This thesis examines the impact of different customary manorial tenures on the land transfer activities of rural tenants between 1645 and 1705. The study of land transfer has formed part of the attempt by historians to establish how and why England developed from family-based subsistence farming into large-scale commercialised agriculture before many of its Continental neighbours. A key element in any study of land transfer is the property rights of those undertaking the transfers. England had a variety of customary tenures, and little research has focussed on how they operated and impacted on rural tenant transfer behaviour in the early modern period. This study uses evidence from eight manors in Hampshire with four different types of tenure to explore how they affected what land transfer options the tenants had, and how transfers were used to further family and economic objectives. The types of tenure were copyhold of inheritance; copyhold for three lives; copyhold for three lives where the first could act alone; and a form of customary freehold. The main documentary sources are manorial records augmented by parish, probate, survey and taxation material. The tenurial and landholding structure of the manors is established for 1645 using the Cromwellian Parliamentary Surveys of confiscated ecclesiastical estates. The analysis of subsequent tenant land transfers through to 1705 then examines their volume and any correlation with prices and population movements. The permanent transfers of death/inheritance and the inter vivos land market are analysed to assess the extent to which tenants were attached still to family, or taking part in an active extra-familial investment and sales market; and whether this led to changes over time in farm holding size and distribution. The temporary transfers of sub-letting of land and sub-tenure of dwellings are then analysed. The latter has not been studied before, and uses the Hearth Tax returns to compare occupiers of dwellings with formal tenants. Finally a detailed study of mortgages is made. Previous studies of the use of land as collateral for a mortgage loan have often overlooked the rural tenant as a participant in the credit market, and changes in the laws of usury at the end of the sixteenth century produced a significant uptake of mortgaging in the seventeenth, which makes this study timely. The research reveals that the tenants were very active with their transfers, but that the way in which they were active was determined by tenure. Those with copyhold of inheritance tenure had many options including inheritance, sale, mortgaging, sub-letting, splitting holdings, and conditional surrenders to provide for old age or several children. Those with copyhold for lives were restricted to after-death transfers, shuffling of reversion lives, or sub-letting. However, they adapted, and while Inheritance-tenured tenants adopted mortgages with enthusiasm, Lives tenants sub-let on a large scale. Both thereby acquired financial support from their lands, so that although the land-family bond was not absent, the bond was strongest in terms of using the land as an economic asset. The sub-letting of dwellings enabled Lives tenants to accommodate a landless workforce, where their tenure prevented the splitting of parcels for sale as manorial smallholdings. Aggressive accumulation of land was largely absent, and purchasers of land and mortgage lenders were overwhelmingly local. Some polarisation of holding size was found, but sub-tenure meant that actual farmed units were probably very different. It is concluded that differences in tenure significantly shaped the transfer behaviour of the tenants, so that any future research involving customary tenants must take tenure into account. However, their economic ambitions were found to be similar whichever tenure they had, so that they had to take different means to the same end.

The Cornish Colony (1895 - 1920) was a group of artists, writers, actors, musicians and public figures attracted to the rural beauty of Cornish, New Hampshire. The colony developed into a social and innovative community of common interests and artistic values that included over 75 artists who shared a love of classical traditions in literature and art. Colony Members included: Augustus Saint-Gardens, Thomas Dewing, Charles Adams Platt, Louis Evan Shipman, Juliet Barrett Rublee, Maxfield Parrish, Lucia Fairchild Fuller, Percy MacKaye and Winston Churchill. This thesis will explore the theatrical productions in the colony based in collaboration between visual and theatrical artists in the Colony and how this collaboration extended to the townspeople. It will also explore how the Colony’s dramatics had an influence on the artistic growth of Cornish and the surrounding Upper Valley of Vermont and New Hampshire.

