Map: Paris Olympics Purple

I was hoping that this 1874 geological map of the Paris area was the inspiration behind the startling purple color theme for the recently concluded Paris Olympics. The map was shared on X (formerly Twitter) by the Geological Society of London.

The sedimentary strata are folded into an arc that looks like the purple athletics track! 

Alas, no. The purple color was selected because the organizers wanted a unique identity for the games. And apparently it made for better television viewing.

There is a geology connection to the athletics track though. A big component of the flooring is calcium carbonate usually obtained by grinding down quarried limestone. For these games, in keeping with the theme of sustainability promoted by the organizers, the purple track was made up of discarded mussel shells obtained from an Italian fishing cooperative. 

Oh well. I like my geology connection story better.

A Geological Map Of The Himachal Himalaya

Digging through my collection of Himalaya geology papers, I came across this geological map of the Himachal Himalaya. It is from a study on the tectonic history of the Himachal mountains by A. Alexander G. Webb and colleagues, published in Geosphere in the year 2011.

The paper itself is quite a detailed work using both field mapping and various geochemical and geochronologic methods. It will be hard reading and likely incomprehensible for non-geologists. I won't discuss the specifics here. I will however simplify the most interesting findings. 

1) The Greater Himalaya are the tallest of the ranges, and they are made up of rocks which were buried the deepest during the mountain building process. Based on the geometric relationship of the fault zones that contain this rock unit, and the timing of fault activity,  the authors propose a mechanism for the emplacement of these rocks from deeper to shallower levels. 

2) By establishing a chronology and comparing their geochemistry,  rock units displaced by faults and dismembered by tectonics and erosion are shown to have been contemporaneously deposited.

3) There are rare instances of preservation of the depositional contacts between major rock groups. Using this as a guide to their original location and supplementing it with geochronologic information, the pre mountain-building geographic locations of these rock units in relation to the northern shoreline of the Indian subcontinent is proposed. I found this paleo-geographic reconstruction most useful. It really helped clarify my thoughts about the origin and relationships of the different Himalayan sub-divisions.

4) Himalayan mountain building beginning around 35-45 million years ago led to metamorphism of sedimentary layers that were deposited on the northern margin of India. The mineral monazite (phosphate mineral) forms during such metamorphic reactions.  It also contains radioactive elements like thorium which geologists can use to estimate the timing of its formation. Dates of monazite formation from some low grade metamorphic rocks has unearthed an even older phase of metamorphism that affected these rocks.  It shows that the northern margin of India was involved in an earlier phase of mountain building around 500-600 million years ago.

Travelers, do download a high resolution version of this map here - Geological Map of the Himachal Himalaya.

Kangra, Chamba, Manali, Spiti, and Shimla. These are all popular places to visit in the Himachal region. Here are a few tips for a broad understanding of the terrain that you will be driving or trekking through. The descriptions below are by reference to the map legend where all the rock groups are tabulated. 

1) Sub-Himalayan Sequence. These are sedimentary rocks deposited in the Himalayan foreland basin. As the Himalayan mountain building progressed from around 45 million years ago, the crust in front of the rising mountains bent to form a depression.  Debris from this eroding mountain chain was deposited in these foreland basins and then folded and uplifted to form the frontal ranges, including the familiar Siwaliks. Jwalamuki Temple, where a flame is powered by natural gas emanating from deeply buried strata, is located within the Siwaliks. These sub-Himalayan ranges were uplifted between 5 to 0.5 million years ago. Lookout for a lot of sandstone, shale, and pebbly and gravel rich layers.

2) Tethyan Himalayan Sequence. These are low grade metamorphic and sedimentary rocks ranging in age from 800 million to around 70 million years old. The fossil bearing strata that you find in the Spiti valley belong to this group of rocks. The Tethyan Himalaya were the first mountain ranges to form following the India-Asia collision, beginning about 45 million years ago. You will see slates, limestone, sandstone. The older part of this sequence is made up of metamorphic rocks like shiny phyllites and mica schists with garnets.

