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Geology (from Ancient Greek γῆ ( gê )  'earth' and λoγία ( -logía )  'study of, discourse') is a branch of natural science concerned with the Earth and other astronomical objects , the rocks of which they are composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences , including hydrology . It is integrated with Earth system science and planetary science .

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95-496: In geology and related fields, a stratum ( pl. : strata ) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either bedding surfaces or bedding planes . Prior to the publication of the International Stratigraphic Guide, older publications have defined

190-535: A characteristic fabric . All three types may melt again, and when this happens, new magma is formed, from which an igneous rock may once again solidify. Organic matter, such as coal, bitumen, oil, and natural gas, is linked mainly to organic-rich sedimentary rocks. To study all three types of rock, geologists evaluate the minerals of which they are composed and their other physical properties, such as texture and fabric . Geologists also study unlithified materials (referred to as superficial deposits ) that lie above

285-485: A petrographic microscope , where the minerals can be identified through their different properties in plane-polarized and cross-polarized light, including their birefringence , pleochroism , twinning , and interference properties with a conoscopic lens . In the electron microprobe, individual locations are analyzed for their exact chemical compositions and variation in composition within individual crystals. Stable and radioactive isotope studies provide insight into

380-601: A bed, a flow should only be designated and named as a formal lithostratigraphic unit when it is distinctive, widespread, and useful for stratigraphic correlation. A band is a thin stratum that is distinguishable by a distinctive lithology or color and is useful in correlating strata. Finally, a key bed, also called a marker bed , is a well-defined, easily identifiable stratum or body of strata that has sufficiently distinctive characteristics, such as lithology or fossil content, to be recognized and correlated during geologic field or subsurface mapping. Geology Geology describes

475-448: A cultural product, and thus cannot be understood without consideration of context. Legal researchers conduct field research to understand how legal systems work in practice. Social, economic, cultural and other factors influence how legal processes, institutions and the law work (or do not work). Mintzberg played a crucial role in the popularization of field research in management . The tremendous amount of work that Mintzberg put into

570-434: A definite homogeneous chemical composition and an ordered atomic arrangement. Each mineral has distinct physical properties, and there are many tests to determine each of them. Minerals are often identified through these tests. The specimens can be tested for: A rock is any naturally occurring solid mass or aggregate of minerals or mineraloids . Most research in geology is associated with the study of rocks, as they provide

665-434: A few millimeters to several meters or more. A band may represent a specific mode of deposition : river silt , beach sand , coal swamp , sand dune , lava bed, etc. In the study of rock and sediment strata, geologists have recognized a number of different types of strata, including bed , flow , band , and key bed . A bed is a single stratum that is lithologically distinguishable from other layers above and below it. In

760-475: A field that aims to understand the particularities of contemporary consumption . Several academic journals such as Consumption Markets & Culture , and the Journal of Consumer Research regularly publish qualitative research studies that use fieldwork. In geology fieldwork is considered an essential part of training and remains an important component of many research projects. In other disciplines of

855-627: A length of less than a meter. Rocks at the depth to be ductilely stretched are often also metamorphosed. These stretched rocks can also pinch into lenses, known as boudins , after the French word for "sausage" because of their visual similarity. Where rock units slide past one another, strike-slip faults develop in shallow regions, and become shear zones at deeper depths where the rocks deform ductilely. The addition of new rock units, both depositionally and intrusively, often occurs during deformation. Faulting and other deformational processes result in

950-512: A library of music to be analyzed by other scholars. Methodologies began to shift in the early 20th century. George Herzog, an anthropologist and ethnomusicologist, published a seminal paper titled "Plains Ghost Dance and Great Basin Music", reflecting the increased importance of fieldwork through his extended residency in the Great Basin and his attention to cultural contexts. Herzog also raised

1045-679: A long history. Cultural anthropologists have long used field research to study other cultures. Although the cultures do not have to be different, this has often been the case in the past with the study of so-called primitive cultures, and even in sociology the cultural differences have been ones of class. The work is done... in " 'Fields' that is, circumscribed areas of study which have been the subject of social research". Fields could be education, industrial settings, or Amazonian rain forests. Field research may be conducted by ethologists such as Jane Goodall . Alfred Radcliffe-Brown [1910] and Bronisław Malinowski [1922] were early anthropologists who set

