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Staff Profile
Associate Professor Antje Schuhmann
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Antje Schuhmann is an Associate Professor in the Political Studies Department and associated to the WITS Centre for Diversity Studies. She is the strategic partner to Berlin Humboldt University in Germany, Chair for Diversity and Social Conflict, which entails research cooperation and student exchange.
She holds a PhD in Postcolonial Studies (and a MA in American Cultural History/ Literature Theory/Social Psychology) from Ludwig-Maximilian's University Munich (Germany).
She worked internationally: America Institute at Ludwig-Maximilian's University Munich (Germany), the American and Black Studies and English-Speaking Cultures Department of the University of Bremen (Germany), at the University Paris 7 (France) and University of Orleans (France), before she was appointed at University of the Witwatersrand. Antje Schuhmann is active in international feminist and anti-racist networks and initiatives. She is the co-editor of Blackness and Sexualities (2007) and of Gaze Regimes. Film and Feminisms in Africa (2015), has produced film and audio features and publishes in various academic and non-academic journals and newspapers.
Research interests:
- Feminist Theories & Methodologies
- Gender based violence
- Critical Diversity Studies, special focus on intersections of race, gender, class, sexuality – Politics of Othering and Normativity)
- Body & Identity Politics including Queer Theory (the body and discourses about gendered, racialised, and sexualized bodies in political thought and social practices, homophobia, hate crimes) and Sexuality Studies (from LTGBI history and movements to deconstruction/strategic essentialism, two –sex system)
- Postcolonial Theory (European und US-American Migration/Refugee-Movements, Orientalism, Anti-racist/xenophobic Theories and Movements)
- Memory Politics (German National Socialism, Shoah/Holocaust, German Genocide in Namibia, links between colonialism and today's forms of racism, decolonization)
- Critical Race Theory
- Critical Theory (Frankfurt School) and Political Protest/Movements (Politics of transgression and subversion and/or oppositional politics)
- Critical Pedagogy, Transdisciplinarity and Mathetics for diverse Classrooms
How do gender, race, sexuality, and class manifest in everyday experiences and politics of representation? How are the ways we memorize past violence subverting or reinforcing contemporary forms of oppression? The intersections of power with body politics, and their historic legacies within today's systems of violence and domination are one of the main foci of her intellectual and political work.
Antje Schuhmann's transdisciplinary intellectual project is rooted in poststructuralist theory production, especially in relation to the analysis of intersectionality as practiced within Gender Studies, Critical Race Theory, Postcolonial Feminist and Queer Studies. Her work is inspired by Critical Theory as developed by the scholars of the German Frankfurt School/New School NY, traversing German Philosophy with Social Psychology and applying psychoanalytic concepts when interpreting socio-political and cultural phenomena such as regimes of violence, politics of othering, identity and belonging such as racism, sexism, homophobia, xenophobia et.al..
She was awarded the WITS Faculty of Humanities Postgraduate Teaching Award. Her teaching practice is inclusive, horizontal, interactive and transdisciplinary.


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iAquaLink 4+
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Ratings and Reviews
Complete garbage, paid over $2k to get this system installed by my pool
Engineer and the web interface never loads, therefore I cannot change the times the pool filter and heat runs, the app looks like something from the 1990's, total disgrace, this company should be embarrassed.
Simple to set up the wifi and it works
Ideal to manage the pool - particularly for those times you forgot to turn off the lights, or the heating whilst on holiday...
Also, as long as every system is zodiac, you can see everything about the pool in one place making management of it simple.
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- © 2017 Zodiac Pool Systems, Inc.
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Family Sharing
Up to six family members will be able to use this app with Family Sharing enabled.

subset: commoncrawl


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New York City and Texas may seem like worlds apart but apparently everything's bigger in the Big Apple. For over a decade, New York City has saluted the Lone Star State by celebrating Texas Independence Day.
