A Sense of People and Place

Author(s):  
Andrew Moutu

This chapter provides a general sense of the geography and economic livelihood, as well as an example of the sorts of (clan) relationships that prevail, in Iatmul villages. Topics discussed include canoes and the riverine economy; the physical geography of the Sepik River basin; and the Kanganamun village. The chapter concludes with some remarks about the nature of research methods and the kinds of problems the author encountered in the gathering of ethnographic information.

Phytotaxa ◽  
2014 ◽  
Vol 172 (2) ◽  
pp. 94
Author(s):  
Wayne Takeuchi

Helicia woxvoldiana (Proteaceae) is described from the Sepik River basin in Papua New Guinea, from classical localities on the Kaiserin-Augusta-Fluss itinerary of 1912–13. The new species is a canopy myrmecophyte with the largest flowers in Papuasian Helicia.


2020 ◽  
Vol 5 (1) ◽  
pp. 39-58
Author(s):  
Nugroho Nur Susanto

 Perang Banjar atau Perang Banjarmasin dapat pula disebut sebagai Perang Barito. Kata Banjar sendiri mengacu pada masyarakat Islam yang diikat oleh Kesultanan Banjar, sedangkan Barito mengacu pada nama sungai yang sangat penting, yang mengalir di sebagian wilayah Kalimantan Selatan, tetapi lebih banyak mengalir di wilayah administrasi Kalimantan Tengah. Tulisan ini bertujuan menjawab permasalahan mengapa istilah perang Banjar dapat pula disebut sebagai Perang Barito berdasarkan bukti-bukti arkeologis. Adapun perang di sini mengacu pada serangkaian perlawanan rakyat yang melibatkan masyarakat yang memiliki asal-usul dan latar belakang beragam. Perang Banjar didukung oleh keturunan Kesultanan Banjar, dibantu oleh komunitas rakyat biasa yang berasal dari berbagai daerah di batang banyu di sepanjang aliran Sungai Barito. Dukungan perjuangan berasal dari masyarakat Banua Lima yang diidentikkan sebagai masyarakat Banjar hulu, masyarakat Bakumpai, serta dukungan dari Dayak Murung, Siang dan Taboyan. Dari aspek bukti sejarah, peristiwa perang ini meninggalkan bukti arkeologis termasuk makam tokoh-tokohnya. Melalui metode penelitian survei yang didukung data pustaka, dan informasi masyarakat, jejak perjuangan rakyat Kalimantan dalam menentang penjajahan Belanda dapat tergambarkan. Daerah aliran Sungai Barito telah menjadi saksi perjuangan dan perlawanan rakyat. Hal ini sudah semestinya menjadi landasan berpikir, bahwa kerjasama antarelemen masyarakat, antardaerah, dan antarlembaga di masa depan sangat diperlukan. Perbedaan bukan menjadi alasan, untuk tidak bekerjasama dalam membangun Kalimantan. The Banjar war or the Banjarmasin war can also be called the. The word of Banjar refers to the Islamic community bound by an empire, while Barito refers to the name of a very important river, which flows in parts of South Kalimantan, but more flows in the administrative area of Central Kalimantan. This paper aims to address the problem of why the term of Banjar war can also be referred to as the Barito War based on archaeological evidence. The war refers to a series of popular resistance involving people from diverse origins and backgrounds. Supported by the descendants of the Banjar Sultanate, assisted by ordinary community people from various areas of the batang banyu and Barito River basin communities. Supporter of the war came from the Banua Lima people who were identified as the Banjar hulu people, from the Bakumpai, Dayak Murung, Siang and Taboyan communities. From the aspect of historical evidence, this war event left some archeological evidences including the graves of war figures. Based on the historical evidence supported by the archeological remains of its characters. Through survey research methods supported by library data and public information, the footsteps of the struggle of the Kalimantan people in opposing Dutch colonialism can be illustrated. The Barito River watershed has witnessed the people's struggle and resistance. This should be the basis for cooperation between communities, regions, and institutions in the future. Difference is not a reason for not to cooperate in the development of Kalimantan.  


