A crucial component of child language acquisition is successful generalization. First, a speaker must acquire abstract knowledge of how a particular linguistic-structure conveys meaning, and use this knowledge to generalize the structure to new lexical-items. For example, a speaker can use abstract knowledge of a SUBJECT-VERB-OBJECT structure to produce a sentence such as The man rolled the ball, even if the verb roll has never been encountered in this structure before. Second, a learner must appropriately restrict ‘overgeneralizations’ whereby a structure is used with an unsuitable verb (e.g. *The man fell the boy). The most prominent theories regarding restriction of overgeneralizations are based on frequency of use and (semantic, phonological or pragmatic) compatibility between the item and construction. Since developmental evidence for these accounts is mostly limited to the judgment paradigm, which is unsuitable for testing children aged 5 and under, the aim of this thesis was to examine whether these restriction mechanisms are used by children as young as 3 or 4 – whose generalization mechanisms are at an earlier stage of development - and to develop new paradigms for doing so. Study 1 used a production priming paradigm to examine children’s (aged 3-4; 5-6) restrictions of verbal un- prefixation (e.g., *unbend). Children’s production probability of verbs in un- form (e.g., *unbend) was negatively predicted by the frequency of the target verb in bare form (i.e., bend/s/ed/ing) and by the frequency of synonyms to a verb’s un- form (e.g., straighten for *unbend). Additionally, grammaticality judgments from older children (aged 5-6) revealed that preferences for un- forms were positively related to the extent to which the verb’s semantics overlapped with a covert, probabilistic semantic “cryptotype” of meanings thought to be shared by verbs that are grammatical in un- form (e.g., tie, pack, twist, screw, cover). Study 2 investigated whether overgeneralization errors in the domain of English past-tense (i.e., when ‘regular’ inflections are applied to verbs that require ‘irregular’ inflection; e.g., *sleeped, *throwed) are best attributed to analogy across exemplars, or to a default, “add –ed” rule applied regardless of a verb’s memorized associations. Past-tense forms of novel verbs were elicited by showing children (aged 3-4; 5-6; 6-7; 9-10) animations of an animal performing a novel action described with a novel verb (e.g., gezz; chake) and asking what the animal ‘did yesterday’. A verb’s likelihood of receiving regular inflection (e.g., gezzed, chaked) was positively associated with its phonological similarity to existing regular verbs, consistent with the analogy-based approach. Study 3 investigated the suitability of an online measure of sentence processing, namely Event Related Potentials (ERP), to investigate the role of verb-frequency in restricting transitive overgeneralizations. In line with previous studies, ‘P600’ and ‘LAN’ components were evoked in response to overgeneralization errors. However, the magnitudes of these components were not sensitive to a manipulation of verb-frequency (e.g., *The clown laughed the boy vs. *The clown giggled the boy), raising doubt toward the suitability of ERP for examining the relative acceptability of overgeneralization errors. Overall, the research indicates that even young children’s generalizations are sensitive to the linguistic input (i.e., statistical regularities and generalized semantic or phonological patterns of use) and are not well explained by a system of abstract rules that act on discrete categories, whether this applies to syntactic categories (e.g., add -ed to any instance of the category “VERB”) or discrete verb classes (e.g., a narrow-range rule that acts invariably on any verb that is part of an ‘alternating’ verb-class).

