Stone.

Description based on: Vol. 7, no. 1 (June 1893)

Scotland of to-day,

The evolution of the Scot.--The kirk and its story.--Education in school and college.--The law and the lawyers.--Architecture, ecclesiastical and other.--Painting and painters.--Literature.--"Edina, Scotia's darling seat."--The kingdom of Fife.--In Lothian fields.--The Lothian shore.--The city of St. Mungo.--The Clyde.--Burns and the Burns country.--The legend of the Covenant.--Yarrow and Traquair.--The Border and the Solway.--Stirling and Perth.--Dundee.--The Granite city.--A highland survey.--A note on Caithness.--Round the islands.--Sports and pastimes.--Music, old and new.--Scots food.--Scots drink.--Scots wit and humour.--The Scot abroad and the stranger in Scotland.

Lydia Mendelssohn Theater

On verso: The 1st set in the first show in Lydia Mendelssohn Theater "Granite" used about early 30's, '31 or '32

Gandy Dancer

401 Depot Street, Ann Arbor, Michigan 48104 (313) 769-0592. This magnificent 1886 Michigan Central RR depot of colorful Michigan granite now offers a glass walled trackside room, an elegant baggage scale room, the Roundhouse Saloon and some of the most romantic dining "on the line".

Vital records of Londonderry, New Hampshire; a full and accurate transcript of the births, marriage intentions, marriages and deaths in this town from the earliest date to 1910.

Printed by order of the town.

History of the town of Jefferson, New Hampshire, 1773-1927,

Mode of access: Internet.

Manchester of yesterday; a human interest story of its past,

Mode of access: Internet.

Calendar

Mode of access: Internet.

General valuation of rateable property in Ireland : valuation of the several tenements.

