Sotamies Honkajoen mineralogisesta propagandasta

Väinö Linnan sentenniaalin kunniaksi olen väkevästä yrityksestä huolimatta ajautunut lukemaan uudelleen kansalliskirjailijan tuotantoa ja viime viikonloppuna vuorossa oli magnum opus eli Tuntematon… pari viikkoa etuajassa, myönnettäköön, mutta menköön. Kirjan kyytipojaksi katselin Netflinxistä valtakunnan satavuotisiksi kolme vuotta sitten valmistuneen Aku Louhimiehen filmatisoinnin ”editor’s cutin” eli sen viisiosaisen neli- ja puolituntiseksi venytetyn version, joka muuten kokonaisuutena ylittää ainakin nyt viimeistään omissa kirjoissani Laineen klassisen 1955 tulkinnan.

Sarjan neljännessä osassa kuvataan vuoden 1943 Syvärin asemasotavaihetta, jossa joukot vähitellen tylsistyvät tappiomielialoihin samalla veistellen lampunjalkoja ja viilaillen potkurinlapoja sormuksiksi.

Jaksossa seuraillaan myös konekiväärikomppaniaan täydennysmiehenä saapuneen sotamies ”valistusupseeri” Honkajoen edesottamuksia ja pyrkimyksiä ikiliikkujan valmistamiseksi. Juho Milonoffin hieman vinksahtanut tulkinta Honkajoen hahmosta on muuten erittäin hyvä esimerkki koko Louhimiehen toteutuksessa mielestäni erityisen onnistuneesta sukupolviroolituksesta. Aika tarkkaan jakson keskivaiheilla mineralogin korva kuitenkin hörähtää…

Kirjassa Honkajoki kiertää komppanian asemissa tukikohdasta toiseen seurustelemassa omaa erikoista maailmankuvaansa, mistä hyvästä joutuu lopulta myös Lammion ripitettäväksi. Honkajoen saavuttua yhdeltä näistä kierroksistaan takaisin joukkueen omaan korsuun, tiedustellaan häneltä:

”Mitenkä se edistyy Honkajoella ikiliikkuja?”

Kirjassa Honkajoki vastailee omaan tavanomaiseen tapaansa, mitä sylki suuhun tuo, mutta uudessa elokuvassa hän kaivaakin yllättäen kassistaan kirjan, josta lukee vastauksen:

”Yksi nelilukuinen symmetria-akseli tuottaa tetragonisen alkeiskopin rajapintoina pari neliötä ja kaksi paria suorakaiteita.”

!?!

Tämä kidetieteen perusteiden lyhyt tietoisku johtaa ilman sen kummempia selityksiä Lammion vakavasävyiseen puhutteluun, joka kuuluu Laineen 1955 kaanonista tarkoituksellisesti pois jätettyihin kohtauksiin. Enteellistä…

Honkajoen mihinkään mitenkään liittymätön, mutta mineralogia tietenkin miellyttävä, töräytys on peräisin sivulta 28 Pentti Eskolan kirjasta Atomit ja Kiteet, jonka kustansi Tammi numerolla 6 kansanvalistussarjaansa Aikamme Kulttuuri. Kirjan käsikirjoitus valmistui jo sodan aikana, mutta mutta, julki se tuli vasta vuonna 1948(!).

Tämä pieni ”glitch” sallittakoon, mutta kiinnostusta se silti herättää.

Elokuvan dialogi seurailee suurimmilta osin, ja myös Honkajoki-episodin aikana, lähes orjallisesti alkuperäistä ja olisikin kiinnostavaa tietää, mikä tämän sarjaan päätyneen ratkaisun taustalla oikein on… ja jos kyseessä on puhdas vahinko, miten Atomit ja Kiteet -kirjan kappale on elokuvan tarpeistoon joutunut?

 

 

"Mineraalivaltti" - Helsingin yliopiston mineraalikokoelmiin perustuva korttipeli

Ennen koronakevättä jo jonkin aikaa muhinut ajatus Geologistet materiaalit -kurssin mineraalikuva-aineiston käytöstä hieman erityyppisessä opetusmateriaalissa otti toukokuussa ratkaisevat toteutuskynnyksen ylittäneet askeleet varadekaani Samuli Siltasen pyöritellessä erilaisia korttipeli-ideoita Twitterissä. Kesän aikana kypsyttelimme materiaaleja ja ajatuksia akatemiatutkija Jussi Heinosen kanssa ja syyslukukauden alkaessa Mineraalivaltti vähitellen alkoi ottaa muotoansa.

