: (i) colluvium is the predominant Quaternary formation in the study area; (ii) there is a predominance of clay, corroborating previous studies of the region; (iii) the spatial distribution of the study area’s Quaternary formations reflect local slope dynamics based on morphology and topographic position; and, (iv) the existence of colluvium-alluvium on the Uruguay River’s banks indicates that slope attributes contributed to the pedogeomorphological dynamics of the study area and not only fluvial dynamics. Based on the results, the methodology applied in this study might be useful for pedogeomorphological studies, notably in the analysis and mapping of Quaternary formations, despite some of its limitations.
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Makeev, V. M., E. A. Pikulik, E. A. Karfidova, and A. O. Agibalov. "Quaternary Tectonics and Geodynamics of the Moscow Region." Moscow University Geology Bulletin 77, no. 3 (June 2022): 263–70. http://dx.doi.org/10.3103/s0145875222030103.

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Rossignol-Strick, Martine. "Late Quaternary climate in the Eastern Mediterranean Region." Paléorient 19, no. 1 (1993): 135–52. http://dx.doi.org/10.3406/paleo.1993.4588.

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Wang, Jinyan, and Jianqiang Chen. "Quaternary Sediments and Paleoenvironmental Evolution in Suqian Region." IOP Conference Series: Earth and Environmental Science 170 (July 2018): 022121. http://dx.doi.org/10.1088/1755-1315/170/2/022121.

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Lee, C. S., and Y. H. Chung. "Late Quaternary sedimentation in the Kadeok region, Korea." Geo-Marine Letters 20, no. 2 (September 27, 2000): 72–79. http://dx.doi.org/10.1007/s003670000037.

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Dissertations / Theses on the topic "Region Quaternary"

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Balzer, Solweig A. "Quaternary geology and dispersal patterns, Winagami region, Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp02/NQ59928.pdf.

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O'Brien, Charlotte Elizabeth. "Quaternary vegetation history of the Medoc Region, S.W. France." Thesis, Coventry University, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.366370.

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Hunt, Jonathan Brewster. "Quaternary tephrology and tephrochronology of the North Atlantic region." Thesis, University of Edinburgh, 1996. http://hdl.handle.net/1842/12096.

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Late Quaternary Climatic Oscillations are known to be intense, and in some cases too rapid to be resolved reliably using a radiocarbon chronology. Tephrochronology, the use of widespread and isochronous layers of volcanic ash is increasingly seen as a valuable tool in the inter-environmental correlation of proxy- palaeonclimatic indicators. A fundamental assumption that underpins tephrochronology in the North Atlantic is the acceptance that tephra horizons can be fingerprinted uniquely, by the major/minor element compositions of their vitric shards. This thesis concentrates on the analytical (Electron Probe Microanalysis) methodology required in the accurate and precise determination of this fingerprint, on factors which inhibit successful correlation using such fingerprints and on the application of geochemical signatures to the establishment of a meaningful regional tephrochronology. In addition, studies of tephra deposition and re-mobilisation have also been undertaken following the 1991 eruption of Hekla, with results indicating the need for caution in interpreting mass-loading and mapping of tephra isochrons. The principal tephrostratigraphy within this thesis relates to the Late Glacial and early Holocene, and is used in an attempt to achieve correlations between marine, terrestrial and ice-sheet environments. At least seven tephra isochrons are shown to be present in the North Atlantic region in the interval ca. 14,000 14C yrs BP to ca. 9,000 14C yrs BP, with one interpretation of evidence from the UK continental shelf suggestive of further horizons. Rigorous investigation of these tephras has revealed the potential inadequacies of major elements as unambiguous indices in the correlation and differentiation of Iceland-derived tephras. This is summarised by the term "geochemical equifinality", associated with higher eruption frequencies of known individual volcanic centres than previously recognised. It is apparent that, (i) geochemical data must be supplemented by more rigorous investigations of stratigraphical context; and (ii) new analytical techniques must be applied to the characterisation of potential trace elements signatures.
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Merritts, Dorothy Jane. "Geomorphic response to late Quaternary tectonism: Coastal northern California, Mendocino triple junction region." Diss., The University of Arizona, 1987. http://hdl.handle.net/10150/184316.