River plays an essential function in providing sediments to the beach stability but this importance has not yet been properly estimated on the Peruvian coastline. So, the aim of this study focuses on the role of river sediments in the stability of the coastline at the Jequetepeque river mouth, located at the northern coast of Peru. This river, whose basin covers an area of ​​4,200 square kilometers, provides in average more than 900 million cubic meters a year (MMC yr-1) of water, and 2.9-8.0 MMC yr-1 of sediments to the ocean. Since the start of the Gallito Ciego dam in 1987, more than 104 MMC of sediments were retained into the reservoir. In order to assess the impact of the dam on the stability of the river mouth, a comparison among different coastline moments (for the years 1962, 1980, 2003 and 2011) with the support of GIS, were made. The results showed that the river mouth retreat to the land between 2003 and 2011 with rates of -2.6 m year-1. Moreover, the retreat of the coastline observed throughout the study area between 1962 and 2011, it could be related to the potential sea level rise and the trend of the worldwide beach erosion. / Los sedimentos fluviales cumplen un papel fundamental para el abastecimiento de las playas en la costa peruana cuya importancia no ha sido aun debidamente estimada. Con este fin, el estudio se centra en el papel que desempeña los sedimentos fluviales en la estabilidad de la línea de costa en la desembocadura del río Jequetepeque, ubicado en la costa norte del Perú. Este río, cuya cuenca abarca una superficie de 4.2 mil kilómetros cuadrados, aporta en promedio más de 900 millones de metros cúbicos al año (MMC año-1) de agua y entre 2.9 y 8.0 MMC año-1 de sedimentos al océano. A partir del inicio de las operaciones de la represa de Gallito Ciego en 1987, más de 104 MMC de sedimentos quedaron retenidos en el embalse. Con el fin de evaluar la influencia de la represa en el comportamiento de la desembocadura, se llevó a cabo la comparación entre las líneas de costa de los años 1962, 1980, 2003 y 2011 con el soporte de SIG. A partir del análisis se identificó el retroceso de la desembocadura entre 2003 y 2011 con tasas de -2.6 m año-1. Por otra parte, el retroceso de la línea de costa observado en toda el área de estudio, entre 1962 y 2011, podría estar relacionado con la posible elevación del nivel del mar y la tendencia a la erosión de las playas a escala global.

Les glaciers des Alpes françaises subissent un recul généralisé depuis la fin du Petit Âge Glaciaire (PAG). Dans le contexte actuel d'élévation de la température et du fait des nombreux enjeux auxquels ils sont associés, l'amélioration de leur suivi apparaît indispensable. Avant ce travail, il n'existait pas d'étude exhaustive récente concernant l'ensemble des glaciers des Alpes françaises, les travaux de Mougin et de Vivian datant respectivement du milieu des années 1920 et 1970. L'objectif de ce travail est de dresser un inventaire diachronique des glaciers des Alpes françaises et de leurs marges proglaciaires. Les données de cet inventaire servent ensuite de base à l'étude des modalités du retrait glaciaire depuis la fin du PAG et à l'établissement de méthodes pour détecter les secteurs susceptibles d'être affectés par des instabilités. L'inventaire diachronique des glaciers des Alpes françaises est réalisé à 3 dates : (i) 2006-2009 à partir des orthophotographies récentes de l'IGN, (ii) 1967-1971 à partir des premières éditions des cartes topographiques 1 :25 000 de l'IGN, et (iii) la fin du PAG (pour les massifs du Mont Blanc, de la Vanoise et des Ecrins), en croisant documents anciens et données géomorphologiques acquises sur le terrain et par photo-interprétation. Les données sont organisées dans un Système d'Information Géographique (SIG) qui permet d'associer cartographie et base de données. La superficie des glaciers était de 275 km² en 2006-2009, 369 km² en 1967-1971 et 544 km² à la fin du PAG pour les massifs du Mont Blanc, de la Vanoise et des Ecrins. A l'échelle régionale, les glaciers ont perdu 25 % de leur superficie depuis la fin des années 1960 et 50 % de leur superficie depuis la fin du PAG. La rétraction des glaciers est environ 2,5 fois plus rapide entre 1967-1971 et 2006-2009 qu'entre la fin du PAG et 1967-1971. A l'échelle individuelle, les glaciers ont perdu en moyenne 52 % de leur superficie entre 1967-1971 et 2006-2009, et 115 ont même disparu. A l'échelle régionale comme individuelle, le retrait glaciaire présente des tendances différentes selon les massifs, la taille des glaciers et leur exposition Des méthodes simples, basées sur les données des inventaires des glaciers et des marges proglaciaires sont établies afin d'identifier les lacs potentiellement instables, les secteurs englacés favorables à la formation de futurs lacs, au déclenchement d'avalanches de séracs ou susceptibles d'être déstabilisés en masse, et les marges proglaciaires favorables à l'occurrence de glissements ou de laves de débris. / French alpine glaciers are retreating since the end of the Little Ice Age (LIA). In the context of the increasing air temperature and because of issues that they represent, it is necessary to improve glacier monitoring. Before the present study, the only two inventories covering the entire French Alps were made by Mougin (1925) and Vivian (1975). The main goal of this study is to realise a multi-temporal glacier inventory of glaciers in the French Alps and of their proglacial margins. Data from this inventory are used to study glacial retreat since the end of the LIA and to develop methods to detect sector that could be affected by instabilities. Multi-temporal inventory of French Alpine glacier glaciers is made for 3 dates: (i) 2006-2009, based on IGN recent orthophotographs, (ii) 1967-1971, based on 1: 25 000 IGN topographic maps, and (iii) the end of the LIA (for Mont Blanc, Vanoise and Ecrins massifs), crossing old documents and geomorphologic data based on field work and interpretation of orthophotographs. Data are integrated in a Geographical Information System (GIS), combining mapping and data base. Glaciers in the French Alps covered 275 km² in 2006-2009, 369 km² in 1967-1971 and 544 km² at the end of the LIA for Mont Blanc, Vanoise and Ecrins massifs. At a regional scale, glaciers lost 25 % of their 1967-1971 area and 50 % of their LIA area. Glacier shrinkage between 1967-1971 and 2006-2009 is about 2.5 times higher than between the end of the LIA and 2006-2009. At an individual scale glaciers lost 52 % of their area between 1967-1971 and 2006-2009, and 115 disappeared. At regional or individual scale, different trends in glacier shrinkage are observed according to the massifs, size and aspect of the glaciers. Simple methods, based on glaciers inventory and proglacial margins data, are developed in order to identify potential unstable lakes, glaciated sectors prone to glacier lake formation, ice avalanche triggering or mass destabilization, and proglacial margins where sliding or debris flows could occur.