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1140-411: A longer period of time. A strength of observation and interaction over extended periods of time is that researchers can discover discrepancies between what participants say—and often believe—should happen (the formal system) and what actually does happen, or between different aspects of the formal system; in contrast, a one-time survey of people's answers to a set of questions might be quite consistent, but

1235-452: A means to provide information about geological history and the timing of geological events. The principle of uniformitarianism states that the geological processes observed in operation that modify the Earth's crust at present have worked in much the same way over geological time. A fundamental principle of geology advanced by the 18th-century Scottish physician and geologist James Hutton

1330-608: A number of fields, laboratory, and numerical modeling methods to decipher Earth history and to understand the processes that occur on and inside the Earth. In typical geological investigations, geologists use primary information related to petrology (the study of rocks), stratigraphy (the study of sedimentary layers), and structural geology (the study of positions of rock units and their deformation). In many cases, geologists also study modern soils, rivers , landscapes , and glaciers ; investigate past and current life and biogeochemical pathways, and use geophysical methods to investigate

1425-428: A picture will be objective, a matter of fact, independent of the state of mind of the particular agents reported on. Approaching the economy from a different angle, another kind of fieldwork can give us a picture of the state of mind of economic agents (their true motivations, their beliefs, state knowledge, expectations, their preferences and values). Business use of field research is an applied form of anthropology and

1520-456: A range of well-defined, although variable, methods: informal interviews, direct observation , participation in the life of the group, collective discussions, analyses of personal documents produced within the group, self-analysis, results from activities undertaken off- or on-line, and life-histories. Although the method generally is characterized as qualitative research , it may (and often does) include quantitative dimensions. Field research has

1615-451: A sedimentary rock. Sedimentary rocks are mainly divided into four categories: sandstone, shale, carbonate, and evaporite. This group of classifications focuses partly on the size of sedimentary particles (sandstone and shale), and partly on mineralogy and formation processes (carbonation and evaporation). Igneous and sedimentary rocks can then be turned into metamorphic rocks by heat and pressure that change its mineral content, resulting in

1710-499: A single environment and do not necessarily occur in a single order. The Hawaiian Islands , for example, consist almost entirely of layered basaltic lava flows. The sedimentary sequences of the mid-continental United States and the Grand Canyon in the southwestern United States contain almost-undeformed stacks of sedimentary rocks that have remained in place since Cambrian time. Other areas are much more geologically complex. In

1805-648: A sociology of culture, which Bourdieu labeled a "theory of practice". His contributions to sociology were both empirical and theoretical. His conceptual apparatus is based on three key terms: habitus , capital, and field. Furthermore, Bourdieu fiercely opposed rational choice theory as grounded in a misunderstanding of how social agents operate. Bourdieu argued that social agents do not continuously calculate according to explicit rational and economic criteria. According to Bourdieu, social agents operate according to an implicit practical logic—a practical sense—and bodily dispositions. Social agents act according to their "feel for

1900-659: A stratum as being either equivalent to a single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both bed and lamina . Related terms are substrate and substratum (pl. substrata ), a stratum underlying another stratum. Typically, a stratum is generally one of a number of parallel layers that lie one upon another to form enormous thicknesses of strata. The bedding surfaces (bedding planes) that separate strata represent episodic breaks in deposition associated either with periodic erosion , cessation of deposition, or some combination of

1995-400: A variety of applications. Dating of lava and volcanic ash layers found within a stratigraphic sequence can provide absolute age data for sedimentary rock units that do not contain radioactive isotopes and calibrate relative dating techniques. These methods can also be used to determine ages of pluton emplacement. Thermochemical techniques can be used to determine temperature profiles within

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2090-441: Is interviewing , specifically interviewing in the qualitative paradigm. Interviewing can be done in different formats, this all depends on individual researcher preferences, research purpose, and the research question asked. In qualitative research , there are many ways of analyzing data gathered in the field. One of the two most common methods of data analysis are thematic analysis and narrative analysis . As mentioned before,

2185-438: Is a point of view that fits very well with anthropological research, which has for some time shown us the logic of local systems of knowledge — and the damage that can be done when "solutions" to problems are imposed from outside or above without adequate consultation. Elinor Ostrom, for example, combines field case studies and experimental lab work in her research. Using this combination, she contested longstanding assumptions about