Mineraalivaltissa on neljäkymmentä varsinaista pelikorttia ja kaksi sääntö- ja lisätietokorttia.

Pelin säännöt ovat yksinkertaiset ja ne perustuvat 1970-80 -lukujen hittikorttipeleihin, joissa toisistaan mittaa ottivat autot, lentokoneet ja monenmoiset muut tekniset vempeleet. Mineraalivaltin idea on, että tunnistamisen kannalta relevantteja mineraalien ominaisuuksia, kuten esimerkiksi ominaispainoa tai kovuutta voi verrata samaan tapaan kuin vaikkapa huippunopeutta tai iskutilavuutta. Jokin mineraali voi olla symmetrialtaan ylivertainen muihin nähden ja jokin toinen puolestaan koostumukseltaan poikkeuksellisen monimutkainen. Mineraalien tuntemus on siis myös eduksi pelipöydissä menestymisen kannalta.

Mineraalivaltissa mineraalit on jaettu kymmeneen soveltavaan luokkaan, jotka noudattelevat pääpiirteissään IMA:n (International Mineralogical Association) suosittelemaa luokittelua. Silikaattien alaluokat (jalo, soro- ja rengas, ino-, verkko- ja hohkasilikaatit) on nostettu peliteknisistä syistä pääluokkien tasoisiksi viideksi luokaksi ja fosfaatit ja sulfaatit muodostavat yhteisen peliluokan. (Kuva: Samuli Siltanen)

Mineraalien ominaisuuksien, luokittelun ja koostumustiedon opetteleminen on vuosien varrella osoittautunut monille ensimmäisen vuoden opiskelijoille hieman haastavaksi rastiksi, joten pelillistämällä tätä pänttäystä on nyt mahdollista tuoda hieman uudenlaista kulmaa opiskeluun. Samalla korttipakka toimii oivana markkinointimateriaalina ja tuo muuten usein niin mystisenä näyttäytyvää mineralogiaa myös suuremman yleisön tietoisuuteen.

Korteissa esiintyvät mineraalit ovat osa Luonnontieteellisen keskusmuseon (LUOMUS) geologisia kokoelmia. Korttipelin mineraaleista voi oppia lisää HY:n Geotieteiden kandiohjelman Geologiset materiaalit -kurssilla, joka on tarjolla vuosittain myös Avoimen yliopiston puolella (AYGEOK_102).

 

Nyt niitä sitten saa...

Mineraalivaltti -korttipeliä on tällä hetkellä myynnissä Helsingin yliopiston keskustakampuksella sijaitsevassa Tiedekulman kirjakaupassa. Todennäköisesti jonkinlainen verkkokaupparatkaisu Helsingin alueen ulkopuolisille mineraaleista kiinnostuneille on myös tulossa piakkoin...

 

Luomus, Kumpulan kampus ja geologiset materiaalit Twitterissä:

@luomus; @KumpulaScience; #geologisetmateriaalit

 

Kartoita kallioperää HY:n geotieteen opiskelijoiden kanssa!

Tule mukaan tekemään Helsingin yliopiston Kallioperägeologian kenttäkurssin harjoitustehtävää! 

Tehtävän alkuperäisenä tarkoituksena oli korvata keväältä koronavirustilanteen vuoksi peruuntunutta kontaktiopetusta ja antaa opiskelijoille mahdollisuus harjoitella itsenäisesti kallioperähavaintojen tekemistä tutussa ympäristössä. Samalla tutustutaan hieman Suomen kallioperän kivilajeihin kurssilaisten tekemien havaintojen ja niistä tehdyn yhteisen koonnin avulla.

Varsinainen kurssilaisten tekemä harjoitustehtävä toteutetaan suljetulla kurssialustalla mutta havainnointiin voi osallistua kuka tahansa ja kaikki kurssin aikana kirjatut havainnot ovat mukana yhteiskoonnissa, joka päivittyy osana tätä julkaisua. Tehtävä sopii kaikille luonnosta ja kallioperän kivilajeista kiinnostuneille ja pienellä perehtymisellä myös esimerkiksi yläkoululaisille tai lukiolaisille maantiedon/maantieteen itsenäiseksi havainnointitehtäväksi.

Tehtävä on yliopiston kurssilaisille täysin vapaaehtoinen, eikä sitä tehdessä ole tarkoitus pakottaa ketään liikkumaan esimerkiksi julkisilla liikennevälineillä tarpeettomasti! Ulkona liikkuessa on muutenkin syytä muistaa turvavälit ja tilanteen mukainen toiminta.