[1] Union: Clogher/Counties: Monaghan & Tyrone -- [2] Union: Castlerea/Counties: Roscommon & Mayo -- [3] Union: Castletowndelvin/Counties: Meath & Westmeath -- [4] Union: Cootehill/County: Cavan -- [5] Union: Clifton/County: Galway, in which is included the Island of Inishbofin in the County of Mayo -- [6] Union: Claremorris/County: Mayo -- [7] Union: Cootehill/County: Managhan -- [8] Union: Clones/(Part of) County: Monaghan -- [9] Union: Ardee/Counties: Louth & Meath -- [10] Union: Bailieborough/County: Cavan -- [11] Union: Ballina/Counties: Mayo & Sligo -- [12] Union: Ballinasloe/County: Roscommon -- [13] Union: Ballinrobe/County: Mayo -- [14] Union: Ballymahon/Counties: Longford & Westmeath -- [15] Union: Ballymahon/County: Westmeath -- [16] Union: Ballyshannon/County: Donegal -- [17] Union: Ballyshannon/County: Leitrim -- [18] Union: Ballyvaghan/County: Clare -- [19] Union: Baltinglass/County: Wicklow -- [20] Unions: Bandon & Kinsale/County: Cork -- [21] Union: Bawnboy/County: Cavan -- [22] Union: Bawnboy/County: Leitrim -- [23] Union: Belmullet/County: Mayo -- [24] Union: Carrick-on-Shannon/County: Roscommon -- [25] Union: Carrickmacross/County: Monaghan -- [26] Union: Castlebar/County: Mayo -- [27] Union: Castleblayney (part of)/County: Monaghan -- [28] Union: Corrofin/County: Clare -- [29] Barony: Upper Deece/County: Meath -- [30] Barony: Cork/County: Cork -- [31] Barony: Coshmore & Coshbride/County: Waterford -- [32] Barony: Trough/County: Monaghan -- [33] Union: Donegal/County: Donegal -- [34] Union: Drogheda/Counties: Louth & Meath -- [35] Union: Dromore, West/County: Sligo -- [36] Union: Dunfanaghy/County: Donegal -- [37] Unions: Cahersiveen, Kenmare, and Killarney/County: Kerry -- [38] Barony: Dunkerron South/County: Kerry -- [39] Union: Dunshaughlin/County: Meath -- [40] Union: Edenderry/County: Meath -- [41] Union: Edenderry/County: Kildare -- [42] Union: Edenderry/King's County -- [43] Union: Enniskillen/County: Cavan -- [44] Union: Ennistimon/County: Clare -- [45] Barony: Glenahiry/County: Waterford -- [46] Union: Gort/Counties: Galway & Clare -- [47] Union: Granard/County: Longford -- [48] Union: Granard/County: Westmeath -- [49] Barony: Iffa & Offa West/County: Tipperary -- [50] Barony: Imokilly/County: Cork -- [51] Union: Kells/County: Meath -- [52] Barony: Kenry/County: Limerick -- [53] Barony: Kerrycurrihy/County: Cork -- [54] Barony: Kilculliheen/County: Waterford -- [55] Union: Killadysert/County: Clare -- [56] Union: Killala/County: Mayo -- [57] Union: Letterkenny/County: Donegal -- [58] Union: Limerick/County: Limerick -- [59] Union: Longford/County: Longford -- [60] Barony: Magunihy/County: Kerry -- [61] Unions: Mallow & Cork/County: Cork -- [62] Union: Manorhamilton/County: Leitrim -- [63] Union: Millford/County: Donegal -- [64] Union: Mountbellew/County: Galway -- [65] Union: Naas/County: Wicklow -- [66] Union: Navan/County: Meath -- [67] Union: Newport/County: Mayo -- [68] Union: Oldcastle/County: Meath -- [69] Barony: Upper Ormond/County: Tipperary, North Riding -- [70] Barony: Orrery & Kilmore/County: Cork -- [71] Union: Oughterard/ Counties: Galway & Mayo together with that portion of the Union of Ballinrobe in the County of Galway -- [72] Union: Portumna/County: Galway -- [73] Barony: Rathdown/County: Wicklow -- [74] Barony: Salt/County: Kildare -- [75] Barony: South Salt/County: Kildare -- [76] Union: Scarriff/Counties: Clare & Galway -- [77] Union: Shillelagh/County: Wicklow -- [78] Union: Stranorlar/County: Donegal -- [79] Union: Tobercurry/County: Sligo -- [80] Union: Trim/County: Meath -- [81] Barony: Trughanacmy/County: Kerry -- [82] Barony: Upperthird/County: Waterford -- [83] Union: Wexford/County: Wexford -- [84] Barony: Castleknock/County: Dublin -- [85] Barony: Balrothery, East/County: Dublin -- [86] Barony: Newcastle/County: Dublin -- [87] City of Dublin, North Dublin Union, Arran Quay Ward -- [88] City of Dublin, South Dublin Union, Fitzwilliam Ward -- [89] City of Dublin, North Dublin Union, Inns Quay Ward -- [90] City of Dublin, South Dublin Union, Mansion House Ward -- [91] City of Dublin, South Dublin Union, Merchants' Quay Ward -- [92] City of Dublin, North Dublin Union, Mountjoy Ward -- [93] City of Dublin, North Dublin Union, North Dock Ward -- [94] City of Dublin, North Dublin Union, North City Ward -- [95] City of Dublin, North Dublin Union, Rotundo Ward -- [96] City of Dublin, South Dublin Union, Royal Exchange Ward -- [97] City of Dublin, South Dublin Union, South City Ward -- [98] City of Dublin, South Dublin Union, South Dock Ward -- [99] City of Dublin, South Dublin Union, Trinity Ward -- [100] City of Dublin, South Dublin Union, Usher's Quay Ward -- [101] City of Dublin, South Dublin Union, Wood Quay Ward.