2280-582: Is a structured type of research strategy. It is a widely used methodology in many disciplines, particularly, cultural anthropology, but also sociology, communication studies, and social psychology. Its aim is to gain a close and intimate familiarity with a given group of individuals (such as a religious, occupational, or sub cultural group, or a particular community) and their practices through an intensive involvement with people in their natural environment, usually over an extended period of time. The method originated in field work of social anthropologists, especially

2375-422: Is accomplished in two primary ways: through faulting and folding . In the shallow crust, where brittle deformation can occur, thrust faults form, which causes the deeper rock to move on top of the shallower rock. Because deeper rock is often older, as noted by the principle of superposition , this can result in older rocks moving on top of younger ones. Movement along faults can result in folding, either because

2470-460: Is an intimate coupling between the movement of the plates on the surface and the convection of the mantle (that is, the heat transfer caused by the slow movement of ductile mantle rock). Thus, oceanic parts of plates and the adjoining mantle convection currents always move in the same direction – because the oceanic lithosphere is actually the rigid upper thermal boundary layer of the convecting mantle. This coupling between rigid plates moving on

2565-478: Is an unbroken series of reactions to all sorts of request that come from all around the manager, from both the internal and external environments. Third, the manager deals with the same issues several times, for short periods of time; he or she is far from the traditional image of the individual who deals with one problem at a time, in a calm and orderly fashion. Fourth, the manager acts as a focal point, an interface, or an intersection between several series of actors in

2660-399: Is as likely to be advised by sociologists or statisticians in the case of surveys. Consumer marketing field research is the primary marketing technique that is used by businesses to research their target market. Fieldwork in ethnomusicology has changed greatly over time. Alan P. Merriam cites the evolution of fieldwork as a constant interplay between the musicological and ethnological roots of

2755-416: Is essential to the process. Field notes are a key part of the ethnographic record. The process of field notes begin as the researcher participates in local scenes and experiences in order to make observations that will later be written up. The field researcher tries first to take mental notes of certain details in order that they be written down later. Field Note Chart Another method of data collection

2850-574: Is essentially a relational procedure whose philosophy fully expresses what in my view constitutes social reality. It is a procedure that 'thinks' in relations, as I try to do it with the concept of field." One of the classic ethnographies in Sociology is the book Ain't No Makin' It: Aspirations & Attainment in a Low-Income Neighborhood by Jay MacLeod. The study addresses the reproduction of social inequality among low-income, male teenagers. The researcher spent time studying two groups of teenagers in

2945-433: Is horizontal). The principle of superposition states that a sedimentary rock layer in a tectonically undisturbed sequence is younger than the one beneath it and older than the one above it. Logically a younger layer cannot slip beneath a layer previously deposited. This principle allows sedimentary layers to be viewed as a form of the vertical timeline, a partial or complete record of the time elapsed from deposition of

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3040-616: Is important for mineral and hydrocarbon exploration and exploitation, evaluating water resources , understanding natural hazards , remediating environmental problems, and providing insights into past climate change . Geology is a major academic discipline , and it is central to geological engineering and plays an important role in geotechnical engineering . The majority of geological data comes from research on solid Earth materials. Meteorites and other extraterrestrial natural materials are also studied by geological methods. Minerals are naturally occurring elements and compounds with

3135-530: Is less likely to show conflicts between different aspects of the social system or between conscious representations and behavior. Field research lies at the heart of archaeological research. It may include the undertaking of broad area surveys (including aerial surveys ); of more localised site surveys (including photographic, drawn , and geophysical surveys, and exercises such as fieldwalking ); and of excavation . In biology , field research typically involves studying of free-living wild animals in which

3230-484: Is primarily accomplished through normal faulting and through the ductile stretching and thinning. Normal faults drop rock units that are higher below those that are lower. This typically results in younger units ending up below older units. Stretching of units can result in their thinning. In fact, at one location within the Maria Fold and Thrust Belt , the entire sedimentary sequence of the Grand Canyon appears over

3325-568: Is that "the present is the key to the past." In Hutton's words: "the past history of our globe must be explained by what can be seen to be happening now." The principle of intrusive relationships concerns crosscutting intrusions. In geology, when an igneous intrusion cuts across a formation of sedimentary rock , it can be determined that the igneous intrusion is younger than the sedimentary rock. Different types of intrusions include stocks, laccoliths , batholiths , sills and dikes . The principle of cross-cutting relationships pertains to