Ajatuksena on, että geologisia havaintoja voi tehdä liikkumalla jalkaisin kotoa vaikkapa lenkkeillessä tai muuten ulkoillessa. Parhaassa tapauksessa kivilajihavaintoja voi tehdä jopa omassa pihapiirissä, lähimetsikössä tai -puistossa. Esimerkiksi pääkaupunkiseudulla on Helsingin keskustaa myöden lähes mahdotonta liikkua kovin pitkiä matkoja näkemättä kalliopaljastumaa tai louhittua kallioleikkausta. Tarkoitus on hyödyntää näitä "lähipaljastumia" kallioperähavaintojen tekemisen harjoitusaineistona.

Mitä tehdään:

Etsi kalliopaljastuma, jolla voit tehdä havaintoja suoraan kallion pinnalta niin, ettei sinun tarvitse paljastaa kalliota lisää, vasaroida murtopintaa, kiivetä vaaralliseen paikkaan tai mennä jonkun toisen pihapiiriin. Lähtökohta on, että havainto tehdään joko omassa pihassa tai julkisella paikalla kenenkään muun omaisuutta, tekemistä tai elinkeinoa häiritsemättä ja omaa turvallisuutta vaarantamatta. Varmistu kuitenkin aina, että teet havainnon kiintokalliosta, etkä esimerkiksi isosta siirtolohkareesta.

Vinkkejä kivilajien tarkasteluun, luokitteluun ja tunnistamiseen löydät mm. seuraavista osoitteista.

GTK:n Retkeilijän kivioppas (sivut. 44-55): http://tupa.gtk.fi/julkaisu/erikoisjulkaisu/ej_060.pdf
Kivikone-sivusto: https://www.kivikone.fi/
Geologia.fi: http://www.geologia.fi/index.php/2018/04/23/suomen-kalliopera-opetusmateriaali-gtk/

Tutki paljastuma ja kirjaa siitä ylös ainakin seuraavat asiat:

• Havainnon tekijä ja havaintoajankohta
• Sijainti sanallisesti (esim. kaupunki, kaupunginosa, puiston nimi tms.)
• Paljastuman koordinaatit EUREF-FIN koordinaattijärjestelmässä (nämä saat muuntamalla esim. puhelimen Google Maps -sovelluksesta saadut koordinaatit paikkatietoikkunan https://kartta.paikkatietoikkuna.fi/ sovelluksessa tai arvioimalla havaintopisteesi sijainnin myöhemmin tietokoneella)
• Paljastuman koko (X m kertaa Y m) ja tyyppi (tieleikkaus, rantakallio, jne.)
• Paljastuman havaintopinnat (silokallio, tieleikkaus/tuore murtopinta, rapaumapinta jne.)
• Listaa paljastuman kivilajit (anna kivilajeille kenttänimet ja arvioi niiden määräsuhteet)
• Kuvaile kivilajit (raekoko, mineraalien laatu ja määräsuhteet eli moodi, suuntaus, väri jne.)
• Rakenteita ei voi ilman geologista kompassia mitata, mutta ne voi kuvailla (mainitse esim. raitaisuus, kerroksellisuus, liuskeisuus, poimuttuneisuus jne.)
• Kuvaile kivilajien suhteet toisiinsa (esim. graniitti tunkeutuu juonina liuskeeseen tms.)
• Ota paljastumasta edustava valokuva, jossa esiintyy mahdollisimman paljon kuvailemiasi asioita. Muista laittaa kuvaan myös mittakaavaksi jokin tunnetun mittainen esine, jonka mitat ilmoitat myös kuvatekstissä (esim. "Mittakaavana kynä, 11 cm").

Anna havainnollesi myös havaintotunnus, joka on muotoa KPK20-APHE-001, jossa KPK20 on kaikille kursisn havainnoille yhteinen, nelikirjaiminen tunnus muodostetaan kahden ensimmäisen etunimesi etukirjaimista ja sukunimesi kahdesta ensimmäisestä kirjaimesta (Aku P. Heinonen --> APHE) ja kolminumeroinen luku kertoo havainnon juoksevan numeron -001, -002, -003... jne. Voit siis luonnollisesti tehdä myös useampia kuin yhden havainnon, jos innostusta riittää!