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Different patterns of uniform-uplift periods associated with passage of the Mendocino triple junction (MTJ) and a change in tectonic regime are based on altudinal spacing analyses of nine flights of marine terraces. Rates of uplift appear to increase from <1 m/ka to 4-5 m/ka, with periods of most rapid uplift that are progressively younger toward the triple junction. The MTJ was about 55 km to the south at about 1 ma ago, where uplift has been uniform at about 1.3 m/ka during the last 300 ka. Maximum uplift of about 4 m/ka is occurring 20-40 km south of the MTJ; prior to about 100-150 ka uplift was slow, being only 0.2-0.5 m/ka. Ten km to the north of the MTJ, accelerated uplift has occurred only during the last 60 ka. Relative strength of soil development in sandy marine deposits on five Pleistocene and Holocene (1.7 to 120 ka) marine terraces near the MTJ is one basis for relative age estimates and correlation of terrace soils. Organic carbon content in the upper 70 cm of the soil profile increases exponentially, and pH decreases exponentially; for both properties steady state is attained by 40 ka. Whole profile content of clay, total free iron oxyhydroxides (Fe(d)), and total free and para-crystalline aluminum oxyhydroxides increase nearly linearly until at least 120 ka. Comparison of these soils with four marine terrace soils (103-405 ka) 100-120 km to the south indicates that maximum percent values of clay and Fe(d) increase exponentially, with highest values reached at about 120 ka. Analysis of three-dimensional morphological properties of 25 coastal drainage basins that have evolved in areas of low (<1 m/ka), intermediate (1-3 m/ka), and high (>3 m/ka) rates of uplift near the MTJ identified channel slopes as the best indicator of tectonism in the landscape. Lower order tributaries reflect tectonically-controlled differences best. The largest streams examined, of third order, are able to adjust to most base-level change and maintain their profile form, whereas lower order streams farther upstream tend to accumulate the effects of net base-level fall, and have steepest profiles in the areas of highest uplift. Although first order streams are excellent indicators of highest uplift rate areas and regional differential tilting, they are less useful in distinguishing between low and intermediate uplift rate areas. Analysis of the longitudinal profile of the main trunk stream of 10 of the 25 drainage basins with the stream-gradient index (Hack, 1957) was useful to broadly categorize uplift rates, and to distinguish between low and intermediate uplift rate streams.
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Moseley, Gina Elaine. "Mid to late quaternary sea level change of the circum-Caribbean region." Thesis, University of Bristol, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.508171.

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Bourne, Anna Julie. "The late Quaternary tephrochronology of the Adriatic region : implications for the synchronisation of marine records." Thesis, University of London, 2012. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.549601.

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Tephrochronologies for three marine core sequences from the Adriatic Sea have been constructed. Two of the sequences, PRAD 1-2 and RF93-77, are located in the central Adriatic and the third, SA03-03, lies in the southern Adriatic. Isotopic and biostratigraphic records are available for all three sequences, features of which have been used as isochronous markers in the region. This project aimed to establish whether tephra layers provide (a) secure, independent isochronous tie-lines and (b) a robust methodology for testing correlations based on other methods. A total of 54 tephra layers have been identified within these sequences, of which only 8 are visible layers, the remainder being classified as cryptotephras. Geochemical characterisation of the ash layers has been undertaken using electron microprobe analysis and laser-ablation trace element methods. Geochemical correlation to the detailed tephra record from Lago Grande di Monticchio was performed using chemical element biplots and discriminant function analysis. Bayesian-based age models were generated for the three Adriatic records using available chronological information that are independent of assumptions of synchroneity between proxy marker events. These models allowed comparisons with tephra and palaeoenvironmental data from Lago Grande di Monticchio and other Mediterranean sites. The results support some assumptions of synchronous regional changes, but not others. The key outcomes are (a) the recognition of additional (non-visible) distal ash layers that enhance the potential for correlating marine and terrestrial records in the central Mediterranean; (b) volcanic ash records preserved in Lago Grande di Monticchio and in some localities proximal to volcanic sources appear to be incomplete; and (c) isotopic records in Adriatic sediment sequences reflect regional forcing factors more than local conditions.
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McMartin, Isabelle. "Quaternary geology and environmental geochemistry of the Flin Flon region, Manitoba and Saskatchewan." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0022/NQ52328.pdf.