3) Igneous Rocks. These are of various ages , ranging from 1.8 billion years ago to about 470 million year ago and point to magmatic activity that affected the northern margin of the subcontinent from time to time. The spectacular Dhauladhar range near the town of Dharamsala is made up mostly of granites which intruded the crust around 500-470 million years ago.

4) Greater Himalaya Crystalline Complex. As the name suggests these rocks are high grade crystalline metamorphic varieties like gneiss and schist. They range in age from about 1000 million to 500 million years ago. These were rocks that formed at depths of about 25 kilometers and then were uplifted about 25-16 million years ago. These rocks have a typical banded appearance and contain pink and red garnets and shiny mica rich layers.

5) Tertiary Leucogranite. This granite formed by partial melting of metamorphic rocks during mountain building. It ranges in age from about 40 million to 8 million years ago. You will see them in the higher reaches of the Greater Himalaya. They are easy to spot. Look for white bands cutting across (dikes) dark banded rock. At places the white bands will be parallel (sills) to the rock layers.

6) Outer Lesser Himalaya. These are low grade metamorphic and sedimentary rocks ranging in age from about 1000 million to 500 million years ago. The common rock types will be the familiar slate and limestone.

7) The rest of the Lesser Himalayan units are among the oldest rocks in the Himalaya. The oldest among them, the Munsiari Group, have been dated to about 1.9 billion years ago. They comprise high to low grade metamorphic rocks. Keep a watch for banded metamorphic rocks as well as quartzites and limestones.

The Lesser Himalayan rocks were uplifted between 16 and 5 million years ago.  

8) Indus Suture Zone. If you wander into the Indus valley. These are rocks that formed in the zone of collision between India and Asia. Ophiolites are fragments of the ocean crust thrust up when the Indian plate dove underneath Asia. The Indus Molasse are beds of sand and gravel derived from the erosion of nearby mountain ranges and deposited in lakes and streams.

To briefly summarize the geology. The Greater Himalaya, the Lesser Himalaya, and the Tethyan Himalaya are rock groups made up of sediments that were deposited on the northern continental shelf of India and intermittently intruded by granitic magmas. This sequence developed across a vast time span ranging from 1.8 billion years ago to 70 million years ago. Sediments of the older units of the Tethyan Sequence (Haimanta), the rocks of the Greater Himalaya, and the units making up the Outer Lesser Himalaya were deposited roughly at the same time but at different geographic locales. All these rock units were metamorphosed to varying degrees during Himalayan mountain building. 

Two cross sections from the paper depicts these units restored to their original locations across the Indian margin and then subsequently disrupted by tectonics. 

Compressive forces have deformed this stratigraphy into a complicated structure made up of folded rock sheets stacked by thrust faults. Erosion, by selectively removing portions of these thrust sheets, and by exhuming deeper levels of the crust, has played a big role in producing the present day rock outcropping pattern.

The paper is open access if  you want to dive in. A. Alexander G. Webb et. al. 2011 : Cenozoic tectonic history of the Himachal Himalaya (northwestern India) and its constraints on the formation mechanism of the Himalayan orogen.

Saved By A Projection

I just had to share this wonderfully imaginative piece of science fiction from xkcd comics.

Using map projections to alter our perception of geography is an old trick.

Char Dham Route Landslide Hazard Maps

The Geological Survey of India has published a report of landslide susceptibility along the Char Dham routes being expanded in Gharwal, Uttarakhand. The Char Dham refers to the four holy sites of pilgrimage in the Uttarakhand Himalaya, namely, Gangotri, Yamunotri, Kedarnath, and Badrinath.

The report is available for download - Uttarakhand 2013 Deluge: Landslide Impact on Char Dham Routes

A series of maps of the routes are published showing landslide hazard zones.An example posted here is of the section between Siri and Gangotri

The report focuses on the damage done to the hill slopes due to the deluge and floods in June 2013 where intense runoff and river erosion  caused massive landslides.  But it also states that road building at places has resulted in the development of new landslide loci. That road building is triggering landslides along these routes is obvious judging by the regular reports of new landslides all across Gharwal. This is a well compiled report, but I despair that the advice of geologists and ecologists on the impact this road expansion is having on this part of the Himalaya is being ignored. 

