Morocco Fieldtrip Recon

I spent a couple of weeks this month in Morocco, the majority of which was scouting out a route for a new physical geography fieldtrip for second year undergraduates at King’s College London. For the last several years the physical geography fieldtrip has been based on the Morocco coast at Agadir and Essaouira, visiting nearby sites. The new fieldtrip will take more of a transect approach, starting in Marrakech, traversing the High Atlas mountains and following the River Draa out to the edge of the Sahara (see map below).


As we work our way up and through the High Atlas one of the things we’ll consider is how vegetation changes and what might be driving those changes. In the picture below you can see colleagues on the trip Prof. Drake and Dr Chadwick (@DrMChad) debating (and betting on!) vegetation on the hills over-looking the town of Demnate.

For example, what are the relative influences of climate and human activity on the vegetation we see? In the picture below Prof Drake confronts one potential disturbance.

As this is a new trip and we’ll be staying in a new location each night, one of our tasks was to check the accommodation we’ll be staying in. Here hotel connoisseurs Drake and Chadwick relax in luxury in the gîte at Toufghine.

There’s some impressive geology in the High Atlas and we’ll discuss that as we go too. The scale of some of the tectonic features is illustrated by Prof Drake in the bottom right of the picture below.

We’ll also be surveying rivers, both their geomorphology and ecology. Another of our tasks therefore was to work out what we would examine and where along the various rivers in the region.

Once we get over the High Atlas and the Anti-Atlas beyond we’ll follow the River Draa all the way to the desert. The Draa is a vital life-line for people in the region, with water drawn from the river used to irrigate agriculture (including wheat).

Once the water has all been used up we reach the desert. There we’ll look for evidence of previous flows of the Draa and of climate change. Some of the dunes can be steep.

But the view from the top is usually good, especially at sunset. We’ll stay a night out in the dunes with the students to get a feel for what it might be like living in such hostile environment.

And of course there will be camels! Below, our driver negotiates a herd as we head back north to Marrakech on the final leg of our trip.

So it looks like we’re going to have a great trip with our students in December and following years! The trip will allow us to investigate how climate, geology, geomorphology, ecology and livelihoods change across space and how they have changed through time.

I’ve posted some more of my favourite pictures on Panoramio so that you can see some of the locations we’ll visit.

Time(-lapse), Environment and Landscape

For the second half of this term I’m teaching the ‘Time, Environment and Landscape’ module of the First year undergraduate class ‘Geography Concepts, Skills and Methods’ at KCL.

Today was my first lecture, on ‘time’. I talked about some of the issues we need to take into consideration when we are collecting data over time, and then how that influences what we can see from the data and how we analyse them (i.e., time-series analysis). To help think through some of the considerations I used some time-lapse movies of landscapes.

I’ve been experimenting with making my own time-lapse videos after getting a remote control for my dSLR last year. In lectures the movies are useful for illustrating how our understanding of things is influenced by the frequency and duration over which we sample our data collection.

As one of the datasets we’ll be analysing in the computer practical sessions that go with the lectures on this module is the Keeling curve, at the outset of the lecture today I showed this movie of some of some Hawaiian landscapes:

Mauna Lapse: From Sea to Summit from The Upthink Lab on Vimeo.

Then, later in the lecture, to get students thinking about how sampling data ‘compresses’ time so that we can see things differently, I showed this movie of the Jorge Montt Glacier in Chile:

Jorge Montt Glacier, Chile (English) TL from Centro de Estudios Científicos on Vimeo.

Finally, we looked at some time-lapse movies I made myself. I show the students different versions of the same video (below) to illustrate how different sampling frequencies combined with different numbers of photos (data points) changes what we can see happening.

Thames Time-Lapse 1 from James Millington on Vimeo.

You can see more time-lapse movies I’ve made in my vimeo album. Once I’ve got enough maybe I’ll try stitching them together with some music like that fancy Hawaii one!

Landscape time-lapse

My blogging’s been quite dry recently. So here’s something more fun. If you like landscape photography, you’ll love this video (expand to fullscreen if you can):

http://vimeo.com/moogaloop.swf?clip_id=10655199&server=vimeo.com&show_title=1&show_byline=1&show_portrait=0&color=&fullscreen=1

Stomacher – Untitled/Dark Divider from Sean Stiegemeier on Vimeo.

There’s some more by the same guy here, and an awesome one of the recent Icelandic volcanic eruptions here.

Autumnal Upper Peninsula


Some pictures from a trip we took to Michigan’s Upper Peninsula earlier this month (fun rather than fieldwork for once).