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Smith, Andrew David. "Late Quaternary tectonics, sedimentation and sea-level changes in the North Aegean region." Thesis, University of Cambridge, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.321021.

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McMartin, Isabelle Carleton University Dissertation Earth Sciences. "Quaternary geology and environmental geochemistry of the Flin Flon Region, Manitoba and Saskatchewan." Ottawa, 2000.

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Woolfenden, Wallace Bird 1941. "Late Quaternary vegetation history of the southern Owens Valley region, Inyo County, California." Diss., The University of Arizona, 1996. http://hdl.handle.net/10150/282184.

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This study analyzes the pollen, spores, and algae in the upper 90 m section of a mostly continuous, well dated, 323 m core (OL-92) from Owens Lake, southeastern California. The entire core has produced a paleoclimatic record for the past ∼800 ka. The 90 m interval dates from ∼9 ka to ∼151 ka beginning with the penultimate glaciation and ending during the termination of the last glaciation. The record shows high amplitude fluctuations in the abundances of pine, juniper, saltbush, sagebrush, chenopods/amaranths, and Ambrosia-type pollen. High percentages of juniper pollen with low percentages of desertscrub pollen during the intervals ∼150 ka to ∼120 ka and 73 ka to ∼20 ka alternate with low juniper pollen and relatively high percentages of desertscrub and oak pollen during the intervals ∼118 ka to ∼103 ka and ∼18 ka ∼10 ka and into the Holocene. Sagebrush pollen varies with juniper pollen but has a tendency to lead it in time. Pine and fir pollen tends to vary inversely with juniper over the long term. These trends are interpreted as vegetation change in response to glacial-interglacial cycles: During cold-wet glacial climates there was a downslope expansion of juniper woodland and sagebrush scrub, contraction of Sierra Nevada mixed conifer forest, and displacement of warm desertscrub, suggesting average temperature and precipitation departures from modern values ranging from -2°C to -6°C and from +100 mm to +350 mm. Conversely under warmer and drier interglacials warm desert shrubs expanded their range in the lowlands, juniper and sagebrush retreated upslope, and the Sierran forests expanded. Estimated average temperature and precipitation departures from modern values ranged from -0.5°C to +3.7°C and +13 to -26 mm. Comparison of the pollen spectra spanning the penultimate and ultimate glacial maxima shows the former to have been longer and more intense, in accord with the Sierra Nevada glacial record. Similarly, the higher abundances of Ambrosia pollen during the last interglaciation, compared to the Holocene, indicate warmer temperatures in the former. The presence of high oak percentages also during the last interglaciation suggest an expansion of the summer monsoon. Finally, the match of the juniper curve with the marine oxygen isotope chronostratigraphy suggests a link between vegetation change in the southern Owens Valley and global climate.
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Books on the topic "Region Quaternary"

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Grant, Douglas R. Quaternary geology of the Appalachian region of Canada. Ottawa: Dept. of Energy , Mines and Resources, 1989.

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Canada, Geological Survey of. Quaternary Geology of the Ottawa Region, Ontario and Quebec. S.l: s.n, 1986.

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Fulton, Robert J. Quaternary of the Ottawa region and guides for day excursions. Ottawa: National Research Council of Canada, 1987.

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Rampton, V. N. Quaternary geology of the Tuktoyaktuk Coastlands, Northwest Territories. Canada: Energy, Mines and Resources Canada, 1988.

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Rampton, V. N. Quaternary geology of the Tuktoyaktuk Coastlands, Northwest Territories. Ottawa, Ont: Geological Survey of Canada, 1988.

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D, Long, and Fyfe J. A, eds. A revised Quaternary stratigraphy for the central North Sea. London: H.M.S.O., 1985.

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Carrara, Paul E. Late Quaternary glacial and vegetative history of the Glacier National Park region, Montana. Washington, D.C: U.S. G.P.O., 1989.

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Sue, O'Connor, and Veth Peter Marius, eds. East of Wallace's line: Studies of past and present maritime cultures of the Indo-Pacific region. Rotterdam: Balkema, 2000.

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Catto, Norman Rhoderick. Quaternary geology and landforms of the eastern Peace River region, British Columbia, NTS 94A/1,2,7,8. [British Columbia]: Province of British Columbia, Ministry of Energy, Mines and Petroleum Resources, Mineral Resources Division, Geological Survey Branch, 1991.