Kirjoita havaintosi alla olevalle keskustelupalstalle tai lähetä ne sähköpostitse alla olevaan osoitteeseen. Alla on myös esimerkkihavainto, josta voit ottaa mallia ja koontikartta, jolle palautetut havainnot päivittyvät vähintään parin päivän välein. Havaintoja otetaan vastaan näillä näkymin ainakin toukokuun loppuun asti.

Kysymyksiä voi esittää joko tämän postauksen kommenteissa tai sähköpostitse

Kurssin opettaja:
Yliopistonlehtori Aku Heinonen
Helsingin yliopiston Geotieteiden ja maantieteen osasto
aku.heinonen@helsinki.fi

Koonti 10.5.2020 (klikkaa kartta kuvasta isommaksi)

Esimerkkihavainto:

Havainnon tekijä ja havaintoajankohta

Aku Heinonen, 29.3.2020, klo 16:05

Sijainti sanallisesti

Helsinki, Hallainvuori, Viilarintien tieleikkaus

Paljastuman koordinaatit EUREF-FIN koordinaattijärjestelmässä

391774, 6677374

Paljastuman koko ja tyyppi

150 m pitkä ja n. 12 m korkea pystysuora tieleikkaus (Kuva 1).

Kuva 1. Yleiskuva Viilarintien paljastumasta.

Paljastuman havaintopinnat

Vanha tienrakennuksessa louhittu murtopinta, joka pääosin jäkälöitynyt, mutta paikoin tuoreempia kohtia, joista havainnointi vielä mahdollista.

Kivilajit

Gneissi (voisi kuvata myös graniittina ja kiilleliuskeena)

Kivilajikuvaus

Paljastuman pääkivilaji on raidallinen, voimakkaasti suuntautunut gneissi, jossa vuorottelevat tummat, biotiittivaltaiset raidat ja vaaleanpunaiset graniittiset raidat. Raitojen paksuus vaihtelee n. 1-30 cm. Tummat raidat ovat pääosin ohuempia kuin vaaleat. Tummat raidat koostumukseltaan biotiittia (100%) ja hienorakeisia. Vaaleiden raitojen mineraalikoostumus hyvin leukokraattinen, päämineraalit kalimaasälpä (80%) ja kvartsi (15-20%), vaihtelevasti plagioklaasia, mutta pääosin alle 5%. Graniittisten osien raekoko vaihtelee n. 1-50 mm (vallitseva raekoko karkearakeinen), paikoin jopa pegmatiittisia osia.

Rakenteet

Raitaisuus on havaintopinnalla pääosin pystysuoraa ja lähes lineaarista tai loivasti poimuttuvaa (Kuva 2).

Kuva 2. Paljastuman pääkivilaji, jossa näkyvät vuorottelevat tummat ja vaaleanpunaiset raidat. Mittakaava: matkakortin pitkä sivu on n. 9,5 cm.

"Rocks and minerals" -video appearance on YouTube

I was recently asked by Markus Salamander, a nature documentary enthusiast, to visit his YouTube channel to talk about rocks and minerals and their identification. Our session boiled down to an almost one and a half hours chat on geology, rocks, and their formation processes. Check the video out below (unfortunately only in Finnish) or on Markus's channel.

#geologisetmateriaalit mineral poster

All the mineral pictures from this autumn's Geological materials (#geologisetmateriaalit) course with mineral names and chemical formulas are now compiled into a neat poster licensed under CC-BY-NC-SA 4.0.

A2-size PDF is available upon request from aku.heinonen@helsinki.fi.

Most of the samples come from the University of Helsinki Department of Geosciences and Geography teaching collections curated by the Finnish Museum of Natural History (LUOMUS).

 

Stepping up the macro game

Since I started my daily geological materials posts on social media a couple of weeks ago, I’ve constantly been thinking and researching ways to improve the quality of my mineral macro shots. I have a decent basic Canon full frame set-up of 6D (v.1) with a 100 mm 2.8/L macro lens and have been using external LED elements for main lighting but many of the objects I want to take pictures of still do not yield to the physical restrictions of optical realities.

Main issue in macro photography is the focal depth that very much starts to become an issue in the cm-scales of mineral samples. For focal depth you need more light but long exposures make magnified shots prone to shaking and other external problems. The basic set-up just hasn’t been enough to achieve all the things I’ve wanted to image and I’ve constantly been looking at some alternatives to improve the situation.

In mid-September, we took the first year students to the traditional “freshman” field trip in Southeastern Finland. One of the stops on the trip is a gem-quality topaz quarry around the town of Kotka, which has been quarried by several mineral clubs on and off for the past decades. I remember going there with my tutors when I started my studies as well.