Thesis advisor: Jeremy D. Shakun / The deglacial extent chronology of the southeastern Laurentide Ice Sheet as it retreated through the northeastern United States and southern Quebec has been well constrained by multiple lines of evidence. By comparison, few data exist to constrain the thinning history of the southeastern Laurentide, resulting in lingering uncertainty about volume changes and dynamics of this ice mass during the deglacial period. To address the lack of thinning information, my team collected 120 samples for in-situ `10Be exposure dating from various elevations at numerous mountains in New England and southern Quebec. Monte Carlo regression analyses using the analytical uncertainties of exposure ages from each mountain are used to determine the most-likely timing and rate of ice thinning for that location, a technique known as the ‘dipstick approach’. While this larger project is ongoing, I have processed and measured 10Be concentrations of 42 samples for this thesis and present my preliminary results and interpretation here. Exposure ages from Peekamoose Mt. in southern NY suggest ice thinning early in the deglacial period (~19.5 – 17.5 ka), near the onset of the Heinrich Stadial I cold period. Samples from Franconia Notch, NH, and Mt. Mansfield, VT, suggest ice thinning from approximately 15 – 13 ka in northern New England, roughly coincident with the Bølling-Allerød warm period. Exposure ages from each of the northern New England dipsticks are nearly identical within 1σ internal uncertainty, indicating that ice thinning was rapid. Higher elevation (>1200 m a.s.l.) samples from the northern New England mountains appear to contain inherited 10Be from previous periods of exposure, indicating a lack of glacial erosion on these surfaces. My high-elevation samples with inherited 10Be suggest that these summit landscapes were preserved beneath cold-based, non-erosive ice during the last glacial and deglacial periods. 40 samples that have yet to be processed will provide more information on ice thinning around Killington Mt., VT, Mt. Greylock, MA, Mt. Bigelow, ME, and Mt. Jacques-Cartier, Quebec. Ultimately, this information will be used to create probabilistic reconstructions of the lowering southeastern Laurentide ice surface during its retreat. / Thesis (MS) — Boston College, 2018. / Submitted to: Boston College. Graduate School of Arts and Sciences. / Discipline: Earth and Environmental Sciences.