Instead, the GSI has this reassuring tip for travelers: 

"This Coffee Table book will be of immense use for pilgrims passing through the landslide vulnerable tracts leading to the Char Dhams in Uttarakhand".

 Happy Journey!
 

Maps: India Contours

Once in a while I point readers to interesting and useful web mapping applications. Last week, Raj Bhagat Palanichamy, a specialist in GIS and Remote Sensing,  showcased a contour map on his Twitter feed. Intrigued, I found out that the contour map was from a web based application developed by Axis Maps. A detailed blog post explains how they developed the application and the elevation data sources they used to generate the contours. It is quite easy to use, with some controls to set contour intervals, line color, and to depict relief in color shades. 

I am putting a few examples from different Indian terrains to showcase this utility. It is not meant to be a critical review of the app (map scale is missing!), but a fun exploration of its capabilities, and the insights one can get about topography and other aspects of geomorphology and geology. Each example has a contour map on top and a satellite image of roughly the same area in the lower panel. All contours maps have been created using Contours- Axis Maps.

Western Ghats- Edge of the Deccan Plateau: Ghangad, Tail Baila Mesas

The edge of the Deccan Plateau has been deeply dissected to form some stunning relief. Steep sided ridges, mesas, and pinnacles poke upwards from more gently sloping and flattish surfaces. This step like appearance occurs due to the differing styles in which lava flows of varying hardness weather and erode away.  Towards the left-center of the contour map, where the brown meets the darker green, is what appears to be a sinuous thick brown line. It is really an amalgamation of contours, spaced closely, due to the extremely steep slopes and cliffs that make up the Western Ghat escarpment. There is a sudden fall there from the plateau to the coastal plain. Contour interval is 100 feet. 

Himalaya-Tibetan Plateau

Notice how the closely spaced contours in the lower left of the contour map give way to more openly spaced contours towards the top right of the map. This is the transition from the Gharwal Himalaya in to the Tibetan Plateau. The Himalaya, because it receives more rainfall, has more prominent relief, formed by rivers carving deep valleys, and glaciers gouging out rock faces into steep sided, sharp edged mountains. The Tibetan Plateau, although also standing high at around 4500 meters, is in the rain shadow region. It shows less relief. 

This has impacted the geology too. In the Himalaya, the rapid stripping of rock cover over millions of years has exhumed rocks which were once buried 25 kilometers below the surface. In Tibet, lesser erosion has meant that the surface geology is still dominated by 'supracrustal rocks', either volcanic or sedimentary rocks formed at shallow levels of the crust. Erosion has not dug deep down. Contour interval is 500 feet.

Nallamalai Fold Belt- Andhra Pradesh

This map shows the folded ridges of sedimentary rocks formed in the Cuddapah Basin around 1500-1600 million years ago. A fine example of topographic expression giving away the geologic structure of the rocks. Contour interval is 200 feet. 

I would urge those readers who are on Twitter to follow Raj Bhagat Palanichamy's excellent account (@rajbhagatt). He is a mapper par excellence.

Map: The Deep Geological Cycle of Carbon

When I was a kid not so long ago in geologic time, my understanding of how diamonds are created went something like this.

In forests and swamps, large trees grew and died. The wood got buried under more wood and layers of sand and mud. The wood in the bottom layers under the influence of great pressure and higher temperatures got converted first to coal. As burial to greater depths continued, this coal turned first to graphite and then finally to diamond. The story of woody material turning eventually to coal and then to graphite was roughly correct, but this geological path doesn't lead to diamonds.

Most diamonds form at depths of about 150- 200 kilometers. Rarer varieties known as sublithospheric diamonds form even deeper down. The carbon required to make a diamond is transported from the earth's surface to those depths by a subducting plate. Subduction is the process whereby an oceanic plate made up of dense Mg and Fe rich rocks sinks into the mantle. The Marianna trench for example marks the place where the Pacific plate is sinking underneath the Japan Plate. Why can't coal then move into the mantle this way? It doesn't because coal deposits occur in continental settings where the crust is made up of much lighter rocks richer in Si, Al, Na and Ca. This continental crust is buoyant and does not subduct into the denser mantle. So there is no way for coal that began its journey in ancient river floodplain, bogs, and swamps to get directly transformed into diamonds.