3420-523: Is used for geologically young materials containing organic carbon . The geology of an area changes through time as rock units are deposited and inserted, and deformational processes alter their shapes and locations. Rock units are first emplaced either by deposition onto the surface or intrusion into the overlying rock . Deposition can occur when sediments settle onto the surface of the Earth and later lithify into sedimentary rock, or when as volcanic material such as volcanic ash or lava flows blanket

3515-535: The Earth and atmospheric sciences , field research refers to field experiments (such as the VORTEX projects ) utilizing in situ instruments. Permanent observation networks are also maintained for other uses but are not necessarily considered field research, nor are permanent remote sensing installations. The objective of field research in economics is to get beneath the surface, to contrast observed behaviour with

3610-506: The bedrock . This study is often known as Quaternary geology , after the Quaternary period of geologic history, which is the most recent period of geologic time. Magma is the original unlithified source of all igneous rocks . The active flow of molten rock is closely studied in volcanology , and igneous petrology aims to determine the history of igneous rocks from their original molten source to their final crystallization. In

3705-512: The geochemical evolution of rock units. Petrologists can also use fluid inclusion data and perform high temperature and pressure physical experiments to understand the temperatures and pressures at which different mineral phases appear, and how they change through igneous and metamorphic processes. This research can be extrapolated to the field to understand metamorphic processes and the conditions of crystallization of igneous rocks. This work can also help to explain processes that occur within

3800-402: The mantle below (separated within itself by seismic discontinuities at 410 and 660 kilometers), and the outer core and inner core below that. More recently, seismologists have been able to create detailed images of wave speeds inside the earth in the same way a doctor images a body in a CT scan . These images have led to a much more detailed view of the interior of the Earth, and have replaced

3895-483: The structure of the Earth on and beneath its surface and the processes that have shaped that structure. Geologists study the mineralogical composition of rocks in order to get insight into their history of formation. Geology determines the relative ages of rocks found at a given location; geochemistry (a branch of geology) determines their absolute ages . By combining various petrological, crystallographic, and paleontological tools, geologists are able to chronicle

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3990-440: The 1960s, it was discovered that the Earth's lithosphere , which includes the crust and rigid uppermost portion of the upper mantle , is separated into tectonic plates that move across the plastically deforming, solid, upper mantle, which is called the asthenosphere . This theory is supported by several types of observations, including seafloor spreading and the global distribution of mountain terrain and seismicity. There

4085-424: The Earth, such as subduction and magma chamber evolution. Structural geologists use microscopic analysis of oriented thin sections of geological samples to observe the fabric within the rocks, which gives information about strain within the crystalline structure of the rocks. They also plot and combine measurements of geological structures to better understand the orientations of faults and folds to reconstruct

4180-484: The Grand Canyon in the southwestern United States being a very visible example, the lower rock units were metamorphosed and deformed, and then deformation ended and the upper, undeformed units were deposited. Although any amount of rock emplacement and rock deformation can occur, and they can occur any number of times, these concepts provide a guide to understanding the geological history of an area. Geologists use

4275-537: The beginning of the 20th century, advancement in geological science was facilitated by the ability to obtain accurate absolute dates to geological events using radioactive isotopes and other methods. This changed the understanding of geological time. Previously, geologists could only use fossils and stratigraphic correlation to date sections of rock relative to one another. With isotopic dates, it became possible to assign absolute ages to rock units, and these absolute dates could be applied to fossil sequences in which there

4370-482: The better will be the absorption of those ideas. Better grasping of such material means a better understanding of the forces of culture operating in the area and the ways they modify the lives of the people under study. Social scientists (i.e. anthropologists, social psychologists, etc.) have always been taught to be free from ethnocentrism (i.e. the belief in the superiority of one's own ethnic group), when conducting any type of field research. When humans themselves are

4465-473: The classification hierarchy of sedimentary lithostratigraphic units, a bed is the smallest formal unit. However, only beds that are distinctive enough to be useful for stratigraphic correlation and geologic mapping are customarily given formal names and considered formal lithostratigraphic units. The volcanic equivalent of a bed, a flow, is a discrete extrusive volcanic stratum or body distinguishable by texture, composition, or other objective criteria. As in case of