This study uses topographic profiles, washover fan volumes, and shoreline retreat rates to explore relationships between barrier types and Hurricane Harvey storm washover sedimentation. Pre- and post-Hurricane Harvey topographic profiles were created on 15 transects using Bare Earth LiDAR (2016) and surveyed elevations (2019). Depth and area of washover fan measurements were collected to estimate washover fan volumes. An inverse relationship was found between washover fan volume and pre- and post-storm barrier heights. Based on the topographic profiles, one section of shoreline had a scarp up to 3m high which blocked overwash, but appears to have increased shoreline erosion. In contrast, a low-lying section of shoreline generated relatively large washover fans, but experienced less shoreline retreat. Shoreline retreat was further quantified between 2014 and 2019 using Google Earth Imagery from 2014, 2016, 2017, and 2019 to track migration of the shoreline. The entire shoreline in the study area is undergoing relatively rapid retreat, but the results suggest that Hurricane Harvey increased erosional rates. The Colorado River Jetty borders the study area and may have acted as an anthropogenic barrier, likely reducing storm surge energy and contributing to marsh aggradation on transects in its close proximity. The study findings indicate that the identification and incorporation of other variables that influence washover magnitude would further the understanding of this complex natural system. The research results provide valuable information on the interaction of hurricane storm surge with natural and anthropogenic barriers, beach and dune erosion, and marsh aggradation along the coast of Texas.

A consequence of climate change is rising global sea levels, predicted to bring increased socio-economic and environmental impacts to coastal communities. The Greenland Ice Sheet has become a prominent contributor to rising sea levels, a consequence of the Arctic warming at twice the rate of the global average. Mass loss from the ice sheet is separated between changes in surface mass balance and ice discharge at marine terminating outlet glaciers, with the later dominating mass loss over the past fifty years. While advances in ice sheet modelling have provided greater clarity on Greenland’s future mass loss, there remains inefficiencies in modelling the response of outlet glaciers in Greenland’s fjords. This thesis aims to provide greater insight into behaviour of Kangerlussuaq Glacier, SE Greenland, by employing a 2D flowline model to understand the processes governing ice dynamics and to explore how the glacier may respond to a warming climate. Results indicate that the presence of a winter ice mélange is the principle dictator of Kangerlussuaq Glacier’s behaviour and likely protects against further retreat towards a reverse sloped section of bedrock. However, if such a retreat does materialise, then large overdeepenings in Kangerlussuaq Fjord raise the spectre of uncontrollable retreat and excessive mass loss.

In the context of changing climate retreat of mountain glaciers occurs at many places on the planet. One of the consequences is emergence or increase of the outburst risk at lakes situated in front of the glacier terminus. Flood caused by the glacial lake outburst often appear suddenly and can threaten settlements in lower parts of a valley. In the Kyrgyz mountains of Tien Shan there are about 350 lakes at risk of outburst, long-term monitored and dangerous locations are presented in this work. The highest attention is paid to Adygine area where several lakes of different genetic type and age can be found. The largest lake of the locality, the Upper Adygine lake, is subjected to more detailed survey aiming to asses its hydrological regime and to confirm or disprove speculation about outburst possibility of this lake. Keywords: glacial lake, hydrological regime, glacier retreat, Tien Shan, Kyrgyzstan