The denser oceanic plate contains carbon from a variety of sources. The lower layers of the oceanic plate is made up of a Mg rich rock known as peridotite. Occasionally, faulting may bring this peridotite to shallower levels where it interacts with sea water and gets transformed into a rock known as serpentinite with calcium carbonate minerals also forming alongside. Carbon is trapped in minerals like calcite and dolomite. The upper layers of the ocean plate is made up of the volcanic rock basalt. It too interacts with sea water, with calcite precipitating in rock cavities. This becomes another source of carbon.

Then there is carbon which is part of the shells and skeletons of planktonic marine creatures. These tiny photosynthesizing organisms which live in the sunlight zones of the ocean precipitate a calcium carbonate skeleton. When the organism dies, these carbon containing skeletons sink and blanket the sea floor. This source of carbon is a relatively late addition in geologic history. Calcareous nanoplankton first appeared in the early Mesozoic, some 225 million years ago. Organic tissue of marine creatures can also get buried, making this another carbon source. And finally, carbon coated sediment washed into the ocean by rivers and then transported into abyssal depths by deep sea currents contribute some carbon to the oceanic plate.

Each oceanic plate has its own selection from this carbon menu, depending on its unique geologic history. For example, calcium carbonate starts dissolving below a depth known as the calcite compensation depth. Sea floor below this depth doesn't retain much skeletal debris. Or, oceanic crust that formed in the Cretaceous contains abundant calcite in veins and vugs, likely because the warmer Mesozoic oceans promoted calcite precipitation on the sea floor.

This beautiful map shows several subduction zones. In the map, SedCarb refers to skeletal carbonate, SedOrgC to organic carbon, AOC Carb to carbonate in altered oceanic crust, SerpCarb to carbonate in serpentinite rocks. The major source of carbon is identified by a particular geochemical signature. Mineral carbonate for example has higher amounts of the heavier isotope of carbon (C13), while carbon that makes up organic tissue is much richer in the lighter isotope (C12).

  Source: Terry Plank & Craig E. Manning: Subducting Carbon

As the oceanic plate subducts carbon begins to get removed from the plate. Some carbon is removed when the sediment and altered oceanic igneous rocks are scraped off and plastered on to the sea floor. Such deposits made from scraped off sea floor are called accretionary prisms. They often poke out above sea level to form island chains. The Andaman Islands is an example of an accretionary prism that is made up of mechanically removed slices of the subducting Indian oceanic plate.

At greater depths, sediments and oceanic crust begins to be metamorphosed under higher temperatures and pressures resulting in the loss of carbon dioxide and water. This carbon dioxide makes its way into the overlying mantle and gets incorporated into magma. The spectacular volcanic eruptions along Japan, Indonesia, Caribbean and the Western North American coastlines are a result of the rising and depressurization of such volatile bearing magma. Some of the carbon in the belched out carbon dioxide has come from the burning of skeletons of marine organisms in the deeply buried plate underneath these volcanic systems.

A quantity of carbon does remain in the downgoing plate and reaches depths of 150-200 kilometer or more. The igneous rocks of the subducted plate gets altered to a dense rock known as eclogite. And at these temperatures and pressures, diamonds may form within these eclogites along carbon dioxide or methane rich domains. The subducting slab is also releasing some trapped carbon along with other volatiles which infiltrate the surrounding mantle. Diamonds can form in such metasomatized or fertile regions of the mantle as well. The main host rock here is peridotite. Subducted carbon is one source of carbon for diamonds.

Geologists think that primordial carbon retained in the mantle from when the earth formed may also be finding its way into diamonds.

Multiple sources perhaps, diamond forming chemical reactions can be summarized simply as driven by the reduction of carbon sourced from either carbon dioxide or methane.

CO2 = C + O2

CH4 + O2 = C + H2O.