Shoemaker impact structure, Western Australia

The Shoemaker impact structure, on the southern margin of the Palaeoproterozoic Earaheedy Basin, with an outer diameter of similar to30 km, consists of two well-defined concentric ring structures surrounding a granitoid basement uplift. The concentric structures, including a ring syncline and a ring anticline, formed in sedimentary rocks of the Earaheedy Group. In addition, aeromagnetic and geological field observations suggest that Shoemaker is a deeply eroded structure. The central 12 km-diameter uplift consists of fractured Archaean basement granitoids of syenitic composition (Teague Granite). Shock-metamorphic features include shatter cones in sedimentary rocks and planar deformation features in quartz crystals of the Teague Granite. Universal-stage analysis of 51 sets of planar deformation features in 18 quartz grains indicate dominance of sets parallel to omega (10 (1) over bar3}, but absence of sets parallel to pi (10 (1) over bar2}, implying peak shock pressures in the range of 10-20 GPa for the analysed sample. Geophysical characteristics of the structure include a -100 mus(-2) gravity anomaly coincident with the central uplift and positive circular trends in both magnetic and gravity correlating with the inner ring syncline and outer ring anticline. The Teague Granite is dominated by albite-quartz-K-feldspar with subordinate amounts of alkali pyroxene. The alkali-rich syenitic composition suggests it could either represent a member of the Late Archaean plutonic suite or the product of alkali metasomatism related to impact-generated hydrothermal activity. In places, the Teague Granite exhibits partial to pervasive silicification and contains hydrothermal minerals, including amphibole, garnet, sericite and prehnite. Recent isotopic age studies of the Teague Granite suggest an older age limit of ca 1300 Ma (Ar-Ar on K-feldspar) and a younger age limit of ca 568 Ma (K-Ar on illite-smectite). The significance of the K-Ar age of 568 Ma is not clear, and it might represent either hydrothermal activity triggered by impact-related energy or a possible resetting by tectonothermal events in the region.

Diplacanthid acanthodians from the Aztec Siltstone (late Middle Devonian) of southern Victoria Land, Antartica

One articulated and several partial, semi-articulated specimens of acanthodians were collected in 1970 from the freshwater deposits of the Aztec Siltstone (Middle Devonian; Givetian), Portal Mountain, southern Victoria Land, Antarctica, during a Victoria University of Wellington Antarctic Expedition. The Portal Mountain fish fauna, preserved in a finely laminated, non-calcareous siltstone, includes acanthodians, palaeoniscoids, and bothriolepid placoderms. The articulated acanthodian specimens are the most complete fossil fish remains documented so far from the Aztec assemblage, which is the most diverse fossil vertebrate fauna known from Antarctica. They are described as a new taxon, Milesacanthus antarctica gen. et sp. nov., which is assigned to the family Diplacanthidae. Its fin spines show some similarities to spine fragments named Byssacanthoides debenhami from glacial moraine at Granite Harbour, Antarctica, and much larger spines named Antarctonchus glacialis from outcrops of the Aztec Siltstone in the Boomerang Range, southern Victoria Land. Both of these are reviewed, and retained as form taxa for isolated spines. Various isolated remains of fin spines and scales are described from Portal Mountain and Mount Crean (Lashly Range), and referred to Milesacanthus antarctica gen. et sp. nov. The histology of spines and scales is documented for the first time, and compared with acanthodian material from the Devonian of Australia and Europe. Distinctive fin spines from Mount Crean are provisionally assigned to Culmacanthus antarctica Young, 1989b. Several features on the most complete of the new fish specimens - in particular, the apparent lack of an enlarged cheek plate - suggest a revision of the diagnosis for the Diplacanthidae.

A new species of Glaphyromorphus (Reptilia : Scincidae) from Mt Elliot, north-eastern Queensland

Glaphyromorphus clandestinus, sp. nov., is described from granite-slab habitat on Mt Elliot, north-eastern Queensland. This species can be distinguished from its congeners by a combination of the following characters: large size (SVL 72 mm), adpressed limbs of adult separated by noticeably more than the length of the forelimb, 26 mid-body scale rows, and flanks patterned with dark flecks forming a series of longitudinal lines. The distribution, habitat preferences and habits of this species are poorly known. Currently G. clandestinus is known from a single locality where individuals have been found in an exposed area of exfoliating granite, set in a mosaic of rainforest and eucalyptus woodland. The discovery of this species brings to three the number of vertebrate species known to be endemic to Mt Elliot and highlights the evolutionary significance of this southerly outlier to the mountainous rainforest of the Wet Tropics.