The road to Paradise (Michigan)

Ship on Whitefish Bay

Whitefish Point, where many ships like that above have foundered.

Arizona’s Ancient Landscape

My landscape interests usually focus on contemporary, biological issues like forest dynamics and human activity. But driving through Arizona’s desert it’s hard not to be impressed by landscape features shaped over geological time scales.

The ancient trees of Petrified Forest National Monument – preserved as quartz crystal moulds of trees buried by sediments before they decomposed – are over 200 million years old.

At that time, in the Late Triassic, northeastern Arizona was located near the equator resulting in a tropical climate and vegetation. The climate and landscape couldn’t be much more different now and the sheer scale of change (both time and location) are hard to comprehend looking out over the desert sunset.

The physical size of the Grand Canyon isn’t much easier to comprehend, even when you’re stood at the very edge of the southern rim.

By the time the Colorado river had begun carving the canyon a mere 17 million years ago, the processes leading to its formation had already been at work for around 2,000 million years (the lowest sediments at the bottom of the Inner Gorge date to around that time). Sunset here is no less timeless than in the Petrified Forest.

Compared with the forest and the gorge the Barringer Crater was created in the blink of an eye. But the 300,000 ton meteor that hit earth 50,000 years ago had probably being travelling on that collision course for a much longer time.

That these awesome features remain – so huge in time and space – reminds us how fleeting our biological landscapes are.

nighthawks

Chicago Skyline
I love the energy of big cities. Sometimes there’s so much it spills over into the early hours of the morning. On a trip to Chicago last weekend we saw Hopper‘s evocative depiction of that straggling energy – when you just don’t want to follow everyone else home to call it a night – in his famous Nighthawks.

Edward Hopper's Nighthawks
I know the feeling, it reminds me of visits to Don Quixote. Not the Don Quixote – Cafe Don Quixote on the Kingsway in London.

Cafe Don Quixote, London
Sometimes the 4am conversation at Cafe Don Quixote was reminiscent of the Spanish Knight; other times it was as lonely as Hopper’s nocturnal scene. But there was always people-watching those other stragglers waiting at the bus stop opposite the cafe, and the warm tea always provided just enough energy to survive the night bus home.

[Nighthawks photo by Mollie E Tubbs]

Cedar Swamps and Deer

Right now I should be back in East Lansing after a week of fieldwork in our Michigan Upper Peninsula (the UP) study area. We’ve been in the UP this last week to finish up on our mesic conifer planting and white-tailed deer density fieldwork that I’ve written about previously. However, an incident with a deer has delayed us (see the bottom of this post) so I’m doing some data entry and writing in Marquette while our Jeep is repaired.


In previous posts about the fieldwork we’ve done in the UP, I have included photos from forest stands containing deciduous hardwood species such as Sugar Maple or American Beech. Generally, it’s understood that white-tailed deer browse juveniles trees in hardwood stands during the daytime in the winter, but shelter overnight in nearby lowland conifer stands. One of the aspects of our project is to identify some quantitative relationships for this behaviour, and so we’ve often had take measurements in the cedar swamps adjacent to northern hardwood stands.


As you can see from the picture above, the density of cedar swamps can make tree measurements a bit tricky. A standard measure of forest stand density (or stocking) is ‘stand basal area’ – a measure of the area occupied by tree stems (i.e. trunks) in a given area. The northern hardwood stands in our study area can have a stand basal area of anywhere between 60 and 100 square feet per acre. Cedar swamps are much more densely populated, with stand basal area values of 280 to 350 square feet per acre. An example of the transition between these stand types is shown in the picture below (click for a larger image).


The high density of the cedar swamps combined with continual cover provided by the evergreen canopy (generally) make winter snow depths lower and winter air temperatures higher compared with the deciduous hardwood stands. The soggy conditions underfoot make surveying cedar swamps even trickier – one has to hop from tree-root island to tree-root island over puddles whilst trying not to impale oneself on the lower branches. Even with care given enough time you’re guaranteed scratches and wet boots.


We’ve completed our fieldwork for now and are just waiting for our Jeep to be fixed after we hit a deer on our last day of work. With so many deer in the area and the high number of miles we drive around our study area, it was only a matter time before we hit one. We were on a major highway and the deer came out of nowhere. We’ve often spooked deer driving on tracks through the forest – it seems to me that when they’re startled they just bolt in whatever direction they happen to be facing at the time. Even if that means running across the road in front of your vehicle. As you can see below, it left quite a dent in the radiator. But Megan did a good job of keeping us on the road and thankfully the only casualty was the deer.