4560-542: The community the anthropologist is studying, and data analysis. Traditional participant observation is usually undertaken over an extended period of time, ranging from several months to many years, and even generations. An extended research time period means that the researcher is able to obtain more detailed and accurate information about the individuals, community, and/or population under study. Observable details (like daily time allotment) and more hidden details (like taboo behavior) are more easily observed and interpreted over

4655-412: The contrary, it is fragmented, irregular, choppy, extremely changeable and variable. This work is also marked by brevity: no sooner has a manager finished one activity than he or she is called up to jump to another, and this pattern continues nonstop. Second, the manager’s daily work is a not a series of self-initiated, willful actions transformed into decisions, after examining the circumstances. Rather, it

4750-515: The creation of topographic gradients, causing material on the rock unit that is increasing in elevation to be eroded by hillslopes and channels. These sediments are deposited on the rock unit that is going down. Continual motion along the fault maintains the topographic gradient in spite of the movement of sediment and continues to create accommodation space for the material to deposit. Deformational events are often also associated with volcanism and igneous activity. Volcanic ashes and lavas accumulate on

4845-437: The crust, the uplift of mountain ranges, and paleo-topography. Fractionation of the lanthanide series elements is used to compute ages since rocks were removed from the mantle. Other methods are used for more recent events. Optically stimulated luminescence and cosmogenic radionuclide dating are used to date surfaces and/or erosion rates. Dendrochronology can also be used for the dating of landscapes. Radiocarbon dating

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4940-425: The discipline. Before the 1950s, before ethnomusicology resembled what it is today, fieldwork and research were considered separate tasks. Scholars focused on analyzing music outside of its context through a scientific lens, drawing from the field of musicology. Notable scholars include Carl Stumf and Eric von Hornbostel, who started as Stumpf's assistant. They are known for making countless recordings and establishing

5035-657: The epidemic (such as the pathogen and vector(s) as well as social or sexual contacts, depending upon the situation). Pierre Bourdieu played a crucial role in popularizing fieldwork in sociology. During the Algerian War in 1958–1962, Bourdieu undertook ethnographic research into the clash through a study of the Kabyle people (a subgroup of the Berbers ), which provided the groundwork for his anthropological reputation. His first book, Sociologie de L'Algerie ( The Algerians ),

5130-570: The fault is a normal fault or a thrust fault . The principle of inclusions and components states that, with sedimentary rocks, if inclusions (or clasts ) are found in a formation, then the inclusions must be older than the formation that contains them. For example, in sedimentary rocks, it is common for gravel from an older formation to be ripped up and included in a newer layer. A similar situation with igneous rocks occurs when xenoliths are found. These foreign bodies are picked up as magma or lava flows, and are incorporated, later to cool in

5225-403: The faults are not planar or because rock layers are dragged along, forming drag folds as slip occurs along the fault. Deeper in the Earth, rocks behave plastically and fold instead of faulting. These folds can either be those where the material in the center of the fold buckles upwards, creating " antiforms ", or where it buckles downwards, creating " synforms ". If the tops of the rock units within

5320-409: The findings earned him the title of leader of a new school of management, the descriptive school, as opposed to the prescriptive and normative schools that preceded his work. The schools of thought derive from Taylor, Henri Fayol , Lyndall Urwick , Herbert A. Simon , and others endeavored to prescribe and expound norms to show what managers must or should do. With the arrival of Mintzberg, the question

5415-483: The folds remain pointing upwards, they are called anticlines and synclines , respectively. If some of the units in the fold are facing downward, the structure is called an overturned anticline or syncline, and if all of the rock units are overturned or the correct up-direction is unknown, they are simply called by the most general terms, antiforms, and synforms. Even higher pressures and temperatures during horizontal shortening can cause both folding and metamorphism of

5510-404: The formation of faults and the age of the sequences through which they cut. Faults are younger than the rocks they cut; accordingly, if a fault is found that penetrates some formations but not those on top of it, then the formations that were cut are older than the fault, and the ones that are not cut must be younger than the fault. Finding the key bed in these situations may help determine whether

5605-414: The game" (the "feel" being, roughly, habitus, and the "game" being the field). Bourdieu's anthropological work was focused on the analysis of the mechanisms of reproduction of social hierarchies. Bourdieu criticized the primacy given to the economic factors, and stressed that the capacity of social actors to actively impose and engage their cultural productions and symbolic systems plays an essential role in