In 2019, Texas country acts Pat Green and Eli Young Band--along with fellow Texans Aaron Watson and Kyle Park--are set to return to New York City for the 11th annual Texas Independence Day celebration at Terminal 5 on March 2, Texas Independence Day propper. You can find tickets on AXS to New York City's 11th Annual Salute To Texas Independence Day by following this link.
Hailing from San Antonio, Pat Green is a household name acoross the length and breadth of the Lone Star State but grabbed national attention with his 2003 song "Wave on Wave," which hit #3 on the Billboard Hot Country Songs chart. Green's latest studio album, Home, arrived in 2015.
Since their formation in the Texas music mecca of Denton, Eli Young Band have had three singles hit #1 on the Billboard Country chart. Eli Young Band released their sixth LP, Fingerprints, in 2017.
Don't miss your chance to catch Pat Green, Eli Young Band, Aaron Watson and Kyle Park when they come to Terminal 5 on March 2 to celebrate Texas Independence Day.


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Scott Laplant Proves .puter Guys Do Not Have To Be Geeks-www.xxsy.net
Hardware Who says that .puter guys have to be geeks? Not Scott Laplant. Although he is a respected network engineer who has been recognized by his colleagues and employers for the excellence of his work, Scott also lives a full life when he is not sitting in front of a .puter terminal. How many .puter engineers do you know who are active in various sports activities as well as being involved in charity work? Truly, Scott strives to find balance in both his work and personal life, and his range of interests in reflected in the strong online presence he maintains. The blog that he maintains on his personal website reveals some of these interests. His recent posts are on topics as varied as unsolicited credit card offers, the importance of exercising your right of suffrage, why we should set big goals for ourselves and the importance of getting back to the basics such as .mon decency and doing the right thing even if it represents an inconvenience for us. Many of these posts also include a lot of useful information that visitors can use, as well as links that they can click on to learn more about the topics Scott discusses in his posts. In his blog, Swell Chap that Loves Linux, he shares some Linux love with his readers. It is well known that Scott is a supporter of the Ubuntu operating system, based on Linux, and his latest blog posts on this site are about the security vulnerabilities of the latest Ubuntu releases. The posts give useful advice on how to address these vulnerabilities by upgrading your system to the re.mended package versions listed. Yes, it is a highly technical blog, but one filled with practical tips and information for the techie guys out there. This site is truly worthy of a guy who is an active member of the Central Pennsylvania Linux User Group (CPLUG). But he is not just a .puter geek and a blogger; he is also an outdoorsy guy who lists biking and cross-country skiing as among his leisure activities. These interests are reflected in his blog, which offers a wealth of information on outdoor and camping activities. The most recent posts on the site include quizzes on how to indentify .mon wild plants that you can find in the woods and articles on medicinal uses of wild plants and trees, as well as announcements of up.ing activities that campers and hikers might be interested in signing up for, such as the Gone Fishin, Not Just Wishing Event which was held last May, and developments of interest such as the vote of the Atlantic States Marine Fisheries .mission to give member states the option to extend the 2010 black sea bass season by 90 days. Outside of his online presence, Scott Laplant is also actively involved with groups such as Big Brother Big Sister, the Special Olympics and the Milagro House in Lancaster. His work with these .anizations highlights his determination to give back to his adopted hometown of Elizabethtown, Pennsylvania. About the Author: 相关的主题文章:
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- 广州戈澜服装有限公司档案企业资质证书中国服装网-19ise.com


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Cases where you loved a figure but hated the character, and vice versa...
Surely I can't be the only one that experiences this!
Have you ever been in a situation where you liked the look and feel of a toy, but disliked the character it represented? OR You hated a toy but desperately wanted to like it because you liked the character?
For me, I have a tendency to collect G1 Starscream toys when they come out. But upon some recent introspection, I realised that I don't actually like the Starscream character as much as I thought I did. As a child, I liked the idea and look of Transformers that turned into jets more than I liked car alt-modes. I also liked the white, blue and red colour scheme. Upon discovering a G1 Starscream toy, I picked him as a favourite character without knowing much about him (the first Transformers fiction I watched didn't have Starscream in it). To this day I still like the aesthetic design of Starscream, but personality/character-wise, I find him hard to root for. If there was blue, red and white (or gray) jet with the personality of Optimus Prime, hed be the perfect character for me. Thats an example of me liking a toy while disliking the character.