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Bajc, Andrew F. Quaternary geology and geomorphology of the Sudbury region: Field trip A5 guidebook, May 24-25, 1999. Sudbury, Ontario: Geological Association of Canada (GAC), Mineralogical Association of Canada (MAC), 1999.

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Book chapters on the topic "Region Quaternary"

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Mikhnevich, Galina. "Composition of Pre-Quaternary Surface and Quaternary Sediments Allocation on the Territory of the Kaliningrad Region." In The Handbook of Environmental Chemistry, 45–79. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/698_2017_87.

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Johnson, Eileen, Gustavo Politis, Gustavo Martinez, William T. Hartwell, Maria Gutierrez, and Herbert Haas. "Radiocarbon Chronology of Paso Otero 1 in the Pampean Region of Argentina." In Quaternary of South America and Antarctic Peninsula, 15–25. London: Routledge, 2022. http://dx.doi.org/10.1201/9780203741429-2.

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Bouza, Pablo J., Claudia Saín, Lina Videla, Patricia Dell’Arciprete, Estela Cortés, and Julio Rua. "Soil–Geomorphology Relationships in the Pichiñán Uraniferous District, Central Region of Chubut Province, Argentina." In Advances in Geomorphology and Quaternary Studies in Argentina, 77–99. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-54371-0_3.

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Sherman, Ian. "Holocene Sea-Level Changes and Crustal Movements in the North Sea Region: An Experiment with Regional Eustasy." In Late Quaternary Sea-Level Correlation and Applications, 1–25. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-0873-4_1.

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Quick, Lynne J. "Future directions of palaeoecological research in the hyper-diverse Cape Floristic Region: The role of palynological studies." In Quaternary Vegetation Dynamics – The African Pollen Database, 225–38. London: CRC Press, 2021. http://dx.doi.org/10.1201/9781003162766-14.

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Echevarria, Karina V., Susana B. Degiovanni, Mónica T. Blarasin, and M. Jimena Andreazzini. "Flash Flood Hazard Assessment in an Ungauged Piedmont Basin in the Sierras Pampeanas Western Region, Province of Córdoba, Argentina." In Advances in Geomorphology and Quaternary Studies in Argentina, 181–201. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-54371-0_7.

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Rodriguez, María Jimena, Eliana Conci, Analía Becker, María Grumelli, M. Micaela Ledesma, Aldo Rangone, Fernando Forgioni, and Pablo Bouza. "Environmental Risk in the Fluvio-Aeolian Plain of the Region Center of the General San Martín Department, Córdoba, Argentina." In Advances in Geomorphology and Quaternary Studies in Argentina, 244–84. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-66161-8_11.

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Irmak, Seyyid, Recep Gundogan, and Hikmet Gunal. "Salinity Problems of Some Quaternary Soils in the Central Anatolia Region of Turkey." In Proceedings of the Fourth International Conference on Precision Agriculture, 373–81. Madison, WI, USA: American Society of Agronomy, Crop Science Society of America, Soil Science Society of America, 2015. http://dx.doi.org/10.2134/1999.precisionagproc4.c33.

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Behling, Hermann, Martin Lichte, and Attila Wolinsk Miklos. "Evidence of a forest free landscape under dry and cold climatic conditions during the last glacial maximum in the Botucatú region (São Paulo State), Southeastern Brazil." In Quaternary of South America and Antarctic Peninsula, 99–110. London: Routledge, 2022. http://dx.doi.org/10.1201/9780203741429-6.

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Ojeda, Guillermo, David Javier Candia Halupczok, Jorge Chiesa, Guillermo Heider, Avto Gogichaishvili, Catriel Greco, Franco Icazatti, Alicia Irurzun, and Claudia Gogorza. "Geomorphology of the Piedmont Area of the Central-East Region of the “Serranias Occidentales”: Fluvial Systems and Geoarcheology. San Luis, Argentina." In Advances in Geomorphology and Quaternary Studies in Argentina, 192–218. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-66161-8_9.

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Conference papers on the topic "Region Quaternary"

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Dornajafi, Mahsa, Steve E. Watkins, Benjamin Cooper, and M. Ryan Bales. "Performance of a Quaternary Logic Design." In 2008 IEEE Region 5 Conference. IEEE, 2008. http://dx.doi.org/10.1109/tpsd.2008.4562722.