The quarry is located in the Kymi topaz granite stock, which is associated with the ca. 1.64 Ga Wiborg area rapakivi magmatism (you can read more about rapakivi granites for example here), and it is possible to find nice amazonite, fluorite, dendritic biotite, and even beryl samples there. The main attraction, however, is the slightly bluish and, at its best, transparent gem-quality topaz. For many years, the yield of the annual trip has not been very good as most of the good samples have already been hounded from the surface and no one has been doing any recent blasting at the site. This year turned out to be a bit different…

Three of the students were able to find some very nice, rather clear and euhedral topaz crystals. The largest one was a 1,4 cm long stubby crystal, with at least five prisms {110}, {120}, {110}, {210}, and {011}, 2 or 3 bipyramides {111}, {221}, and possibly {112}, and a terminating pinacoid {001}.

I was allowed to loan the crystal to take some shots but was again not happy with the way the first round of images turned out so I was finally motivated to invest a bit to get the shot I wanted. I ended up ordering a ring flash, extension tube set, and an adjustable macro rail in order to fine-tune the focal depth for focus stacking. Below you can see some results. There is always room for improvement especially in the far end of the focus range, but with this, I already start to be quite satisfied…

Canon 6D; 100 mm 2.8/L macro; GENESIS GMR-150 macro rail; Viltrox extension tubes: 12+20+36 mm; Meike FC110 ring flash (LED-mode); ISO160, F/6.3, 1/30; focus stack of seven images (Adobe PS edits). Length of crystal: 1.4 cm.

Crystal and flame - An essay on Italo Calvino and geosciences

 

The latest edition of Geologi-magazine of the Geological Society of Finland (SGS) features an article I have been basically writing on and off for the past ten years. The paper is not really a scientific contribution but reflects on the many ideas and personal inspirations I have experienced while reading the works of the Italian author Italo Calvino throughout the last decade.

Originally I found Calvino through his Cosmicomics short stories and was fascinated by the way he digested and presented scientific theories and ideas in his unparalleled style and had found innovative ways to write about the complexities of the natural world. I quickly noticed there were plenty of geological and especially mineralogical parallels in many of his works and remember being completely paralyzed by his depictions of time and temporal experience in general.

Most of Calvino's ideas on time I have later found embedded for example in the works of Hannah Arendt (Vita Activa especially), Max Frisch (Homo Faber), and many many others. However, Calvino was always the first, and I still annually return to his "Six Memos for the Next Millennium" to refresh my points of view.

After getting more and more familiar with his works throughout the years, I started seeing this overarching theme that finally about a year ago coalesced into a concrete framework and found its home in the recent work on thermodynamic modeling of igneous systems that we have been developing in our research group. It became clear to me that Calvino's entire production could be portrayed in terms parallel to thermodynamic systems and many of the minutiae and details actually followed very similar logic to the principles of modeling thermodynamic equilibria.

The ideas of juxtaposed crystal and flame depicted in Calvino's "Six Memos" became the leading principles of my interpretation of his work already early on, but only now they found their true meaning and everything kinda fell into place.

At the beginning of the year, I started working on the essay by rewriting some earlier passages and compiled notes from old notebooks etc. Over the winter lecture break in March I re-read the entire translated works of Calvino in order to clarify the image I had put together in my head and finished polishing the essay in May. There had been many earlier attempts at getting everything into context but this thing couldn't had been written at any other time than right now.

Seeing the article in print meant more to me than I dared to admit earlier on, but I am really happy with the way that it turned out. I'm glad that now I'm able to share these ideas also with everyone else. I think I won't touch much of his other work in a while, but I will still try to read the "Six Memos" every year. Every time it seems to have something more to offer...

You can read the entire article here (only in Finnish for now, except for the short summary, sorry) and if you have something to share about it, please drop a line. Several readers of the print edition have already contacted me but I hope the online version will reach an even broader interested readership.

TSV Science photography exhibit, 24 Sep - 16 Jan

Early this year, I found out about a Science Photography Competition organized by TSV (The Federation of Finnish Learned Societies) as a part of their 120th anniversary celebrations.

Around that time I had also started a macro photography project to update some of the mineralogy teaching materials for my geological materials course and gradually developed the idea that some of the images would possibly be suitable for the competition.