On the flipside, there are many instances when I liked the character, but didnt like the toy because it didnt line up with my aesthetic preferences. An example is the Marvel Legends Vintage Wolverine. Im a big Wolverine fan, but Im not fond of the mould Hasbro used for the ML Vintage figure. To me the neck looks too long for my liking and the legs are a bit short. It looks a bit dwarf-like. Its not bad, and its accurate to the comics; but I like my action figures to look tall and heroic.
Another example (TF-related this time) is the Cyberverse figures. I like G1 Optimus Prime and Megatrons characters and their aesthetic designs, but the Cyberverse figures (G1 inspired) dont do it for me.
Yeah, I know. Im being really REALLY superficial. But the way I see it, these are toys that are made to be objectified
Dislike toys, like character: CHEETOR (BM) - Cheetor is by far the best written character in Beast Machines... which isn't hard. But seriously, even on his own merit, Cheetor is well written. His character arc is a natural continuation from Beast Wars and progresses well throughout BM. The original Mega and Supreme Class figures are rubbish. Night Slash Cheetor is nice though.
Dislike character, like toy - HUBCAP (G1). Of course, he's meant to be an unlikeable characters
Both: WHEELIE (G1) - dislike the G1 toy and dislike the G1 cartoon character. However I don't dislike Wheelie in other G1 continuities beyond the cartoon, and I quite like Titans Return Wheelie.
I love you 3000
For Sale: AOE Optimus Prime, Universe Darkwing, Retro Vol 2 and more!
Transformers collection: 2313
Mine was Sunstreaker. Loved his IDW incarnation (despite the rockiness during All Hail Megatron), but the Generations toy.... I dunno he just never sat right with me. I actually gave him away before I left my old job to a friend as a keepsake.
Transmutate - absolutely terrible even as a pack-in build-a-figure. But luuuuurv the character and what she represents.
I love you 3000
For Sale: AOE Optimus Prime, Universe Darkwing, Retro Vol 2 and more!
Transformers collection: 2313
I buy figures because I like the character.
It's less about the toy. If the toy is rubbish, then I'll happily leave it sealed.
Sadly, I like a lot of unrepresented characters, disliking a lot of the popular ones. That said, I don't think I dislike any character enough to negatively impact my enjoyment of a figure, I just wouldn't buy more than the one or two figures I'd need to represent that character.
And man o man am I sick of Optimus Prime.
Some company gets the license for Transformers, they make a Prime, I buy it to support the line, they stop making their product.... rinse, repeat and my collection starts to look more like an Optimus Prime collection and less of a Transformers collection.
*Gazes over collection trying to find familiarity*
"Is that Optimus Prime? He looks a bit weird"
"No actually thats God Ginrai, he's a Japanese character. He only looks like Optimus Prime."
*Eyes glaze over*
"Oh right, yeah, uh huh....."
A lot of characters from RID(01), S4 of the G1 cartoon and a lot of characters from the Unicron Trilogy I did not like one bit but enjoyed the toys. I'm don't think there has ever been a character I've ever hated enough to make me bypass a toy I wanted, though a lot from ROTF like the twins came damn close
I am guilty of buying the odd toy that wasn't much good just because I wanted a representation of the character.
Not having the TF-budget I used to have makes it easier. If its a character I don't like, and most definitely a toy I don't like, I'll just bypass it now. And as others have stated, there are characters I just bypass completely as I have so many already - I've got over 100 different Optimus, I don't need anymore
Join the Trevolution!
Follow on FB: BigAngryTrev Twitter: @BigAngryTrev and Tumblr: BigAngryTrev!