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Khan, Md Mahmud Muntakim, Ayan Kumar Biswas, Shuvro Chowdhury, Mehbuba Tanzid, Kazi Mohammad Mohsin, Masud Hasan, and Asif Islam Khan. "Quantum realization of some quaternary circuits." In TENCON 2008 - 2008 IEEE Region 10 Conference (TENCON). IEEE, 2008. http://dx.doi.org/10.1109/tencon.2008.4766486.

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Pujol, Jaume, Josep Rifa, and Faina I. Solov'eva. "On new quaternary Reed-Muller codes." In 2008 IEEE Region 8 International Conference on Computational Technologies in Electrical and Electronics Engineering (SIBIRCON). IEEE, 2008. http://dx.doi.org/10.1109/sibircon.2008.4602620.

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Das, A., I. Jahangir, M. Hasan, and S. Hossain. "On the design and analysis of quaternary serial and parallel adders." In 2010 IEEE Region 10 Conference (TENCON 2010). IEEE, 2010. http://dx.doi.org/10.1109/tencon.2010.5686045.

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Jahangir, Ifat, Dihan Md Nuruddin Hasan, and Md Shamim Reza. "Design of some quaternary combinational logic blocks using a new logic system." In TENCON 2009 - 2009 IEEE Region 10 Conference. IEEE, 2009. http://dx.doi.org/10.1109/tencon.2009.5396095.

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Khaleduzzaman, Syed, Sabyasachi Paul, and Shaikh Asif Mahmood. "Performance Analysis of Perovskite and Quaternary Compound for X-ray Image Detectors." In TENCON 2019 - 2019 IEEE Region 10 Conference (TENCON). IEEE, 2019. http://dx.doi.org/10.1109/tencon.2019.8929558.

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Abdollahie Fard, Iraj. "3D Seismic Interpretation of the South Caspian Plio-Quaternary Channelling System in Revealing Structural Evolution." In Atyrau 2011 - First Caspian Region Workshop. Netherlands: EAGE Publications BV, 2011. http://dx.doi.org/10.3997/2214-4609.20144363.

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Mahmood, Syed Amer, Faisal Shahzad, and Richard Gloaguen. "Remote sensing analysis of quaternary deformation using river networks in Hindukush region." In 2009 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2009. http://dx.doi.org/10.1109/igarss.2009.5418089.

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Mytrokhyn, O., L. Gavryliv, and V. Bakhmutov. "Neogene-Quaternary Magmatic Activities In The Region Of Ukrainian Antarctic Station “Akademik Vernadsky”." In 12th International Conference on Monitoring of Geological Processes and Ecological Condition of the Environment. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201803176.

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Rawling, J. Elmo, Andy Breckenridge, and David Ullman. "1:100,000 SCALE PRELIMINARY QUATERNARY MAPPING IN THE LAKE SUPERIOR REGION OF WISCONSIN." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-368462.

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Reports on the topic "Region Quaternary"

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Fulton, R. J. Quaternary geology of the Ottawa region, Ontario and Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122374.

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Gadd, N. R. Geological Setting and Quaternary Deposits of the Ottawa Region. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122375.

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Fulton, R. J., and S. H. Richard. Chronology of Late Quaternary Events in the Ottawa Region. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122379.

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McCuaig, S. J. Quaternary geology of the Nass River region, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208616.

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Brennand, T., M. Hinton, and D. Sharpe. Terrestrial Quaternary geologic and hydrogeologic framework - Port Hope region (Oshawa-Cobourg). Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/205055.

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Stasiuk, M. V., and J. K. Russell. Quaternary Volcanic Rocks of the Iskut River Region, northwestern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131382.

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Grant, D. R. Chapter 5: Quaternary Geology of the Atlantic Appalachian Region of Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131539.

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Minning, G. V., W. R. Cowan, D. R. Sharpe, and T. A. Warman. Quaternary geology and drift composition, Lake of the Woods region, northwestern Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194813.

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Kaszycki, C. A. Quaternary geology and glacial history of the Haliburton region, south central Ontario. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/208201.

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Webb, K. Soils As a Resource: Atlantic Region [Chapter 11: Quaternary Resources in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131672.

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