Welcome!

Why hello there and welcome to my Geography blog. I'm an A-level student from Somerset studying Environmental Science, Geography and Archaeology. I should probably explain how this blog has come about. During my first lesson of the new year my teacher exclaimed that I should start a “What I learnt this week…” blog. I thought this would actually be a good idea to help for revision and “consolidate my learning” which is what the teachers always tell me to do and it might (hopefully) help other people doing geography as well. So this is my geography blog.

There are two of us!

So i am a geography geek and got added so i can blog too. what can i say, i love it absolutely love it! i'm not really that clever (that's a lie she is!) but it doesnt stop a love i have for the subject, i also study environmental science and geology.

My portrait photo should reflect what topic I'm studying at the time. If I remember to change it... If you have any questions or want to talk to us about anything Earth Sciences related please don't hesitate to ask!

Friday, 18 February 2011

Encounters at the End of the World

This is one of the best films I have ever seen and has made me definitely want to visit Antarctica before I either die or it becomes 'westernised'. The view I have of Antarctica is one of never-ending snow and ice with a vast biodiversity under the ice in the ocean. Most of the continent is still like that apart from McMurdo which in the Spring/Summer becomes a normal functioning town with a population of about 1000, that kind of disappointed me but I suppose there needs to be a central hub to act as a base.

What I dislike about McMurdo is easily made up for with its inhabitants. They range from the adventurous to the pure weird. One former philosopher states that he thinks all the people who are a bit strange and like to explore end up in Antarctica, a theory later backed up by a linguist who describes that "all people who aren't tied down fall to the bottom", in this case Antarctica. If you're thinking these people are a bit odd then they're nothing compared to a plumber who believes that he's descended from the Aztec royal family or the Bus driver (former Banker) who once got chased by the Mayans because they thought he was a child catcher. Although strange you get the sense that these people live here because they really love it, the linguist also raises a very thoughtful point. We try to solve all kinds of biodiversity needs/climate change/stop deforestation etc. yet in 2005 it was reported that we were losing a language at the rate of one a fortnight. Should we focus on protecting our cultural heritage as much as the environment?

What I find remarkable about Antarctica is how people describe it as an incredibly peaceful place and the next minute they're dynamiting the ice to create a dive hole. I don't think it's a problem, just a bit strange. The scientist explains that some of the creatures in the deep seem like they're out of a sci-fi film and once the camera descends into the waters it's easy to tell why. In the darkness of the ocean looks mean nothing, it doesn't matter if you have rainbow scales what you actually need are some sharp spines. The ecosystem here is one of the most violent and extraordinary on the planet. The divers are looking for are the most primitive forms of life, trying to understand how life could have formed in the first place. The cameraman captures the moment when they state they've potentially found a new species, something which they claim to be remarkable. The head scientist continues eating his cereal.

One of my favourite moments in the film is when they visit a scientist who has worked in isolation with penguins for so long that he doesn't really enjoy talking to humans anymore. You can tell that Herzog has to try and keep a dying conversation going. The extent can be seen by the fact that Herzog has to ask if there are gay penguins and if they can go insane. It's the most surreal conversation in the film without a doubt.



The film also visits Mt Erebus which allowed me to construct a new view of volcanologists. They're quite strange but then again so is everyone on Antarctica... Volcanologists visit Erebus as it's easier/safer to visit than Congo and Kenya which are the only other places where volcanoes with exposed inner magma are found. As you'd expect the volcanologists are dressed up in thick layers of thermal equipment apart from Professor Clive Oppenheimer from Cambridge who's wearing... tweed.

I can't recommend this film enough. It's unbelievable, I loved it and think I'll probably watch it again at some point. Werner Herzog's gruff German accent is perfect for the documentary which has been filmed so brilliantly. It's definitely up there with my favourite films.

Sunday, 13 February 2011

Week 6 - Nothing?

I apologise for the lack of post this week geographers.
I spent all of Saturday working and then 9 hours today recording an EP with my band, I will however be updating this tomorrow... as long as the field-trip doesn't prevent me.

James

Wednesday, 9 February 2011

Mount Merapi

Here is my Merapi case study, void of any photos at the moment because I think I might fall asleep but I'll put some photos up soonish (if I remember...) 