The igneous charnockite—high-K alkali-calcic I-type granite—incipient charnockite association in Trivandrum Block, southern India

The Pan-African (640 Ma) Chengannoor granite intrudes the NW margin of the Neoproterozoic high-grade metamorphic terrain of the Trivandrum Block (TB), southern India, and is spatially associated with the Cardamom hills igneous charnockite massif (CM). Geochemical features characterize the Chengannoor granite as high-K alkali-calcic I-type granite. Within the constraints imposed by the high temperature, anhydrous, K-rich nature of the magmas, comparison with recent experimental studies on various granitold source compositions, and trace- and rare-earth-element modelling, the distinctive features of the Chengannoor granite reflect a source rock of igneous charnockitic nature. A petrogenetic model is proposed whereby there was a period of basaltic underplating; the partial melting of this basaltic lower crust formed the CM charnockites. The Chengannoor granite was produced by the partial melting of the charnoenderbites from the CM, with subsequent fractionation dominated by feldspars. In a regional context, the Chengannoor I-type granite is considered as a possible heat source for the near-UHT nature of metamorphism in the northern part of the TB. This is different from previous studies, which favoured CM charnockite as the major heat source. The Occurrence of incipient charnockites (both large scale as well as small scale) adjacent to the granite as well as pegmatites (which contain CO2, CO2-H2O, F and other volatiles), suggests that the fluids expelled from the alkaline magma upon solidification generated incipient charnockites through fluid-induced lowering of water activity. Thus the granite and associated alkaline pegmatites acted as conduits for the transfer of heat and volatiles in the Achankovil Shear Zone area, causing pervasive as well as patchy charnockite formation. The transport Of CO2 by felsic melts through the southern Indian middle crust is suggested to be part of a crustal-scale fluid system that linked mantle heat and CO2 input with upward migration of crustally derived felsic melts and incipient charnockite formation, resulting in an igneous charnockite - I-type granite - incipient charnockite association.

Influence of explosive energy on the strength of the rock fragments and SAG mill throughput

Extensive in-situ testings has shown that blast fragmentation influences the performance of downstream processes in a mine, and as a consequence, the profit of the whole operation can be greatly improved through optimised fragmentation. Other unit operations like excavation, crushing and grinding can all be assisted by altering the blast-induced fragmentation. Experimental studies have indicated that a change in blasting practice would not only influence fragmentation but fragment strength as well. The strength of the fragments produced in a blast is clearly important to the performance of the crushing and grinding circuit as it affects the energy required to break the feed to a target product size. In order to validate the effect of blasting on fragment strength several lumps of granite were blasted, under controlled conditions, using three very different explosive products. The resulting fragments were subjected to standard comminution ore characterisation tests. Obtained comminution parameters were then used to simulate the performance of a SAG mill. Modelling results indicate that changes in post blast residual rock fragment strength significantly influences the performance of the SAG mill, producing up to a 20% increase in throughput. (c) 2004 Elsevier Ltd. All rights reserved.

A trace element study of siderite-jasper banded iron formation in the 3.45 Ga Warrawoona Group, Pilbara Craton - Formation from hydrothermal fluids and shallow seawater

Shale-normalised rare earth element and yttrium (REE + Y) patterns for siderite-jasper couples in a banded iron formation of the 3.45 Ga Panorama Formation, Warrawoona Group, eastern Pilbara Craton, display distinct positive Y and Eu anomalies and weak positive La and Gd anomalies, combined with depleted light REE relative to middle and heavy REE. Ambient seawater and hydrothermal fluids are identified as major sources of REE + Y for the BIF. In the case of siderites, strong correlations between incompatible trace elements and trace element ratios diagnostic of seawater indicate variable input from a terrigenous source (e.g. volcanic ash). We propose a volcanic caldera setting as a likely depositional environment where jasper and siderite precipitated as alternating bands in response to episodic changes in ambient water chemistry. The episodicity was either driven by fluctuations in the intensity of hydrothermal activity or changes in magma chamber activity, which in turn controlled relative sea level. In this context, precipitation of jasper probably reflects background conditions during which seawater was saturated in silica due to evaporative conditions, while siderites were deposited most likely during intermittent periods of enhanced volcanic activity when seawater was more acidic due to the release of exhalative phases (e.g. CO2). © 2005 Elsevier B.V. All rights reserved.