From eclogite and peridotite parent rocks, diamonds are transported to the surface by an unusual magma type known as kimberlite and even less commonly by lamproites. These magmas are rich in volatiles like water, carbon dioxide, fluorine and chlorine and are also rich in magnesium. They are generated at the base of thick continental plates generally during episodes of continental fracturing. The volatile rich magma physically disaggregates diamonds from their parent rocks and carry them as they ascend through deep continent penetrating cracks with amazing speed, traveling 200 kilometers in a matter of hours, bringing to the surface its tiny but dazzling prize. The block diagram below summarizes the geological environments of diamond formation and their ascent.

Source: Steven B. Shirey et. al., Diamonds and Geology of Mantle Carbon; modified from Tappert R and Tappert M 2011.

The famous Panna diamonds from Bundelkhand in Central India came to the surface in a kimberlite magma eruption around 1 billion years ago. It is possible that its source carbon was transported from the surface to diamond forming depths hundreds of millions of years earlier, perhaps during the convergence and assembly of an earlier supercontinent.

Diamonds are often older than their host kimberlites by hundreds of millions to billions of years. During diamond growth, other minerals get trapped inside them as micro-inclusions. Their composition is therefore a record of the fluid chemistry of the mantle and the carbon cycle as it existed in deep time, billions of years before present.

Diamonds are one component of the deep geological cycle of carbon. We are familiar with the exchange of carbon between the atmosphere and the biosphere. Carbon is transferred to and fro in this system on a timescale of days to years to hundreds of years, but not much more. Longer geological sequestration of carbon occurs at shallower levels of the crust too. Soil can store carbon for thousands of years. Carbon can get trapped for millions of years in carbonate minerals that make up limestone and also in coal and oil. It is this shallow crustal carbon cycle that we are breaking by burning limestone and fossil fuels.

The deep geological cycle can take carbon from the surface and keep it in the mantle for hundreds of millions of years. The mantle releases it through sustained volcanism thus modulating earth's climate on long time scales. And occasionally as a return gift it throws up a few diamonds as well. 

Mapping: In Praise Of The Triangle

Jerry Brotton in his book A History Of The World In 12 Maps writes about France's National Map Project. Begun around the 1670's upon the establishment of the Academie de Sciences and the Paris Observatory and headed by the astronomer Cassini I, it first attempted to create an accurate geodetic survey of France using the latest surveying instruments. At the heart of the survey was the calculation of distances and directions using the method of triangulation. Latitude was calculated using a quadrant that measured the altitude of celestial bodies. Then, using a measuring stick, a baseline of a known length was established. A third point on the landscape was sighted. The angles between the three control points were measured. Using trigonometric tables the lengths of the remaining two sides of the triangle could be calculated.

I liked this passage:

In 1744 the survey was finally completed. Its geometers had completed an extraordinary 800 principal triangles and nineteen base lines. Cassini III had always envisaged printing regional maps as they were produced, and by 1744 the map was published in eighteen sheets. Its new map of France, on an approximately small scale of 1: 1,800,000, shows the country represented as a network of triangles, with virtually no expression of the land's physical contours,and with large areas such as the Pyrenees, the Jura and the Alps left blank. It was a geometrical skeleton,a series of points,lines and triangles following coasts, valleys and plains in connecting key locations from which observations were carried out. Over it all lay the triangle, the new immutable symbol of rational, verifiable scientific method. On Cassini III's map the triangle almost takes on its own physical reality, a sign of the triumph of the immutable laws of geometry and mathematics over the vast, messy chaos of the terrestrial world. The Babylonians and the Greeks had revered the circle, the Chinese celebrated the square, the French now showed that it was the application of the triangle that would ultimately conquer the earth.

Cassini III was the grandson of Giovanni Domenico Cassini (Cassini I). The directorship of the Paris Observatory remained in the Cassini family over four generations.

This surveying method was quickly adopted and adapted by others. The Ordnance Survey began mapping the British Isles using this method in the late 1700's.  William Lambton took the Ordnance Survey's acquired expertise and began the Great Trigonometrical Survey of India in the year 1800, a feat that took nearly 50 years to complete. John Keay's book The Great Arc details that mammoth effort.