·             Active Stratovolcano (composite)
·             Located on the border between central Java and Yogyakarta
·             Has erupted regularly since 1548
·             Thousands of people live on the flanks – high risk from mass movement e.g. Lahars
·             2010 was the largest eruption since the 1870s

Background to the Volcano
·             Found where the Indo-Australian plate is subducting beneath the Eurasian plate.
·             Used to be basic; basaltic lava, effusive but now it’s more intermediate; antedesitic lava and explosive which cause lava domes that produce pyroclastic flows when they collapse

Chronology of Events
·             25th October – Three major eruptions are recorded

·             26th October – A column of smoke rises 1.5km from the top of the volcano, also the first fatalities are recorded

·             29th October – Pyroclastic flowing 3km down the side of the volcano for 4-9 minutes, pyroclastic flows also hit the Lamat, Senowo and Krasak rivers. Pollution of water courses – social + environmental

·             30th October – Eruptions get more violent, ash fallout is found over 30km away and police/military personnel posted closest to the volcano are seen fleeing with civilians, which cause a mass ‘clog’ of the roads. Heat clouds flow into the Krasak and Boyong Rivers (heat pollution, not good). Yogyakarta’s airport was closed from 05:00 until 07:00. A pyroclastic flow headed toward Gendol River, Kuning River, Krasak River, and Boyong River. A fresh eruption then caused sand to rain up to 10km away

·             1st November – Louder explosions than before caused a sudden rush of panic evacuation clogging the transport systems. A continuous stream of steam clouds was sent into the air for 40 minutes. The ash from that day reportedly raised 1.5km into the air; air travel is disrupted. Over 70,000 people have now been displaced and some are beginning to develop health issues such as respiratory infections and eye irritation.

·             2nd November – 26 Pyroclastic flows are reported

·             3rd November – Heat clouds travel up to 10km from the volcano, forcing the government to evacuate previously set up refugee camps. 38 pyroclastic flows reported in the first 12 hours of the day, 19 of which travelled 4km south. Volcano spewed ash and cloud 5km into the atmosphere for an hour. Biggest eruption so far, 3 times that of the eruption the week before

·             4th November – Heavy rain the night before triggered Lahars with mixtures of water and rock debris cascading down the Kuning, Gendol, Woro, Boyong, Krasak and Opak rivers on the slopes of the volcano, a bridge was destroyed. The volcano had now been erupting for 24 hours with the largest eruption being recorded at 05:55. Heat clouds of between 600° and 800° spread 11.5km and reaching toward the edge of the 15km exclusion zone.

·             5th November – Another major eruption causing the extension of the exclusion zone to 20km, residents within 15km asked to leave for safety. Bronggang, 15km from the volcano had its’ streets covered with 30cm of ash. 100,000 people had now been evacuated and the scientists began to retreat.

·             6th November – Just before midnight smoke, hot air and jets of flames as high as 3km occurred in the north, west and east. The official exclusion zone remained at 20km after a day of high activity.

·             7th November – Merapi continues to ‘belch’ out pyroclastic flows with hot ash heading towards the Gendol and Woro rivers. The death toll on the slopes now reached 135. Police report that they’re having difficulty keeping people out of the exclusion zone.

·             8th November – Gas and ash soared 4km into the air

·             9th November – Bodies were retrieved from villages, which had been destroyed by pyroclastic flows as the volcano intensity dies down. Hot ash is confirmed to be reaching heights of 14.5km making it the biggest eruption in Merapi’s history. A 5.6 magnitude earthquake was measured in Yogyakarta yet it had no connection to the volcano.

·             11th November – The volcano continued to erupt however at a reduced intensity. 17 avalanches, 1 hot ash eruption and 1 volcanic earthquake were reported.

·             17th November – Hot air clouds, smoke columns, avalanches and volcanic eruptions continued on the 16th, 17th and 18th. The main threat was from hot air and ash clouds whilst lava injections were regarded as an indirect threat.

·             Late November – Merapi was still a threat due to hot ash clouds however eruptions (although still frequent) were decreasing in intensity. Lava and lahars are regarded as indirect threats. The exclusion zone is between 5 and 20km

·             December – The official volcano threat level is reduced from 4 to 3; the threat level had been increased to 4 in late October. Although the threat level had been reduced volcanologists maintained that there would be threat from hot ash and possible lahars. An ongoing exclusion zone of 2.5km was set up.