5700-579: The geological history of the Earth as a whole. One aspect is to demonstrate the age of the Earth . Geology provides evidence for plate tectonics , the evolutionary history of life , and the Earth's past climates . Geologists broadly study the properties and processes of Earth and other terrestrial planets. Geologists use a wide variety of methods to understand the Earth's structure and evolution, including fieldwork , rock description , geophysical techniques , chemical analysis , physical experiments , and numerical modelling . In practical terms, geology

5795-717: The history of rock deformation in the area. In addition, they perform analog and numerical experiments of rock deformation in large and small settings. Fieldwork Field research , field studies , or fieldwork is the collection of raw data outside a laboratory , library , or workplace setting. The approaches and methods used in field research vary across disciplines . For example, biologists who conduct field research may simply observe animals interacting with their environments , whereas social scientists conducting field research may interview or observe people in their natural environments to learn their languages, folklore , and social structures. Field research involves

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5890-443: The importance of examining institutional contexts when performing economic analyses. Both Ostrom and Williamson agree that "top-down" panaceas or "cookie cutter" approaches to policy problems don't work. They believe that policymakers need to give local people a chance to shape the systems used to allocate resources and resolve disputes. Sometimes, Ostrom points out, local solutions can be the most efficient and effective options. This

5985-423: The internal composition and structure of the Earth. Seismologists can use the arrival times of seismic waves to image the interior of the Earth. Early advances in this field showed the existence of a liquid outer core (where shear waves were not able to propagate) and a dense solid inner core . These advances led to the development of a layered model of the Earth, with a lithosphere (including crust) on top,

6080-464: The later end of the scale, it is marked by the present day (in the Holocene epoch ). The following five timelines show the geologic time scale to scale. The first shows the entire time from the formation of the Earth to the present, but this gives little space for the most recent eon. The second timeline shows an expanded view of the most recent eon. In a similar way, the most recent era is expanded in

6175-454: The lowest layer to deposition of the highest bed. The principle of faunal succession is based on the appearance of fossils in sedimentary rocks. As organisms exist during the same period throughout the world, their presence or (sometimes) absence provides a relative age of the formations where they appear. Based on principles that William Smith laid out almost a hundred years before the publication of Charles Darwin 's theory of evolution ,

6270-497: The mantle and show the crystallographic structures expected in the inner core of the Earth. The geological time scale encompasses the history of the Earth. It is bracketed at the earliest by the dates of the first Solar System material at 4.567 Ga (or 4.567 billion years ago) and the formation of the Earth at 4.54 Ga (4.54 billion years), which is the beginning of the Hadean eon  – a division of geological time. At

6365-405: The matrix. As a result, xenoliths are older than the rock that contains them. The principle of original horizontality states that the deposition of sediments occurs as essentially horizontal beds. Observation of modern marine and non-marine sediments in a wide variety of environments supports this generalization (although cross-bedding is inclined, the overall orientation of cross-bedded units

6460-427: The models for future work. The quality of results obtained from field research depends on the data gathered in the field. The data in turn, depend upon the field worker, their level of involvement, and ability to see and visualize things that other individuals visiting the area of study may fail to notice. The more open researchers are to new ideas, concepts, and things which they may not have seen in their own culture,

6555-492: The number of field courses has not kept pace with demand. Cost has been a barrier to student participation. In applied business disciplines, such as in marketing , fieldwork is a standard research method both for commercial purposes, like market research , and academic research . For instance, researchers have used ethnography , netnography , and in-depth interviews within Consumer Culture Theory ,

6650-424: The organization: external and internal environments, collaborators, partners, superiors, subordinates, colleagues, and so forth. He or she must constantly ensure, achieve, or facilitate interactions between all these categories of actors to allow the firm to function smoothly.’’ In public health , the use of the term field research refers to epidemiology or the study of epidemics through the gathering of data about

6745-536: The possibility that groups of people could cooperate to solve common pool problems, as opposed to being regulated by the state or governed by the market. Edward J. Nell argued in 1998 that there are two types of field research in economics. One kind can give us a carefully drawn picture of institutions and practices, general in that it applies to all activities of a certain kind of particular society or social setting, but still specialized to that society or setting. Although institutions and practices are intangibles, such