Toy Reviews: Studio Series Scrapmetal
Articles: TCG Devastator Pack Review Part 1 and Part 2
A couple more examples of toys that I liked, but didn't like the characters (or was just plain indifferent); lots of Beast Wars characters. When they were first released, outside their tech spec bios, there was little to no supporting fiction for Terrorsaur and Razorbeast (who was basically a pig) and yet I still looovved their toys. Even after the cartoon came out, Terrorsaur did nothing on the show to really wow me, but I still enjoyed fiddling with the toy.
Example of liking the character but hating the toy; RiD Prime Knock Out (Deluxe). Knock Out was my favourite character from TF Prime, but his deluxe toy was lacking. It looked like it'd been painted by a crack addict (I ended up buying the reprolabels set to make his look more palatable), the transformation was a pain, and the robot mode was flimsy. I like TFP Knock Out, but can't really say the same for that deluxe. I hope Hasbro revisits the character in Generations and gives him a better toy.
While we're on TFP, while I felt that Breakdown never got a whole bunch of screentime to flesh the character out (so never really stuck with me as a favourite), boy oh boy his toy looked appealing. Curse you, Takara!
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Walking tour for the Harding pegmatite mine
Regional geological map, Road map
Walking tour for the Harding pegmatite mine
Stop 2: (Quartz knoll and prospect pit on East Ridge)
Stop 3: (Quartz knoll at east end of quarry)
Stop 4: (Bench at east end of quarry)
Stop 5: ("Spotted rock" face, west end of quarry)
Stop6: (North wall of west entry way to quarry, north of Stop 5)
Stop 7: (Road-cut in access road)
Stop 1: (Top of North Knob)
Pegmatites are widespread magmatic rocks that form confined bodies of various shapes and sizes. Pegmatite magmas are volatile rich fractions derived from other magmas, commonly a crystallizing granitic pluton. The derivative magma, or pegmatite magma, is enriched with volatiles and because of density differences these bodies of magma can travel large distances from the parent magma. Often no parent magma is readily apparent for a pegmatite district; that is the case here. When a pegmatite magma reaches temperature and pressure conditions that allow it to crystallize, the isolated body begins cooling from the walls inward. Fractional crystallization proceeds with incomplete reaction between early-formed crystals and the remaining melt. This process enriches the liquid with volatiles, of which water is the most important. Sequential crystallization of minerals forms distinct lithologic units in the consolidated pegmatite body. These zones sub-parallel the contact of the pegmatite with the surrounding country rock. During the final stages of crystallization, the liquid becomes highly corrosive. The liquid at this stage can often replace previously consolidated pegmatite. Mineral replacement (pseudomorphism) and replacement bodies are common. During all stages of crystallization the liquid can fill fractures in consolidated pegmatite or escape into the country rock. Zones, replacement bodies and fracture fillings are the three types of lithologic units that are found in many complex pegmatites. Pegmatite magmas crystallize at a depth of 4-10 kilometers in the crust.
The Harding pegmatites intrude a complex terrane of Precambrian metamorphic rocks. The pegmatites were emplaced approximately 1330 m.y.B.P. along a complicated boundary between amphibolite to the south and quartz-muscovite schists to the north. Several generations of granitic plutons intrude the area, Cerro De Los Arboles (to the SW), Cerro De La Cruz (to the S) and Cerro Alto (to the E). No genetic link between any of the plutons and the pegmatites has been established. Most of the pegmatite bodies are lensate dikes ranging from a few meters in exposed length to as much as 350 meters. All are granitic in composition. Some are completely homogeneous and others display internal zoning, replacement bodies and fracture fillings. The main dike, which we shall refer to as the Harding pegmatite, strikes along the East Ridge in the form of a large flat disk. The thickness varies from 1 meter in areas to the east to as much as 25 meters in the quarry. The dike dips gently (10° to 15°) to the south. Looking toward the quarry, we can see the exposed thickness of the western portion of the main dike. The hanging wall contact between the overlying amphibolite (dark colored) and the pegmatite (light colored) is clearly visible. The foot wall contact with the underlying schists is exposed for a short distance in the main entry way to the quarry. We are standing on a dip slope remnant of the dike. Pegmatite is exposed on much of the south slope of North Knob. The eastern extensions of the dike are complicated by pinching, swelling and branching. The down plunge portions of the dike in the western part are known from extensive core drilling done by the U. S. Bureau of Mines in 1943 and 1948. This exploratory work extends the down plunge portions of the dike for 500 meters. The up plunge portions of the dike, beyond where we are standing, have been eroded away. Eight lithologic units can be distinguished in the main dike. These include continuous zones and discontinuous replacement bodies, but not fracture fillings. The main dike is disk-shaped so that zones appear as layers across the quarry face. The layered appearance is enhanced by the asymmetric zoning. The zones comprising the footwall are not the same as those in the hanging wall. The internal structure is best exposed in the main quarry, but first we will examine exposures along the East Ridge.