Field Photos: Glacial Deposits Of The Darma Valley, Kumaon Himalaya

During my recent trek to the Panchachuli Glacier in the Kumaon Himalaya, I obsessed about observing changes in metamorphic grade of the Greater Himalayan Sequence on the trek route and also about finding the South Tibetan Detachment fault system. I wrote about this in an earlier post.

But there were other interesting geological observations too. The Panchachuli Glacier has left a thick record of glacial deposits. The river Dhauliganga originates from this glacier. Along this river valley, glacial deposits can be observed to a distance of at least 5 kilometers downstream of the present location of the snout of the glacier, indicating that the glacier was much more extensive in the past. Tributary glaciers flowing out of the ranges east of the Dhauliganga have also left an extensive record in the form of thick fluvio-glacial deposits. These can be observed as far south as the village of Baaling.

We heard anecdotes in village Dugtu about how this glacier was much bigger in living memory and how it has been receding rapidly in the past few decades. On one level such stories are believable because studies of Himalayan glaciers have shown that many of them have been shrinking over the past few decades (ref). This is partly due to anthropogenic global warming, but glacial response to warming may be varied due to local variations in topography, precipitation and wind conditions. Some glaciers don't show retreat while some are actually seen to be expanding. Overall though, there a substantial ice loss observed across the Himalaya. Exactly how much of that is due to recent global warming and how much, as some scientists caution, due to natural factors is still being studied. Sustained warming though will cause these glacier to shrink further over the next century.

There is also a longer geological story of glacial advance and retreat written in these deposits.

I've embedded below an annotated interactive map of the glacial deposits of the Dhauliganga river valley in the Panchachuli Glacier area. This will enable readers to zoom in and recognize the various glacial landforms present in the valley. You can also access it via this Permanent Link.



The annotations depict:

a) The dark blue lines are the snout of the glacier.
b) The light blue lines are the recent terminal moriane fields.
c) The pink lines are older lateral moraines.
d) The yellow lines are outlines of older fluvio-glacial deposits
e) Numbers 1 -12 mark the locations of glacial deposits.

I have mapped only a few representative examples of each of the feature types. Readers can use these to explore similar features scattered throughout the valley. 

Location 1: This is the snout of the glacier. It is a mass of ice and frozen mud. The river Dhauliganga emerges out of an ice cave.

Location 2: Taken from near the snout of the glacier looking downstream. Ridges of the terminal moraine can be seen in the foreground. The arrows in the background outline a ridge of an older lateral moraine. Notice how the ridge decreases in elevation downstream suggesting that the terminus of this older glacial phase in somewhere nearby downstream.

Location 3: The older lateral moraine can be clearly seen as a sharp ridge line (arrow) separated from the valley wall by a depression. 

This moraine top is a few hundred meters above the valley floor implying that the glacier was thicker in the past. When was this lateral moraine deposited? It may be at least a few hundred years old. In the Garhwal Himalaya, similar older lateral moraines close to the glacier has been dated to be several hundred years old. They have been interpreted to be a result of glacial growth and deposition during the Little Ice Age, a period of earth cooling and climate instability that lasted from around the 1300's to the mid 1800's (for more on this climatic episode, I recommend Brian Fagan's book The Little Ice Age: How Climate Made History 1300-1850).

Location 4: A view of the glacier and an older lateral moraine (arrow) on the other side of the valley.

Location 5: Further downstream are thick glacial deposits. The river has incised or cut through these sediments. As a result the deposits form flattish plateaus or terraces that hug the mountain slopes. Village Dugtu, where we stayed, has been built on top of one such glacial terrace. The arrow in the top picture points to an exposure of these glacial deposits. A close up of this deposit is seen in the bottom picture. Notice the extremely ill sorted texture. Such ill sorted sediment deposited by glaciers is called Till. Large boulders are mixed in with  gravel, pebbles and much finer sized rock flour (the light to brown colored matrix).

Location 6: Another exposure of a glacial deposit near Dugtu. Again, notice the ill sorted deposit. However, at the top is a well sorted pebbly layer. This suggests deposition in more vigorous flowing water. Glacial retreat from time to time would have resulted in the establishment of a fluvial regime and deposition in these streams. These deposits may be a few hundred to several thousand years old.