Management
·             The government initially set up refugee camps within 15km of the volcano yet these needed to be moved further as the volcanoes intensity increased.
o    This resulted in logistical problems with the movement of people resulting in poorer healthcare being provided
·             On the 7th November the price of vegetables was reported to be increasing, many schools also began to close.
·             The Health Ministry reported on the 7th November that the supplies to deal with the many refugees were not sufficient but they could manage.
·             9th November, the Chairman for the Indonesian Red Cross calls for education and training to be provided to help deal with Natural Disasters in the future.
·             11th November, a report suggests that the refugees will start developing mental health issues due to the events and the limbo between refugee camps. 1 man has already committed suicide due to stress.

Casualties and Displacement
353 people died overall. Most of the casualties were a result of gas clouds, respiratory problems and burns. Some deaths were also caused by road accidents as evacuation took place. On the 11th November it was reported that the volcano had displaced 350,000 people. 800 people are reported to have suffered minor to severe physcological trauma due to the volcanic events.

Stuff to link to SPEED:
Social – loss of life/buildings, mental health issues
Political – Had to call on help from UAE
Environmental – Huge amounts of pollution to river systems, thermal pollution and nasty gases
Economic – Increases in food prices whilst people aren’t getting a wage
Demographic – Reduction in workforce through death/illness means a reduction in the economy and the ability to produce what’s needed for the country e.g. food. 

Sunday, 6 February 2011

Week 5 - Tectonics

You should totally listen to this whilst reading the blog, it's in no way a shameful plug of my own band... 


Week 5 - After what seems like months trawling through endless sheets of data about Belfast and learning obscure geography terminology which I'm not sure if I'll ever use again it's finally over and we get to start one of my favourite modules. Tectonics.


Now tectonics isn't one of my favourite modules only because it has a t-rex but also because it produces such amazing things like this and continuously amazes people worldwide. It's unlikely that we will ever understand everything there is to know about tectonics and that's what makes it so interesting.


Right so, where did we leave off? I know many people are probably thinking that, not able to remember much about tectonics. Vicky's already so elegantly gone through what we did during the week involving volcanoes so I'll reintroduce you to the tectonics module from the start...


The year started off with us having to do that lovely essay... remember that one? It was all about the history of plate tectonics. The Wilson Cycle, similar fossils found on different sides of the world etc.
Next came the different types of plate boundaries and seeing as I'm a nice person (most of the time) I'll summarise them for you:


Conservative Boundaries: e.g the San Andreas Fault Line


There is no subduction or adduction, the plates try to move laterally against each other instead. No volcanoes occur here but instead there are massive earthquakes




Hotspots: e.g. Iceland, Hawaii (shows plate moving NW) and Yellowstone (biggest and highest risk) 


Not really a boundary type, rather a surface representation of a mantle plume, causes the production of a chain of islands, can result in massive volcanoes e.g. Yellowstone and Iceland




Divergent: e.g. Iceland (Mid-Atlantic Ridge), the East African Ridge


This diagram probably explains it best. There's only one example of a divergent plate boundary not in the middle of a plate and that's Iceland. It begins with an upwelling of magma in a plume driven by thermonuclear decay in the core, this causes a bulge in land mass. The plume then rises and starts a convection current at the base of the Lithosphere which begins the spreading of the Lithosphere and causes the thinning of the lithosphere. The thinning causes the creation of the valley, lakes form in these. Once the lithosphere becomes thin enough volcanoes form and then a rift, once a rift reaches the ocean it will flood separating the plate. 


Convergent: The writing should be next to the correct diagram, it isn't... my bad? 
Oceanic - Oceanic: e.g. Japan is a mature Island Arc, Aleutian Islands
1. Subduction produces partial melting and the formation of a chain of volcanoes. Produces an island arc. 
2. Build up of intrusive and extrusive igneous material, mixed with sediment forms larger Islands. 
3. The island chains join up and sediments form an accretionary wedge or prism which builds onto the fore arc area. 
4. Hazards - Volcanoes (variety of types), Earthquakes (very powerful) and Tidal Waves
Oceanic - Continental: e.g. Mt Saint Helens, Popcatepetl 
1. Weight of the continental sediments causes subsidence of the oceanic crust.
2. Subduction develops and an island arc forms
3. Compression from plate movement cause the crust to thicken and shorten through folding and thrust faulting. Fold mountain chain is formed e.g. the Andes. 
4. Hazards - Very explosive volcanoes e.g. MSH, Popocatepetl (Mexico City)


Continental - Continental: 
This is the mountain building process (known as Orogeny), the best case study for this are the Himalayas. During continental - continental collision neither plate is subducted instead they are either forced upwards or pushed sideways. 
Hazards = Earthquakes and huge potential for mass movement e.g. Lahars. There are no volcanoes because the crust is too thick.