Because pegmatite magmas are volatile fractions, they host a unique and unusual collection of elements. The conditions of crystallization allow these elements to form minerals that are rare in other rocks and crystals that are gigantic in size. Many of the world's largest crystals are found in pegmatites. The Harding pegmatite is no exception. About 50 minerals occur in the main dike. This number is not astounding; some pegmatites in New England have over 100 different mineral species. The Harding is famous as the world's largest deposit of microlite, a complex tantalum oxide. The bulk the dike is composed of six major minerals: quartz [SiO2], albite [NaAlSi3O8], microcline [KAlSi3O8], muscovite [KAl2(AlSi3)O10(OH)2], lepidolite [K(Li,Al)3(Si,Al)4O10(F,OH)2], and spodumene [LiAlSi2O6]. The four principal accessory minerals are beryl [Be3Al2Si6O18], garnet [(Mn,Fe)3Al2(SiO4)3], microlite [(Na,Ca,U)2(Ta,Nb)2O6(OH,F)] and tantalite-columbite [(Fe,Mn)(Ta,Nb)2O6].
Stop 2: (Quartz knoll and prospect pit on East Ridge)
We have just traced the strike of the upper contact of the pegmatite with the country rock. Here we stand on a quartz outcrop. This is part of a continuous zone composed almost entirely of quartz, the quartz zone. This zone is a few centimeters thick to as much as several meters thick in the down plunge portions of the western part of the main dike. At the prospect pit rim you are standing on the hanging wall contact of the pegmatite; the country rock has been eroded away. The pegmatite body dips to the south. Beneath your feet you will see three units. An upper thin continuous band a few centimeters thick composed of a relatively fine-grained aggregate of quartz, albite and muscovite forms the border rind. Underlying this think band is another layer composed of slightly coarser aggregate of the same minerals. Several accessory minerals not seen here are locally abundant. They include microcline, apatite, lepidolite, tantalite-columbite and beryl. In the thick western portions of the dike, beryl frequently forms immense anhedral crystals with dimensions measured in meters. This border rind and wall zone are collectively known as the berry zone. Beneath the berry zone, we encounter a cleavelandite layer. Cleavelandite is a variety of albite, a sodium plagioclase feldspar. Here we see typical examples; the cleavelandite forms radiating aggregates of lusterous white or cream colored curving plates. This cleavelandite unit, composed almost entirely of cleavelandite, is a distinct lithologic unit. The unit forms discontinuous masses throughout the dike. Beneath the cleavelandite unit, we see a new assemblage of minerals. The long white blades or laths are spodumene; the matrix is quartz. This unit is the quartz-lath spodumene zone. Spodumene is a lithium pyroxene found exclusively in granitic pegmatites. These white elongate crystals are typical. When unaltered, they frequently are here, spodumene displays two good cleavages parallel to the length of the crystal. We have now seen four of the eight lithologic units comprising the dike. The three zones, the beryl zone, the quartz zone and the quartz-lath spodumene zone, form the upper portions of the dike; the cleavelandite unit is more often in the core of the pegmatite.
If we visualize the crystallizing pegmatite magma, the border rind in contact with the cooler country rock is the first to crystallize. Its fine-grained texture is typical of a chilled margin. Quartz crystallizes next, not all the quartz in the magma, just a zone of quartz. Many minerals will occur in several units. As crystallization continues we expect to see an increase in crystal size toward the center of the dike. In general, and in this outcrop, this is observed. The late stage liquid may, however, replace zones of consolidated pegmatite and disrupt this trend.