6840-480: The prevailing understanding of a process, and to relate language and description to behavior ( Deirdre McCloskey , 1985) . The 2009 Nobel Prize Winners in Economics, Elinor Ostrom and Oliver Williamson , have advocated mixed methods and complex approaches in economics and hinted implicitly to the relevance of field research approaches in economics. In a recent interview Oliver Williamson and Elinor Ostrom discuss

6935-413: The primary record of the majority of the geological history of the Earth. There are three major types of rock: igneous , sedimentary , and metamorphic . The rock cycle illustrates the relationships among them (see diagram). When a rock solidifies or crystallizes from melt ( magma or lava ), it is an igneous rock . This rock can be weathered and eroded , then redeposited and lithified into

7030-569: The principles of succession developed independently of evolutionary thought. The principle becomes quite complex, however, given the uncertainties of fossilization, localization of fossil types due to lateral changes in habitat ( facies change in sedimentary strata), and that not all fossils formed globally at the same time. Geologists also use methods to determine the absolute age of rock samples and geological events. These dates are useful on their own and may also be used in conjunction with relative dating methods or to calibrate relative methods. At

7125-419: The question of how the formal qualities of the music he was studying demonstrated the social function of the music itself. Ethnomusicology today relies heavily on the relationship between the researcher and their teachers and consultants. Many ethnomusicologists have assumed the role of student in order to fully learn an instrument and its role in society. Research in the discipline has grown to consider music as

7220-456: The reproduction of social structures of domination. Bourdieu's empirical work played a crucial role in the popularization of correspondence analysis and particularly multiple correspondence analysis . Bourdieu held that these geometric techniques of data analysis are, like his sociology, inherently relational. In the preface to his book The Craft of Sociology , Bourdieu argued that: "I use Correspondence Analysis very much, because I think that it

7315-428: The rocks. This metamorphism causes changes in the mineral composition of the rocks; creates a foliation , or planar surface, that is related to mineral growth under stress. This can remove signs of the original textures of the rocks, such as bedding in sedimentary rocks, flow features of lavas , and crystal patterns in crystalline rocks . Extension causes the rock units as a whole to become longer and thinner. This

7410-433: The simplified layered model with a much more dynamic model. Mineralogists have been able to use the pressure and temperature data from the seismic and modeling studies alongside knowledge of the elemental composition of the Earth to reproduce these conditions in experimental settings and measure changes within the crystal structure. These studies explain the chemical changes associated with the major seismic discontinuities in

7505-532: The southwestern United States, sedimentary, volcanic, and intrusive rocks have been metamorphosed, faulted, foliated, and folded. Even older rocks, such as the Acasta gneiss of the Slave craton in northwestern Canada , the oldest known rock in the world have been metamorphosed to the point where their origin is indiscernible without laboratory analysis. In addition, these processes can occur in stages. In many places,

7600-874: The students of Franz Boas in the United States, and in the urban research of the Chicago School of sociology. Max Gluckman noted that Bronisław Malinowski significantly developed the idea of fieldwork, but it originated with Alfred Cort Haddon in England and Franz Boas in the United States. Robert G. Burgess concluded that "it is Malinowski who is usually credited with being the originator of intensive anthropological field research". Anthropological fieldwork uses an array of methods and approaches that include, but are not limited to: participant observation, structured and unstructured interviews , archival research , collecting demographic information from

7695-411: The subject of study, protocols must be devised to reduce the risk of observer bias and the acquisition of too theoretical or idealized explanations of the workings of a culture. Participant observation, data collection, and survey research are examples of field research methods, in contrast to what is often called experimental or lab research. When conducting field research, keeping an ethnographic record

7790-417: The subjects are observed in their natural habitat , without changing, harming, or materially altering the setting or behavior of the animals under study. Field research is an indispensable part of biological science. Animal migration tracking (including bird ringing /banding) is a frequently-used field technique, allowing field scientists to track migration patterns and routes, and animal longevity in

7885-550: The subsurface. Sub-specialities of geology may distinguish endogenous and exogenous geology. Geological field work varies depending on the task at hand. Typical fieldwork could consist of: In addition to identifying rocks in the field ( lithology ), petrologists identify rock samples in the laboratory. Two of the primary methods for identifying rocks in the laboratory are through optical microscopy and by using an electron microprobe . In an optical mineralogy analysis, petrologists analyze thin sections of rock samples using