The narrative research journey and pilgrimage into and epistemological reflection on the relevance of the Benedictine, Franciscan and Taizé monastic-mystic traditions (associative spirituality) for retreat within the Dutch Reformed tradition (disassociate spirituality) began because of a passion for, an interest in retreat and because of lack of research done on the subject. The research developed in story form as a participative active process of story development, interpretation, and reflection in which the researcher and the research subject as valued co-researchers (co-pilgrims) constructed a shared reality and new story together. Consequently, the observations and experiences reflected on may tell just as much about the researcher as about the action of retreat and the research participants. The action of retreat was not approached in a neutral, objective stance but with self-awareness, particular presuppositions, and a postmodern philosophical mindset with ideological-critical, deconstructive and inclusive thought processes. The research problem was viewed as a narrative situation of action, explained by means of empirical research, and interpreted via epistemological reflection and theological theories. The focus has not been on new or adapted theory formulation, hypotheses, or “conclusions” as such but on the empiric interaction between the experiences of Mystery (noumenon), the Jesus narrative, stories of the co-pilgrims, monastic traditions, Dutch Reformed tradition, the researchers’ own story, and those who might read the thesis. A potential amplifying or expanding of the repertoire of existing options and meanings were viewed as a possibility in the creative development of a new reality or research story. The aim was to listen to, understand, and interpret qualitatively the subjective dimension and experience of the reality (story/ies) of retreat as a situation where pilgrims (from different traditions and spiritualities) were in relation with God, self and others. The research journey took me into the life world of the monastic-mystic traditions and my own internal dialectics and story within a Dutch Reformed context. From here arose questions, engagement, and re-engagement with the monastic traditions and a new story. The concern was the beliefs and practices of the retreatants (co pilgrims) under study as beings in real-life human experiential reality, taking seriously their concerns, expressions of belief, practice, perceptions, and stories. The data from the empirical encounter was subsequently investigated, mapped with the major themes and interests highlighted and reflected on in the process. The main themes and focal points that were identified and researched were: -- The lives and stories of St. Benedict, St. Francis, and Br. Roger, their respective communities’ monastic-mystic spirituality, the way these traditions approach retreat and the way they live or express their respective monastic rules or orders in comparison with the Dutch Reformed traditions’ retreat narrative. -- The main elements of Monastic retreat namely silence, solitude, lectio divina in facilitating an awareness of God and the mystery of God as part of the journey to the inner mountain, ever deeper into his presence. -- Different types of retreat and especially the experience of monastic retreat, the experience of holy places (desert spirituality) as places saturated by prayer, Eucharist and the community of pilgrims, and retreat as pilgrimage experience. -- Retreat as ritual following a rite of passage structure of separation, marginality and reincorporation focusing on structure and anti-structure (power of liminality) as helpful tool of analysis and framework for planning of retreat. -- The potential therapeutic or pastoral care qualities of a monastic way of retreat facilitating in pilgrims, life story interpretation and new understanding of stories. The research story ended in the form of findings and the posing of possible questions for future research. / Thesis (PhD (Practical Theology))--University of Pretoria, 2006. / Practical Theology / unrestricted

In my thesis project I wanted to learn about how architecture affects people and how we can design spaces that can make people feel less stressed. I started out by researching about environmental psychology and the senses and combined what I learned into a building that can help promote mental well being.  Stressed people have a harder time living in the present, with so much going on in their head, so a sensoric layer is incorporated, helping people become more present. Colours are used according to colour psychology, creating different moods in different spaces that affect the visitor.The building also provides several social meeting places, spaces where you can relax by yourself and focus inwards, and beautiful views that connect you to nature. My proposed building is a retreat in Sälen, A building that serves as a place for recreation, health and experience, where you are able to take a step back from your stressful life both mentally and physically. The retreat would also become a new destination to visit  all year round, helping with the tourism in Sälen in the summertime.

Dark Retreat - to spend days in total darkness. A qualitative content analysis of people's experiences of dark retreats and the potential health benefits of such a retreat. This essay will examine spiritual and personal development YouTube channels where the content is about what it is like to do a dark retreat. The questions of the study is if they talk about that there are any health and physical benefits in doing a dark retreat and how their experience can be explained. This is linked to one of the key messages in the study which is to point to the altered state of consciousness and what life-changing transformation and positive change that can bring for the person who have experienced a transcendent and mystic state of consciousness. A dark retreat is one practice used in the tantric Tibetan Buddhist movement "the Great Perfection" Dzogchen where a person is for a long time in total darkness to gain knowledge of the emptiness of everything. The dark retreat tradition that is the focus of this study are linked to the new age movement that differs from the Dzogchen tradition regarding dark retreat in that there are no masters or rules that the person doing their dark retreat must follow. There is also an underlying commercial agenda for why people share their experiences of what it is like to do a dark retreat and upload their videos on YouTube. The pattern that became clear with the collection of the material was that those who are doing a dark retreat are working with some form of spiritual and personal development and it is these services that they want to sell by creating an interest by sharing their dark retreat experiences. This is something that is addressed and discussed in the study. The methods are conversation analysis to determine how genuine people are when they talk about their experiences in the dark. Content analysis is used to be able to find themes in the material for how the people experience their dark retreat stay, the focus on themes, phrases and words is linked to health or life-changing transformation. The findings from the content analysis are that people talk about surrender/acceptance when the situation became intense in the dark, that they met themselves/gained new insights, got a glimpse of relationships that have not been good and where there are things to work with and that there were a lot who were positive about their dark retreat stay.