Stop 3: (Quartz knoll at east end of quarry)
We have just walked down part of the dip slope remnant of pegmatite blanketing North Knob. By the repeated appearance of pegmatite and country rock down the slope you begin to appreciate that the external morphology of the dike is very complicated. The contacts are not smooth, gently curving surfaces. The dike is a disk only in generalized form.
Again we are standing on the quartz zone. From under our feet the quartz zone can be traced onto the quarry face where it is much thinner. The beryl zone is above and the quartz zone is below, a similar sequence of units observed at Stop 2. The hanging wall contact is abrupt and discordant. Reaction between country rock and pegmatite is minimal.
A different unit, forming the shelf directly in front of us and the two knolls in the quarry, lies beneath the quartz-lath spodumene zone. This lithologic unit is composed of an even-grained aggregate of microcline, spodumene and quartz with lepidolite, lithium muscovite and albite. The texture of this unit, "spotted rock," is markedly less coarse than overlying zones and displays abundant mineral replacement. "Spotted rock" forms a lobe extending down the center of the dike. Its maximum breadth is exposed in the quarry, extending form the east to the west end. "Spotted rock" contains numerous accessory minerals, such as apatite, microlite, tantalite-columbite and spessartine.
The mining operations as seen form here appear to be irregular and haphazard. This is due to the primitive mining techniques (small crew and mule) and the several episodes of mining. Quartz outcrops, similar to what we are standing on, first attracted prospectors in search of gold. Lepidolite, a lithium mica, was found instead and used in the glass industry. Joseph Peyer mined the lepidolite from 1919 until 1930. The quarry was excavated and the main adit, a southward extension of the main entry way, was driven. The next episode of mining, 1942-1947, produced the world's largest production of microlite, an unusual ore of niobium and tantalum. 10,000 kilograms of microlite concentrate containing an average of 68% Ta2O5 and 7%Nb2O5 were produced. During this period the quarry was enlarged and three adits on the east side of the main adit were driven. The last episode of mining, 1950-1958, produced great quantities of beryl, a beryllium cyclosilicate. Three adits to the west were driven along the hanging wall contact where large masses of beryl were encountered. The Harding mine was the country's leading beryl producer in 1950 and 1951. Annual beryl production during the peak years exceeded 13,000 kilograms. Total beryl production during this period was 622,000 kilograms of ore containing 11.2% BeO and 167,000 kilograms containing 5.5% BeO. The underground working are very DANGEROUS. DO NOT ENTER ANY OF THE UNDERGROUND WORKINGS.
Stop 4: (Bench at east end of quarry)
Here we see the effect of a late stage residual liquid reaction with the consolidated quartz-lath spodumene zone. Laths of spodumene are replaced by fine scales of rose muscovite. The shapes of the laths are still recognizable (pseudomorphs), but in other areas the spodumene crystal form is obliterated. Cleavelandite replaces the quartz matrix. This replacement unit forms discontinuous masses throughout the core of the dike. The aggregate of rose muscovite-cleavelandite is another of the eight lithologic units. It is evident that replacement units often transect other zones and do not necessarily parallel the contacts between primary zones. At this time, most of the pegmatite magma has crystallized and very small amounts of residual liquid can cause extensive replacement by reaction with previously consolidated zones, as in the "spotted rock" unit.