The series I ended up submitting came to be called "Platon's five-fold mistake" and it features four images of minerals in the isometric crystal system that have a strong euhedral tendency each in the shape of one of the five Platonic solids: magnetite (octahedron), pyrite (dodecahedron), fluorite (cube), and tetrahedrite (tetrahedron). The fifth image in the series features a structural model of the last Platonic solid, icosahedron, which is not permitted as a crystal form due to its non-periodic five-fold rotational symmetry. Therefore, there are also no minerals that could take up its form. Icosahedron has, however, been observed in synthetic materials and also in some very minute phases related to meteorite impacts in which it is said to form quasi-periodic structures, or quasicrystals.

I guess the jury is still out about the inclusion of quasi-crystalline materials in the official mineral family but, regardless, the founder of the first quasi-periodic structure Dan Shechtman was awarded the 2011 Nobel price in chemistry for his discovery.

The results of the photography competition were made public today in TSV's 120th anniversary celebrations and at the same time the related photography exhibition was opened for the public at Tieteiden talo (house of sciences) in Helsinki.

Even though I did not place in the competition, I was very happy to find out that two of my pictures had the honor of being featured in the exhibit. The exhibit will be open, free of charge, until "The Night of the Science", which will be organized on January 16th next year.

Go check it out if you're in town...

Further reading on quasicrystals:

Bindi et al. 2009. Natural quasicrystals. Science 324: 1306-1309.

Shechtman, D. 2013. Quasi-periodic crystals - the long road from discovery to acceptance. Rambam Maimonides Medical Journal.

On Dark Crystals…

A recent Guardian long read piece on “Dark Crystals” has popped up on my feed several times in the past couple of days and it sparked some immediate but maybe not too coherent responses in my head. Regardless of coherence, here are some thoughts:

Basically the piece is reporting that:

1) The demand for crystals (sensu lato) has been on the increase due to their alleged health effects.

2) Crystals are mined in hazardous conditions by people who don’t benefit (enough) of their perilous efforts.

The article then proceeds to describe several first hand accounts on these conditions and the people who have to deal with them. Alongside of not really defining what crystals in this context are, what is almost completely left out of the report is the “alleged” part in the health effect claims.

Lets be clear; there are none!

If a health effect is claimed it needs to be verified. In order for something to be verified, it needs to be observed. No observations of said health effects have been made. Full stop, period. To claim something else is unethical, at the least.

Where do the urge and need to come up with some bogus magical properties of natural objects then stem from? Crystalline structures with their many unbelievable and aesthetically astounding (and 100% scientifically proven) properties are already in themselves natural wonders and nothing short of an actual real life miracle! Where lies the need to invent something more? There is still so much we don’t understand about the true and really exciting phenomena in the crystalline world.

I can think of two reasons:

First is the primal need for people to come up with supernatural explanations for natural phenomena. This is further amplified by the inherent complexity and mathematical characteristics of nature (and especially crystalline matter). It's more difficult to understand things in order to explain them but very easy to come up with stories, analogues, and anecdotes, which follow some made up internal logic.

Secondly, and more importantly, there is financial benefit from feeding these said beliefs. This is the worse of the two and also the major machinery behind the problems described in the Guardian piece.

However, observations about problems in tracing supply chains made in the article are true for almost all modern commodities. I am not sure why the situation with crystals or minerals would be somehow special. Without belittling the troubles of people featured in the article, the framework descriptions of small-scale crystal mining could basically be replaced with a description of an Asian t-shirt factory. The problems are the same: lousy pay for strenuous and risky work, mostly executed by under-aged children.

I guess mining has an eerie aura to it nowadays and these kinds of stories somehow fit the prejudices of the tarnished industry image better than other products used in everyday life.

The reason why this topic resonates with me is that I feel rather passionately about the intricacies of crystalline structure and its actual scientific study. I also use the aesthetics of natural symmetry displayed by natural minerals to teach mineralogy and crystallography. The awe arisen by euhedral natural crystals is proven to be an intuitive and effective motivator to find out more about the inner workings of the natural world. There is, however, nothing supernatural about them, only pure and beautiful natural symmetry.

Maybe the line between bogus health claims and acknowledging the reality of the crystal realm is thinner than I have previously thought…

To underline, the long read logic is correct and I 100% agree that the business they describe is flawed on many levels.

Geological materials on Twitter

I was recently inspired by a really nice book on research and professional communication in social media by Petro Poutanen (@petropoutanen) and Salla-Maaria Laaksonen (@jahapaula).