Subvolcanically emplaced granitic, miarolitic pegmatites associated with the White Mountain Igneous Province (WMIP), New Hampshire, were sampled and analyzed using modern analytical techniques including X-ray fluorescence, electron microprobe, scanning electron microscopy, and direct-coupled plasma spectrophotometry. Analytical results suggest that all the sampled miarolitic pegmatites from this study are petrogenetically related to the same intrusive suite, the WMIP. Based on the geochemical data, all the samples formed in an anorogenic tectonic setting and are rift-related. They are classified as NYF-type and plot in the “within plate granite” field on tectonic discrimination diagrams. The majority of the samples are peraluminous, A1-type granites. The trace element abundances on the spider diagram and chondrite-normalized diagram, which include a pronounced negative Eu anomaly and REE enrichments, are consistent with these miarolitic pegmatites resulting from a strongly fractionated granitic parental melts, but less fractionated than the classic NYF-systems such as South Platte (Simmons et al. 1987) and the Wausau Syenite Complex (Meyers et al. 1984).

Thesis (M.M.E.)--Boston University / PLEASE NOTE: Boston University Libraries did not receive an Authorization To Manage form for this thesis or dissertation. It is therefore not openly accessible, though it may be available by request. If you are the author or principal advisor of this work and would like to request open access for it, please contact us at open-help@bu.edu. Thank you. / 2031-01-01

Texte remanié de: D.Phil.--University of Oxford, 1998. / Bibliogr. p. 108-130.

Two studies were conducted to evaluate the effectiveness of using copper sulfate (CuSO4) as a drench in Hampshire ewes to control stomach worms (Haemonchus contortus). A study was conducted to assess the effectiveness of CuSO4 to control gastrointestinal nematodes (GIN) over a three year period. Ewes were FAMACHA scored, hematocrit evaluated for packed cell volume (PCV), and fecal egg counts (FEC) were determined from 2007 through 2009. Ewes received only CuSO4 to control GIN. Ewes with FEC exceeding 6,000 eggs/g feces were drenched. A separate study during the summer of 2008 assessed the potential of CuSO4 drench to cause copper toxicity in Hampshire ewes. Eighty-four ewes were blocked to one of two treatments according to parity and balanced for FEC. One group received CuSO4 (D) and the other was not drenched (ND). Jugular blood samples were collected at pre-determined intervals after CuSO4 was administered to D ewes. Serum was analyzed for aspartate aminotransferase (AST), alanine aminotransferase (ALT), and creatine kinase (CK). Elevated serum levels indicate copper toxicity. Results suggest CuSO4 has the potential to control stomach worms in Hampshire ewes without causing copper toxicity.

Theses (M.S.)--University of New Hampshire (Dept. of Zoology), 2007. / Includes bibliographical references. Also available online.

New Hampshire has become a competitive swing state in presidential elections over the past two decades. Though New Hampshire was once a reliable red state and the home for many “Yankee Republicans,” the state has experienced a shift toward the Democratic Party beginning in the early 1990s. Scholars often attribute this shift to the “migration theory,” arguing that the influx of Massachusetts liberals who migrated to New Hampshire in the latter half of the twentieth century has created a larger Democratic voting bloc in the state. However, a county-level analysis of New Hampshire provides a different story. Southern urban counties with the highest migration rates, such as Hillsborough and Rockingham, had relatively small gains of Democratic voters and remain competitive swing counties. Northern rural counties with much lower migration rates, such as Coos and Grafton, have experienced a far greater political shift to the left. By using both of these case studies, this report casts doubt on the “migration theory” by showing that numerical migration rates do not fully account for New Hampshire’s shift. Instead, this report finds that the different types of economies in the southern and northern parts of New Hampshire significantly influence the political effects of migration in the state, offering a more nuanced theory based on county-level data than the one currently provided for the state as a whole.

