Romania viewed from above - Carpathians and the Black Sea

Envisat image showing the deep freeze that affected the southeastern Europe in January 2010.
Image source - European Space Agency

Weather in Europe has been very rough recently, so it looks like the year will end the same as it started: cold!  The picture above is from January 25, 2010 and it shows the deep freeze in SE Europe at the time.  The Carpathians are visible in the center left, the Danube Delta is seen in the center of the image, at the edge of the Black Sea.

Geology on 35mm film - Conglomerates

I started going through my old 35mm slide collection representing geological field work from the pre-digital era.  Some of these places I will probably not visit again, at least not anytime soon, so I am bringing them to life with the help of a digital scanner.

The Paleocene rocks in the Southern Carpathians foredeep are represented by poorly sorted, massive, clast-supported conglomerates, which onlap  the crystalline basement.  They consist of angular fragments of schist up to 1m in diameter, as shown in the photo below.

©RomaniaRocks
Calimanesti Conglomerate on Topolog Valley, Southern Carpathians - Romania

The schist fragments are lithologically similar to metamorphic rocks in the Southern Carpathians.  The massive conglomerates grade upward into upward-fining cycles of conglomerate and sandstone, each cycle about 8m thick.

©RomaniaRocks
Upward-fining cycles of conglomerate and sandstone.
Calimanesti Conglomerate, Valsan Valley-Romania.

The upward-fining cycles have a clear erosional base, and the lithology of the clasts are more diverse, consisting not only of crystalline rocks, like lower in the section, but also of sandstone and limestone.

©RomaniaRocks

Calimanesti Conglomearte, Valsan Valley - Romania.

Note the erosional base and fining-upward character.

The sandstone at the upper part of each cycle is medium- to very coarse grained and massive, flat-beddd or cross-laminated.

©RomaniaRocks

Calimanesti Conglomerate, Valsan Valley-Romania. Note the erosional base,  

large fragments of crystalline rocks and the finning-upward character

The conglomerates described above were deposited by overlapping alluvial fans sourced by the Southern Carpathians.  The poorly sorted, angular, coarse textured deposits, with fragments up to one meter in diameter are indicative of debris flow deposits, a common occurrence in alluvial fans.  The Paleocene landscape of Romania was probably not too different than the landscape in the photo below, from the Rocky Mountain National Park in Colorado.

©RomaniaRocks

Alluvial fan at the mouth of a canyon in Rocky Mountain National Park, Colorado.

A hike on top of the fan in the Rockies reveals the size and complexity of the fan.  I bet a hike in the Paleocene in Romania, on top of the Calimanesti Conglomerate would have been somewhat similar, less the ability to use the humans for scale :)

©RomaniaRocks

Close-up view of the alluvial fan in Rocky Mountain Park, Colorado.

Earth as art #1

Photo credit - European Space Agency

Fascinating geomorphology in the Arctic tundra combined with modern technology (multitemporal Advanced Synthetic Aperture Radar), gives this amazing image that rivals the most creative human talent.

Rivers, geology and culture (#1) - Arges, Romania

A river represents the perfect fusion between geology and culture.  Rivers  are characterizesd, generally speaking, both by erosion and deposition; this is where the geology aspect comes from.  Think of the Grand Canyon and you can visualize the results of river erosion through time.  Take a canoe down or up a river, stop on the river bank for lunch and look around; the canoe trip and the lunch break will help you witness river processes, deposition and their resulting features.
Rivers are also amazing "cultural centers", in the sense that human settlements usually started along a river.  Any major city in Europe for example is  associated with a river: Paris-Seine, Vienna-Danube, Frankfurt-Main, Bucharest-Dambovita, Rome-Tiber, and the list could go on...  This is where the cultural aspect comes from.
With this post, I am starting a geological-cultural trip along a river, the Arges River in Romania, to be more precise; I imagine I am a rock particle (or a water molecule) originating from the Southern Carpathians and traveling along the Arges River all the way to the Danube.  The trip will witness some amazing history (geological and human), culture and landscapes.
The Arges River headwaters are located in the Southern Carpathians, between the two highest mountain peaks in Romania: Moldoveanu and Negoiu.

Google map showing the headwaters of the Arges River, located between Negoiu and Modoveanu, the highest mountain peaks in Romania.  Top of the map is towards South.

Geologic sketch of the area around
the Arges River (modified after  Mutihac, 1990). Note that only
the geology relevant to the Arges River is represented in color.
Cn2= Serbota crystalline series; Cn1=Fagaras crystalline series;
Pg=Paleogene; m=Miocene; N=Neogene

The Arges River has its headwaters in the metamorphic rocks of the Fagaras Mountains.  The views are breathtaking, the weather is harsh and as a result, the few motels and chalets that exist in the area function only during the summer.
The upstream part of the Arges River is probably most famous because it parallels the second highest paved road in Romania - the Transfagarasan. The road was built in early 1970's in response to the Soviet invasion of Czechoslovakia. Ceausescu, the Communist President of Romania at the time, wanted to have quick access across the mountains in case the Soviets attempted a similar move in Romania.  The road was built with heavy human (forty people lost their life) and financial sacrifice.
The next posts will take us to the Vidraru lake, then through the most upstream permanent settlements (villages) along the river; this will allow us to explore more geology and culture.

Romania viewed from above - Bucharest

Synthetic Aperture Radar (SAR) multitemporal colour composite image of south-central Romania with focus on Bucharest. Photo Credit - European Space Agency

Bucharest (Bucuresti in Romanian) is the bright area in the center right.  The city lies on the banks of the Dambovita River, and its name comes from Bucur who, depending what legend you take into account, was either a prince, an outlaw, a shepherd or a hunter.
More on Bucharest from the local administration website and the Wiki site. More on Synthetic Aperture Radar here.