Faktat nettiin is a really good manual for any researcher who would like to take up a more active role on social media, bring forth their expertice on broader forums, or generally just develop themselves as a communicator.

It sure got my juices flowing...

Previously I've mostly been only following some interesting topics, people, and handles on Twitter but after reading this book I got the inspiration to try moving some of my posts from Instagram to Twitter. From there, things got out of control pretty fast as I got the idea to migrate some of my Geological materials course teaching materials also there...

The plan at this point is to tweet a picture of a mineral (or other cool stuff) from the course's teaching materials and to deliver a related short infoid every day for as long as the course is running this semester. Let's see how this takes off...

You can follow the #geologisetmateriaalit hashtag to keep up (and me @AkuHeinonen) also on Instagram.

Student projects picking up some momentum

Just a quick note on a couple of student projects that were successfully launched during the Q1/2019.

Petrology of the Suvasvesi granitoid intrusion in northern Savonia

The first one, SUVAS-19, was graciously funded by the K.H. Renlund foundation and will partly be realized in collaboration with the Battery Minerals project operations ran by the Geological Survey of Finland in Northern Savonia. The aim of the project is to map and study the mineralogy and petrology of the ca. 1.87 Ga Suvasvesi granitoid intrusion and its relationship with nearby pegmatites intruding the Paleoproterozoic metasediment sequences of the Viinijärvi suite.

Hanna Rantanen is the MSc student who has been hired to do the field work and hopefully we will see some nice results already by the end of the year.

http://projects.gtk.fi/akku/index.html
http://khrenlund.fi/en/

Mineralogy and petrography of the Kuohenmaa orbicular quartz monzonite

Another student project will take a closer look at some orbicular rocks and especially at this stage the world-class multi-shelled example from Kuohenmaa in Kangasala. The Kuohenmaa orbicular quartz monzonite has a particularly well-developed orbicular structure consisting of a core and several alternating radial plagioclase-rich shells and tangential biotite-rich shells.

One of the largest samples of the Kuohenmaa orbicular quartz monzonite from the collections of the Geological Survey of Finland. The Survey was very kind to let us take detailed pictures of their samples for research purposes. The ruler used as a scale is 20 cm long.

The petrogenesis of orbicular rocks is controversial and several theories have been suggested to explain how the orbicules were formed. The two prominent theories suggest their origin to relate either to generation of local diffusion-controlled enrichment fronts onto the orbicules crystallizing from magma or cyclic changes in crystallization pressure or temperature. In this project, major and trace element mineral chemical analyses combined with statistical petrography will be used to test the applicability and validity of existing orbicule-forming theories and, if possible, create a new hypothesis for orbicule forming process of the Kuohenmaa orbicular rock.

The student working on this topic is Minna Markkanen and she has already made some very interesting discoveries based on very basic petrographic observations. She gave a poster at the Geoscience Colloquium earlier this year on the topic and is making strong progress also on other fronts. You can read more about recent discoveries in the abstract volume of the meeting, p 42:

http://www.geologinenseura.fi/files/Abstract_Collection_v1-5th_National_Colloquium_of_Geosciences.pdf

Wrap-up of the year 2018...

The year 2018 comes to a close and now there's finally some extra time (not really) to summarize some recent achievements and milestones...

1) A new PhD project!
The year got off to a great start as Riikka Fred got funding from DONASCI to study the monzodioritic rocks and evolution of the anorthosite parental magmas in Ahvenisto. This was great in many respects, not least due to the fact that we finally got to collaborate with Jussi Heinonen and his PALIN project for this one. Riikka has been working hard all year and the labors have also born some nice fruit...

2) Journal of Petrology Paper
This was a long running project that went over a lot of hindrances but finally saw the light of day in early 2018. Technically the paper was published in the last JPET issue of 2017 but the editorial handling ended only in March. Finally something complete to show for he SA project...

3) Teacher of the year award
The students elected me as the teacher of the year 2017. It was great to get acknowledged for all the hard work put into the first year of teaching. Looking back at it, I would do many things differently... but wouldn't change a day...

4) New teaching duties
As the Department lost invaluable P. Heikkilä to the Geological Survey last spring I stepped up to take the extra teaching load and ditched most of my old stuff in return. Preparing the materials and teaching basic crystallography and mineralogy has taken most of the past year but has been really rewarding. Research duties have had to take a second row seat because of this though...

5) Mineral photography
Teaching the basic mineral course has given a nice excuse to photograph plenty of mineral samples for lecture notes and there might be some additions to this site as well in the near future... am planning to add a page for the best shots but need to think more about the layout possibilities still... stay tuned...