Though the American marten (Martes americana) is widely distributed across northern North America, habitat use and population abundance vary widely across the range. Due to its status as a furbearer, the species has been extensively researched, resulting in a large body of knowledge about the species’ ecology, distribution, and abundance, as well as drivers of population structure and dynamics. More recently, marten research has shifted focus to genetics, habitat associations, and estimation of population state variables. The rapid increase in estimation of states such as occupancy, abundance, and density has likely been driven by the increasing accessibility of noninvasive field technology, such as noninvasive genetic sampling and remote camera trapping, and by the statistical development of ecological hierarchical models. This convergence of advances in field and analytical methods is most apparent in the now widespread application of spatial capture-recapture, an approach that produces robust estimates of population densities and abundance that can be compared across time and space. These new models are especially valuable near the edges of marten distribution where populations are often recovering from historic overexploitation, and expanding into areas they have previously been absent from. In these areas, detailed, landscape-scale understanding of marten populations is necessary in order to establish current conditions, effectively monitor changes, and predict what effect management actions may have on marten populations. I utilized these models to study marten populations in New Hampshire where marten are a species of management interest, and recent recovery has led to their removal from the state endangered species list. Through a collaborative effort with New Hampshire Fish and Game Department in the winters of 2017 and 2018, marten were surveyed across northern New Hampshire using a novel camera trap design that allows for the identification of individuals. These data were analyzed using spatial capture-recapture models, allowing me to evaluate habitat associations that explain spatial variation in marten density and provide a population status assessment for the New Hampshire marten population. Marten densities are highest in the White Mountain National Forest, though other protected lands in northern New Hampshire also appear to support larger populations. The greatest population densities coincided with deeper snows, increased canopy closure, and intermediate boreal biomass. These results provide additional support for several hypotheses explaining marten habitat use across their range while also providing novel insight that will inform active management of both marten and the habitat they occur in. In addition to the population status assessment, I evaluated the relationship between estimates of occupancy and density in New Hampshire. Though utility of non-invasive methodology can decrease research costs, the need for individual identification in spatial capture-recapture models represents a cost increase over occupancy models. My results suggest that the two are positively correlated; however, occupancy is a poor predictor of the entire range of density, especially because the variables used to predict each of the state variables are different. Thus, occupancy is likely not a good proxy for density in New Hampshire, however it could be used to track general trends through time so long as density is re-evaluated periodically.

The Cardigan pluton, located in the southern half of New Hampshire, is a strongly peraluminous, S-type granite which is granodioritic in composition. It is inferred to have been emplaced rapidly, thrust up along west-verging nappes during the Acadian orogeny. Distinctive pods, consisting of 50 to 70 percent modal garnet, are found throughout the pluton in assemblages of garnet + sillimanite + biotite + plagioclase + quartz. These garnetite rocks present an intriguing case for restite. Textural features of the garnetite rocks, such as fibrolitic sillimanite mats and flat, unzoned major and trace-element garnet grain profiles, provide evidence for biotite dehydration melting with single-stage garnet growth from the reaction: bio + plag + qtz + kspar = gar + sill + liq. Temperatures calculated using garnet-biotite (GB) thermometry and garnet-aluminum silicate-quartz-plagioclase (GASP) barometry yield estimates between 662-714ºC and 3.8 kbars. These low calculated temperatures are most likely the result of biotite compositions which have been altered by retrograde exchange reactions. The dominant source rock for the Cardigan magmas was likely calc-pelitic to greywacke in composition. Major element modeling suggests that ~70% melting of a calc-pelitic metasediment from the Central Maine trough could have generated a granodioritic melt similar to the average granodiorite of the Cardigan pluton. However, most of the Cardigan garnetite rocks appear to have been derived from pelites, as they are too poor in CaO and Na2O. Hence, though the majority of garnetite rocks cannot represent the dominant restite of the source rocks that produced the Cardigan pluton, they do appear to be the melt-depleted residue of an unidentified pelitic source. Comparison of Nd and Sr isotopic data from garnetite and Central Maine trough metasediments permit an interpretation that the Lower Rangeley Formation, from the Central Maine trough, could be the source rock of the Cardigan magmas. However, one feldspar Pb isotopic analysis in the literature (Moench and Allienikoff, 2002) and rare monazite chemical ages near 600 Ma suggest that the Cardigan pluton does not have a Laurentian source (i.e. Lower Rangeley Formation or other Central Maine trough metasediments), whereas an inferred peri-Gondwanan basement source is permissible.