7980-407: The surface of the Earth and the convecting mantle is called plate tectonics . The development of plate tectonics has provided a physical basis for many observations of the solid Earth . Long linear regions of geological features are explained as plate boundaries: Plate tectonics has provided a mechanism for Alfred Wegener 's theory of continental drift , in which the continents move across

8075-488: The surface of the Earth over geological time. They also provided a driving force for crustal deformation, and a new setting for the observations of structural geology. The power of the theory of plate tectonics lies in its ability to combine all of these observations into a single theory of how the lithosphere moves over the convecting mantle. Advances in seismology , computer modeling , and mineralogy and crystallography at high temperatures and pressures give insights into

8170-479: The surface, and igneous intrusions enter from below. Dikes , long, planar igneous intrusions, enter along cracks, and therefore often form in large numbers in areas that are being actively deformed. This can result in the emplacement of dike swarms , such as those that are observable across the Canadian shield, or rings of dikes around the lava tube of a volcano. All of these processes do not necessarily occur in

8265-742: The surface. Igneous intrusions such as batholiths , laccoliths , dikes , and sills , push upwards into the overlying rock, and crystallize as they intrude. After the initial sequence of rocks has been deposited, the rock units can be deformed and/or metamorphosed . Deformation typically occurs as a result of horizontal shortening, horizontal extension , or side-to-side ( strike-slip ) motion. These structural regimes broadly relate to convergent boundaries , divergent boundaries , and transform boundaries, respectively, between tectonic plates. When rock units are placed under horizontal compression , they shorten and become thicker. Because rock units, other than muds, do not significantly change in volume , this

8360-407: The third timeline, the most recent period is expanded in the fourth timeline, and the most recent epoch is expanded in the fifth timeline. Horizontal scale is Millions of years (above timelines) / Thousands of years (below timeline) Epochs: Methods for relative dating were developed when geology first emerged as a natural science . Geologists still use the following principles today as

8455-444: The two. Stacked together with other strata, individual stratum can form composite stratigraphic units that can extend over hundreds of thousands of square kilometers of the Earth 's surface. Individual stratum can cover similarly large areas. Strata are typically seen as bands of different colored or differently structured material exposed in cliffs , road cuts, quarries , and river banks. Individual bands may vary in thickness from

8550-481: The type of analysis a researcher decides to use depends on the research question asked, the researcher's field, and the researcher's personal method of choice. In anthropology , field research is organized so as to produce a kind of writing called ethnography . Ethnography can refer to both a methodology and a product of research, namely a monograph or book. Ethnography is a grounded, inductive method that heavily relies on participant-observation. Participant observation

8645-482: The wild. Knowledge about animal migrations is essential to accurately determining the size and location of protected areas . Field research also can involve study of other kingdoms of life, such as plantae , fungi , and microbes , as well as ecological interactions among species. Field courses have been shown to be efficacious for generating long-term interest in and commitment for undergraduate students in STEM, but

8740-470: Was based on his decade of work as a participant-observer in Algerian society. One of the outstanding qualities of his work has been his innovative combination of different methods and research strategies and his analytical skills in interpreting the obtained data. Throughout his career, Bourdieu sought to connect his theoretical ideas with empirical research grounded in everyday life. His work can be seen as

8835-615: Was datable material, converting the old relative ages into new absolute ages. For many geological applications, isotope ratios of radioactive elements are measured in minerals that give the amount of time that has passed since a rock passed through its particular closure temperature , the point at which different radiometric isotopes stop diffusing into and out of the crystal lattice . These are used in geochronologic and thermochronologic studies. Common methods include uranium–lead dating , potassium–argon dating , argon–argon dating and uranium–thorium dating . These methods are used for

8930-429: Was no longer what must or should be done, but what a manager actually does during the day. More recently, in his 2004 book Managers Not MBAs, Mintzberg examined what he believes to be wrong with management education today. Aktouf (2006, p. 198) summed-up Mintzberg observations about what takes place in the field:‘’First, the manager’s job is not ordered, continuous, and sequential, nor is it uniform or homogeneous. On

9025-711: Was successful in France and published in America in 1962. A follow-up, Algeria 1960: The Disenchantment of the World: The Sense of Honour: The Kabyle House or the World Reversed: Essays , published in English in 1979 by Cambridge University Press , established him as a significant figure in the field of ethnology and a pioneer advocate scholar for more intensive fieldwork in social sciences. The book

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