6) Two new MSc projects
I was able to launch two new MSc resarch projects, one to go even deeper into the mineral chemistry of Ahvenisto complex and to assist Riikka in her project and another to finally take a closer look at the Kangasala orbicular rocks. Both projects are still in their infancy but promise to get more wind under their wings at the beginning of next year... exciting times...

7) Riikka's first paper!!!
Riikka's first research paper was accepted for publication (today) and with that the monzodiorite project takes a major leap forward... more to come next year... Look out for the first edition of the Bulletin of the Geological Society of Finland next year...

That's about it... will add more if something pops up... maybe more frequent updates from now-on... :D

OpenFIRE in the books and some other stuff

Lots of new stuff going on...

The end of May saw my last contributions to the FIRE-ATT project at the Insitute of Seismology. During the past nine months I contributed to five external pieces and four conference papers on the OpenFIRE project and presented the application and the project in five conferences and other marketing forums.

Bulk of the project on my behalf is, however, still unpublished as the full version of the application is not yet released and the geological descriptions that were my main responsibility in the OpenFIRE are going to be out only when it happens. You can still check out the beta (or the full version when it gets released) here.

Anyways, good times, but now it's time to move on to other things.

Starting from the beginning of June I have returned to the Division of Geology and Geochemistry. First as a visiting scholar and from the beginning of August in the position of a University Lecturer in petrology.

Beginning in the fall most of my time will, therefore, be spent teaching basic petrology but during the summer I will mostly be concentrating on my book project. Also hoping to finally(!) tie up some loose research project ends before the teaching hassle begins.

So, major gears shifting but I'm excited at the face of all the new challenges...

Geology paper on rapakivi zircon

We just got a manuscript accepted in Geology.

The paper (A priori evidence for zircon antecryst entrainment in megacrystic Proterozoic granites) presents a first-order U-Pb and trace element comparison of suspected antecryst zircon populations that are included within the megacrystic rapakivi texture -forming alkali feldspar ovoids to their respective groundmass zircon populations.

We utilized a simple (but also rather tedious) microdrilling approach to extract zircon from within the rapakivi ovoids and were able to show that the populations show dissimilar geochronological and compositional characteristics.

The paper will appear in the March 2016 issue...


Abstract
Entrainment of antecrystic zircon in early saturated main silicate phases has been recognized as a complicating factor in high-precision U-Pb geochronology of Phanerozoic granitic systems, but has not been demonstrated for Precambrian rocks. We report U-Pb ages (secondary ion mass spectrometry) and trace element (laser ablation–inductively coupled plasma–mass spectrometry) compositions of zircon from three main ferroan granite types of the late Paleoproterozoic Wiborg rapakivi granite batholith of southeastern Finland and vicinity. Zircon was extracted from the interior parts of megacrystic (diameters as large as 15 cm) rapakivi-textured alkali feldspar ovoids using a microdrilling technique. Compared to zircon in ovoid groundmass, zircon in the ovoids has higher incompatible element values (e.g., uranium and rare earth elements) and, for two of the three samples examined, slightly older (by ∼1 m.y.) average U-Pb ages. These observations suggest that the ovoid material of the rapakivi granites entrained zircon from earlier magmas that were compositionally different than the final magmatic host of the ovoids. Groundmass zircon implies similar average U-Pb ages for all the studied samples, ca. 1628 Ma; this is regarded as the final crystallization age of the granites. These observations show that it is viable to measure statistically valid age differences between antecrysts and groundmass of Proterozoic granites. Overall, our sampling technique provides enhanced textural control of antecrystic zircon in a wide range of sample materials.

NGWM16

Hit the ground running in January with only two weeks to prepare for the Nordic Geological Winter Meeting (NGWM), which were held in Helsinki on 13th to 15th Jan.

I gave a talk on the micro-drilling methods we've been using for zircon sampling and a poster on the geochronological results. Also participated in preparations of three other presentations, which totaled the Wintermeeting at five personal contributions, and chaired a session of Fennoscandian granitic magmatism.

Met a lot of people and had a cool meeting! Didn't have enough time for the social events though, and the poster sessions were organized a bit weirdly in between oral sessions but otherwise all was good.

With that, the quota for scientific meetings is full for the time being... time to concentrate on getting some new material published.

Pages online

Finally got around to finishing the layouts and most of the content framework on these pages. Some of the features required abit more nerd-out than I expected but I think the end-result looks ok...