Stop 5: ("Spotted rock" face, west end of quarry)
The top of this pinnacles is the hanging wall contact. The country rock has been removed. We see zones as layers: the beryl zone (top), the quartz zone (middle) and the "spotted rock" (bottom). Note the absence of the quartz-lath spodumene zone. You can see how the "spotted rock gets its name. The white "eyes" are spodumene; the matrix is mostly microcline so impregnated with lepidolite and lithium muscovites that it is pink. "spotted rock" locally grades into masses of pure lepidolite. Many of these lepidolite masses have been mined out. Lepidolite is characterized by compact, finely crystalline, lilac to purple masses or by curving platelets in quartz or cleavelandite. Often it is impossible to distinguish lepidolite from rose muscovite, but in general the rose muscovite is more red than purple in color, and it does not form large masses like the lepidolite. The dark glassy specks in the "spotted rock" are uranium rich microlite crystals. Microlite is common throughout the "spotted rock," but the economic occurrences are found at the base of the quartz-lath spodumene zone. There the microlite is lighter in color and in dense aggregates of tiny crystals.
Another mineral difficult to identify is beryl. Here a mass is exposed in the wall zone. All the beryl is white to light pink in color and almost always without crystal form. The masses resemble quartz and feldspar. The beryl has a resinous or greasy luster and often a basal cleavage that distinguishes it from quartz and feldspar. The beryl mass in the wall zone displays a broad flat cleavage surface.
Stop6: (North wall of west entry way to quarry, north of Stop 5)
The replacement of microcline by micas in the "spotted rock" masks the original character of that zone. Exposed in the north wall of the west entry way are masses of perthitic microcline that are not replaced. Microcline is a potassium feldspar that forms large blocky crystals in pegmatites. The mineral displays two good cleavages at approximately right angles. The color ranges from white to tan. Perthite is an intergrowth of potassium and sodium feldspar. All the microcline is perthitic. This perthitic microcline unit is another of the eight lithologic units. This zone occupies much of the lower portions of the dike. We have now seen seven units. Keep in mind that as the pegmatite magma was crystallizing, zones were forming simultaneously in both the top and bottom of dike.
Stop 7: (Road-cut in access road)
In passing through the main entry way we have walked past the footwall contact of the dike with the underlying schist. Here the footwall contact is also exposed on part of the dip slope remnant that rests on North Knob. The lower contact is sharp and discordant. We can trace this contact to the basal contact exposed in the main entry way by a curved plane. The basal unit here is a mixture of the perthite zone (as seen at last stop) and aplite. The aplite zone here is composed of fine-grained albite and forms large continuous units in the base of the dike. The aplite zone constitutes another lithologic unit. The eight lithologic units are: the beryl zone, the quartz zone and the quartz-lath spodumene zone comprising the top portions; the "spotted rock," rose muscovite-cleavelandite, and cleavelandite units, all interior units; and the perthite zone and the aplite zone forming the bottom of the dike. Keep in mind these lithologic units are generalized. They do exist, but gradations between units are common. When looking at an exposure it is not always possible to identify the unit, especially in the eastern extensions.
As pegmatite magmas crystallize the rest liquid is enriched in volatiles, so we should see a specific paragenesis of mineral chemistry reflecting the changing composition of the melt. More volatile rich minerals should occur in the interior portions of the pegmatite body. This is not apparent with ubiquitous minerals like quartz and feldspars, but is better displayed by the rarer minerals. For example, the micas here have the following paragenesis: green muscovite (in the wall zones), then lepidolite (interior units), and finally rose muscovites (interior units). Trace element chemistries in nearly all the minerals reflect the volatile enrichment.
Walking tour designed by Bryan Chakoumakos.


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Annual financial statements are necessary
As an independent business, you know that recurring tasks such as annual financial statements and tax returns can take many hours out of a busy schedule. We are experienced accounting consultants and help over 750 small businesses with their annual financial statements and tax returns.
The annual accounts help you get an overview of all income and expenditure in your business, creating insight on the direction in which your business is going. At the same time, as an independent business you must ensure that you have the necessary documentation for the Danish Customs and Tax Administration.
When you run your own business, under the Danish Financial Statements Act you are obliged, as a minimum, to prepare annual accounts that show your financial activities during the year. Additionally, you may use your annual financial statements as documentation in dealings with banks, credit institutions and partners.
Preparation of annual financial statements and tax returns
For the preparation of annual financial statements and tax returns in a personally owned business, we have an indicative price of DKK 5,200 excl. VAT.