Phytotaxa ◽  
2014 ◽  
Vol 163 (3) ◽  
pp. 173
Author(s):  
Wayne Takeuchi

Phyllanthera piforsteriana (Apocynaceae) is described from the Sepik River basin in Papua New Guinea. Distributional notes are also provided for P. lancifolia, a frequent associate of the new species but otherwise rarely represented in herbarium collections.


Water History ◽  
2021 ◽  
Author(s):  
Giacomo Parrinello ◽  
Simone Bizzi ◽  
Nicola Surian

AbstractThe morphology of rivers and deltas, like many features of the Earth’s physical geography, is today subject to dramatic and rapid changes due to human actions. Deprived of sediment from their basins and besieged by rising sea levels, many deltas are at risk of complete disappearance. Despite a rich historical scholarship on rivers, we know little about the history of these important geomorphological processes. This paper sheds light on the geomorphological history of rivers by investigating the case of the Po River basin and its delta during the twentieth century. By combining the insights of fluvial geomorphology and a historical methodology, the paper analyses three main drivers of geomorphic alterations in the catchment that had an impact on the delta: hydroelectricity, sand and gravel mining, and methane extraction. In each case, it focuses on how experts, policy-makers, and overseers understood and regulated (or not) these geomorphic alterations. During much of the twentieth century, engineers and hydrologists monitored geomorphic processes with increasing detail, while state and business actors practiced multiple forms of sediment management. For most of the twentieth century, however, experts did not acknowledge the scale and nature of human-induced geomorphic alteration. Sediment management, moreover, did not take into account sediment scarcity until late in the century, and remained exclusively motivated by local concerns. Through this particular case, this paper offers insights on the historical limits to environmental expertise and policy when facing long term and large-scale geomorphic processes, and encourages a more sustained incorporation of fluvial geomorphology into the history of water systems.


Formulation of the problem. A national climate program, complying with the Association Agreement between Ukraine and the EU, is aimed at long-term adaptation measures to climate change, providing for the development of legislation in the field of environmental protection, sectoral strategies, improving air and water quality. These measures require identification of climatic factors’ impact on hydrological characteristics of water bodies in any area in order to protect and improve them, as well as a comprehensive approach to the rational management of water resources. Analysis of previous research. Using mathematical models of atmospheric circulation allows us to obtain generalized calculations of the average global and regional air temperature, characterized by significant errors in case of different models. Problems of further research. Modern changes in climatic conditions in Ukraine are characterized by locality and rapidity: increasing number of anomalous atmospheric phenomena, frequency of droughts, dry winds which, according to preliminary estimates, may lead to reduction of water resources, changes in internal annual redistribution of water temperature and runoff against the background of increasing thermal resources of the territory. The purpose. The article analyses climatic indicators’ influence on the main hydrological characteristics on the example of the Psyol river basin within Ukraine. Research methods. Research methods are presented by statistical and cartographic analysis (correlation analysis method). The initial information is the results of observations contained in the State Climate Cadastre and the State Water Cadastre for the Dnieper Valley. Presentation of the main research material. Analysis of climate change in the Psyol river basin indicates a decrease in water consumption, both in the main river of the basin and in its main tributaries. In addition to changes in temperature and humidity, the reasons for this process were the shifts that occurred in the nature of the intra-annual distribution of the runoff. During the late XX – early XXI century the share of spring floods decreased due to the reduced period of ice phenomena and corresponding decrease in the thickness of the snow cover on the rivers. As a result, the most important component of the annual runoff of rivers began to decrease rapidly. The role of groundwater in the formation of water runoff increased against the background of a predominant decrease in precipitation. This is especially true for medium-size and small rivers, subject to significant anthropogenic pressure: over-regulation of channels, creation of artificial lakes, their shallowing. Practical value. Based on the main provisions of the national environmental policy of Ukraine on the use of water resources and the implementation of European principles of the Water Framework Directive 2000/60 / EC (ERVD) the study of changes in hydrological regime of rivers is of practical importance for sustainable management. Research results. The study of the impact of changes in climatic indicators on hydrological characteristics makes it possible to determine the reference conditions and classes of ecological status of rivers under conditions of anthropogenic pressure against the background of further changes in climatic indicators that will have different trends.


