Why would some migrants choose to engage in degrading work?

This paper develops a model of voluntary migration into degrading work. The essence of the model is a tension between two “bads:” that which arises from being relatively deprived at home, and that which arises from engaging in humiliating work away from home. Balancing between these two “bads” can give rise to an explicit, voluntary choice to engage in humiliating work. The paper identifies conditions under which a migrant will choose to engage in degrading work rather than being forced into it, to work abroad as a prostitute, say, rather than on a farm. The paper delineates the possible equilibria and finds that greater relative deprivation will make it more likely that the equilibrium outcome will be “engagement in prostitution.” It is shown that under well specified conditions, every individual will work as a prostitute, yet every individual would be better off working on a farm. Put differently, when specific conditions are satisfied, there is a possibility of a “coordination failure:” if individuals believe that everyone else will choose to be a prostitute, this belief will be self-fulfilling. In this case, all the individuals choose to engage in prostitution, which renders each of them worse off. The paper discusses various policy implications. It is shown that a policy intervention (a crackdown on migrants’ engagement in prostitution), if implemented strictly, can increase everyone’s welfare, but when the policy is implemented loosely, cracking down on prostitution will only reduce individuals’ welfare without reducing their engagement in prostitution.Migrants, Relative deprivation, Degrading work, Humiliation, Multiple equilibria, Welfare assessment, Policy implications, Labor and Human Capital, Political Economy, F22, J24, J81,

The Dalradian rocks of the central Grampian Highlands of Scotland

The central Grampian Highlands, as defined here, are bounded to the north-west by the Great Glen Fault, to the south-west by Loch Etive and the Pass of Brander Fault and to the south-east by the main outcrop of the Loch Tay Limestone Formation. The more arbitrary northern boundary runs north-west along the A9 road and westwards to Fort William. The detailed stratigraphy of the Dalradian Supergroup ranges from the uppermost Grampian Group through to the top of the Argyll Group, most notably seen in the two classic areas of Loch Leven–Appin and Schiehallion–Loch Tay; Southern Highland Group strata are preserved only in a small structural inlier south of Glen Lyon. Major F1 and F2 folds are complicated by co-axial northeast-trending F3 and F4 folding, as well as by locally important north- or NW-trending folds. In the Loch Leven area, nappe-like F1 folds verge to the north-west, whereas to the south-east the major recumbent F1/F2 Tay Nappe verges to the south-east. The trace of the upright Loch Awe Syncline lies between the opposing nappes, but in this region a large mass of late-Caledonian granitic rocks obscures their mutual relationship. Three tectonic ‘slides’ are identified that are certainly zones of high strain but which in part could be obscuring stratigraphical variations. The regional metamorphism ranges from greenschist facies on the western seaboard of Argyll to amphibolite facies in most of the remainder of the region. The study of garnets, together with kyanite and staurolite in the Schiehallion area, has enabled a detailed history of the metamorphism and structure to be unravelled. Stratabound mineralization occurs in the Easdale Subgroup, where there is also evidence of changes of sedimentary environment associated with volcanicity and lithospheric stretching. The region is dissected by a series of NE-trending, dominantly left-lateral, faults, subparallel to the Great Glen Fault, whose movement history is illustrated here by that of the Tyndrum Fault