I have explained this in a very hap-hazard way, for a decent description/explanation go here, they don't have awesome music though... 

Saturday, 5 February 2011

volcanoes

We are now back to volcanoes (: and although todays lessons was not thrilling it was definately a vast improvement upon that of Belfast. We have also been set an essay, nothing like ensuring we don't relax-- it hadnt even been 24 hours after the exam! oh well such as life.


Today was a lesson running through what we were doing before christmas:


There are 2 key types of magma Basaltic and Rhyolitic this is judged upon how much silica (SiO2) is found within the magma, see the table below.


Summary Table
Magma TypeSolidified RockChemical CompositionTemperatureViscosityGas Content
BasalticBasalt45-55 SiO2 %, high in Fe, Mg, Ca, low in K, Na1000 - 1200 oCLowLow


RhyoliticRhyolite65-75 SiO2 %, low in Fe, Mg, Ca, high in K, Na.650 - 800 oCHighHigh


 
  • Hawaiian - These are eruptions of low viscosity basaltic magma. Hawaiian Eruptions are considered non-explosive eruptions.  Very little pyroclastic material is produced.

  • Strombolian - These eruptions are characterized by distinct blasts of basaltic to andesitic magma from the vent. Strombolian eruptions are considered mildly explosive.

  • Vulcanian - These eruptions are characterized by sustained explosions of solidified or highly viscous andesite or rhyolite magma from a the vent.  Eruption columns can reach several km above the vent, and often collapse to produce pyroclastic flows.  Widespread tephra falls are common.  Vulcanian eruptions are considered very explosive.

  • Pelean - These eruptions result from the collapse of an andesitic or rhyolitic  lava dome. Pelean eruptions are considered violently explosive.

  • Plinian - These eruptions result from a sustained ejection of andesitic to rhyolitic magma into eruption columns that may extend up to 45 km above the vent.  Eruption columns produce wide-spread fall deposits with thickness decreasing away from the vent, and may exhibit eruption column collapse to produce pyroclastic flows.  Plinian ash clouds can circle the Earth in a matter of days. Plinian eruptions are considered violently explosive.


i feel there is a good chance i may add to it soon!

Wednesday, 2 February 2011

here are the types of volcano i will write a post to go with them soon!

Tuesday, 1 February 2011

eek! so belfast is finally over me and my panic has left! now time to do that pile of work left with the excuse of i have an exam!

so after watching the age of stupid last night i have brought 2 things out of it:
-firstly, why on earth has this world got a crazy habit of producing something in one country processing it another packaging another then selling it in the country it was produced in! are we thoroughly gone as a species.
Subsistent farming here i come. i think we would all be better off buying areas of green land and having it to grow our own food, LDCs do it so why can't we i think the western world needs to stop thinking they are superior to those who are lessed developed because in fact soon they will be the ones with the advantage as they use low level technology (loving this idea already) grow the majority of their own food in a permaculture or similar idea in their garden and if they don't have it then they just trade within the country.
-Secondly, i have a little bit of a love for the idea of a carbon card, now i can't quite remember how it was metioned within the film as this was me post exam! (brain dead) Anyway, i think it would be awesome if we were to ration carbon, that would surely not only help with global climate change but also lessen the development gap, so if everyone was given an equal percentage of carbon they were allowed to use each year and have it 'credited' to them then everytime we used anything that used a high amount of carbon it would be deducted from our total and once we run out thats it. of course the total amount credited to the world population would have to be under what is considered relatively sustainable as i am pretty sure so corrupt government or western snob would find their way around the scheme. Also the country as a whole would still be emitting carbon and other green house gases into the atmosphere from activities such as industry.

Finally it seems upon discussion in this mornings pre exam work shop that the world would be a better place if everyone had an alpaca in their back garden and a few chicken or perhaps even a street cow!