2018 ◽  
Vol 3 (3) ◽  
pp. 403
Author(s):  
Isabel Teresinha Leli ◽  
Rafael Sanches Martins ◽  
Altair Bennert ◽  
Elcisley David Rodrigues de Almeida

A Geomorfologia é a ciência que estuda os processos e produtos envolvidos na construção do relevo, e estes como resultado de um longo e duradouro processo de agentes formadores e escultores do relevo. No contexto do estudo Geomorfológico, para o ensino básico, a Bacia Hidrográfica surge como um elemento substancial para aplicar os conceitos, e como ocorre a transformação do relevo diante dos fenômenos associados. O objetivo deste artigo é propor a bacia hidrográfica como unidade de estudo para estimular o ensino de geomorfologia através das transformações que ocorrem neste meio. Para tanto, foram adotados dois métodos de ensino: Planejamento “Histórico-Crítico” que descreve as fases de abordagem e desenvolvimento durante o processo de ensino e outro que usa um modelo proposto por Piaget, onde os elementos e suas interações estão relacionados com a leitura e a escrita. A aplicação dessa proposta parte da concepção de que todos os elementos naturais que envolvem a transformação do ambiente dentro de uma bacia hidrográfica, devem ser apresentados e discutidos com os alunos em etapas de crescente compreensão. No final, é esperado que os alunos venham adquirir uma percepção baseada na relação entre conceitos e vivência cotidiana, podendo assim, interpretar a paisagem de uma bacia hidrográfica, como resultado de diversos elementos interligados.Abstract:Geomorphology is the science that studies the processes and products involved in the construction of relief, whose development are defined over temporal and spatial scales. As the river is considered the most powerful exogenous relief sculptor element, the hydrographic basin, by its turn, is the stage where act all the involved geomorphological variables. Face with this, the hydrographic basin is recognized by the most of geomorphologists as the fundamental relief unit for understanding relief transformation. Therefore, the understanding of the structure and functioning of a hydrographic basin is also fundamental in the Physical Geography background disciplines. This paper uses the concept of study-unit applied to the hydrographic basin as a base for the understanding the geomorphological processes and landscape changes in the teaching of Geomorphology for the basic education. Therefore, two methods of relief transformation teaching were adopted: "Historical-Critical" Planning that describes the phases of approach and development during the teaching process and another one that uses a model proposed by Piaget, where the elements and their interactions are related to reading and writing. The application of this proposal starts from the idea that all the natural elements that involve the transformation of the environment within a river basin must be presented and discussed with the students in stages of progressive understanding. As a result, it is expected that the students have acquired a perception based on a relationship between concepts and everyday life, in the way they can diagnose a river basin as a result of several interconnected elements.Keywords: Physical Geography; Teaching-learning Relation; Relief; Hydrographic Basin; Rivers


Author(s):  
Charles Coleman ◽  
Cynthia Conrad

The authors of this study endeavor to explore the negative opinions and perceptions of graduate students in business and social science programs, regarding their required statistics and research methods courses. The general sense of instructors of such courses is that students dread and resent having to take courses dealing with statistics and social research because they are both intellectually demanding and require students to call on mathematics skills. Students also seem to put a low value on such courses in terms of application to their own careers.  Clearly, the above-mentioned perceptions derive from intuitive knowledge and anecdotal statements by students. The authors of this study devised a research design to test the validity of the perceptions of negative attitudes among students in their graduate programs and to gain some understanding of the basis of the negativity.


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