For partnerships, there is an additional fee per partner of DKK 550 excl. VAT.
The price assumes that the material we receive is balanced and divided into proper accounting periods, and that the received annexes are complete.
In connection with start-ups, the following is also required:
- Acces to finance system
- Company reg. no. and E-tax code
- Civil reg. no. and E-tax code
In order to perform the task on a recurring basis, the following is needed each time:
- Bank statements for the full period in paper form and, ideally, in an Excel file (CSV format)
- Income receipts for the full period
- Expense receipts for the full period
What do customers say about our accountants
What are annual financial statements?
As the name indicates, annual financial statements have to be prepared once per year. The annual financial statements are where it is possible to see how the year has been overall for your business. The annual financial statements have two main parts: 1) the income statement, which tells how your company's financial resources has been used during the year and 2) the balance sheet, which provides a snapshot of how your company's finances are doing.
If you need help with your annual financial statements, we have a whole team ready to help you. So you can be 100% sure that they are prepared properly from start to finish.
What is a tax return?
As a self-employed person running a business, you are required to fill out a tax return (or, to give it its proper name, an extended tax return). In the tax return, you inform the Danish Customs and Tax Administration how much you have earned, how much you have to pay in tax, what allowances you have, etc. The tax return can be completed electronically via E-tax at skat.dk.
If you are unsure whether you have taken advantage of all your allowances or whether your tax return is filled out correctly, you can get tax return assistance from us. Our professional knowledge and experience is your guarantee that you make optimal use of all your allowances and file a correct tax return.
In Zealand, Funen and Jutland.
Whether you live in or around Odense, Fredericia or Copenhagen, we can help you.
We have offices in these three cities, and therefore cover an area near you. All our offices are easily accessible by public transport, and there is ample free parking right by the door. You are always welcome to drop in for an informal chat.
Azets in Herlev
+45 32 96 80 37
Azets in Odense
+45 32 96 80 37
Azets in Fredericia
70 23 31 30
Want more information?
You are always welcome to give us a call. If you want us to contact you, fill in the form and we will contact you as soon as possible.
+45 44 51 81 80


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20% of adolescents may experience a mental health problem in any given year
20% of adolescents may experience a mental health problem in any given year
50% of mental health problems are established by age 14
10% of children and young people (aged 5-16 years) have a clinically diagnosable mental problem
yet 70% of children and adolescents who experience mental health problems have not had appropriate interventions
Neuroscience is the study of the nervous system, mainly the brain, where most of the nervous system activity takes place. It shows how the nervous system develops, its structure, and what it does. As we know, our brains did not evolve to enable us to cope with many of the demands and requirements of modern life, and yet amazingly, we do! If your brain is not working well, you may struggle with many details of life – in effect battling with your own brain.
Although a scientific understanding of how the brain has changed by educational interventions is only now merging, it is likely to help contribute to the future of teacher education and the development of educational policies in the 21st Century.
This area of research work is developing at a pace and there is a growing emphasis and evidence on the ability of our minds to change, adapt and develop to the world around us. In terms of learning and the way we learn, this has massive implications. It simple terms in means we have significant influence over what and how we think, how this can affect our total life experience. Work of this type in schools has shown to improve behaviour, learning, emotional literacy, mental health and OFSTED ratings.
We are collaborating with academic experts. To understand how neuroscience connects with education, have a look at our summary of Breakdown of Key Summary Areas
"Anything that has an impact on learning will ultimately have a brain basis. The idea that our understanding about how the brain works could impact upon educational practice is therefore an attractive one. This idea has gained traction in the last 10–15 years (particularly in the last five years), with considerable discussion and a step change in the number of articles connecting the brain with education."
Dr Paul Howard-Jones, University of Bristol, United Kingdom
Focusing on neuroscience helps young people and teachers to look at who we are, how we develop and learn, and offers opportunities to change and grow.
Please, read more about bring neuroscience into education:
Professionals we are working with have a wide range of expertise including:
See the experts we are working with and what they are currently working on on our Research page.


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