Location 7: The glacial terrace on which village Dugtu is built is seen in the lower right corner. Farther away is village Philam built on the thick fluvio-glacial deposits of a tributary glacier originating in the range east of Dugtu. At village Dugtu, the east flowing river Dhauliganga makes a sharp southerly turn. The river has cut through these deposits and the slopes of the valley are thickly forested suggesting the great antiquity of these deposits.

Location 8: A nice view of glacial deposits south of village Baun along a smaller tributary of the  Dhauliganga. Notice the waterfall!

Location 9: A walk right through these thick fluvio-glacial deposits along a forested section of the valley slope. Again, notice the ill sorted nature of the deposits. Glacier are viscous and cannot sort sedimentary particles like water or air can. The result is a jumble of boulder, gravel and rock flour.

Location 10: Another cliff made up of fluvio-glacial deposits. I'm calling the deposits east of Dugtu as fluvio-glacial, since I observed intervals which show layering. This suggest deposition in water, either in streams or in melt water lakes and ponds that form in front of glaciers.

Location 11: A thick sequence of fluvio-glacial deposits along the Dhauliganga river. If you zoom and pan the satellite image you can recognize these terraces  southwards almost up to the village of Baaling.

I did not observe such deposits south of Baaling. However, there are smaller glaciers, such as the Naagling glacier, originating in the ranges on either side of the Dhauliganga. There would be smaller deposits scattered in these tributary valleys.

I have been vague about how old these deposits could be. If we assume that the Panchachuli glacier would have attained its maximum extent in the Pleistocene during the Last Glacial Maximum about 20,000 years ago, then the deposits furthest away from the present location of the glacier would be the oldest. As the glacier recedes one should find younger and younger deposits closer to the active glacier.

A study by Dirk Scherler and colleagues in the Garhwal Himalaya found such a pattern. They studied deposits of the prominent Jaundhar Glacier and the Bandarpunch Glacier in the Tons Valley. I've posted below a map showing the interpreted ages of deposition of glacial sediments.

 Source: Scherler et. al. 2010

Notice how the oldest deposits are further away from the present location of the glaciers (eastern most extremity of the map). These oldest deposits point to the maximum extent of the glacier that was reached in the Pleistocene during the Last Glacial Maximum.  However, the decreasing ages of the deposits upstream aren't the result of a uniform recession of the glacier. Instead, they point to several glacial episodes during which the glacier advanced, then receded, and then advanced again during the Holocene. Their data shows five such episodes of glacial growth dated to approximately 16 ka (ka = thousand years ago), 11-12 ka, 8-9 ka, 5 ka and less than 1 ka.


It turns out that the climate history of the Holocene is not one of uniform warming since the end of the last glacial period. The earth has gone through several minor cooling phases during the Holocene. The well known Younger Dryas Event around 12.9 -11.7 ka is one example.  Some studies suggest cooling episodes around 8.2 ka  and around 4.2 ka . And there is the Little Ice Age during the last millennium.

Another climate dynamic is fluctuating monsoon strength through the Holocene. The authors don't favor the explanation that these periods of glacial growth were triggered by global cooling events.  They argue that glacial growth corresponds to small phases of increased monsoon strength interrupting a longer trend of decreasing monsoon strength. More moisture means more snow and glacial growth. Since the long term trend in this part of the world is one of decreasing monsoon strength, every successive phase of glacial growth was smaller than the previous, resulting in younger and younger deposits upstream. The Little Ice Age deposits (which were likely driven by global cooling and not necessarily increased precipitation) mark the last major phase of glacial growth.

How are these deposits dated? Scherler and colleagues use a technique known as cosmogenic nuclide dating. This technique is one way to date the timing of surface exposure. Glaciers carry rock debris. These form a layer below the moving ice. When the glacier recedes the rock debris is deposited as a moraine or as an erratic boulder. It is exposed to the atmosphere and starts getting bombarded by cosmic rays. Energetic cosmic ray neutrons falling on atoms of minerals like quartz results in spallation reactions. This means that the collision of neutrons is energetic enough to fragment the nucleus. Oxygen bound up with silicon in the mineral quartz gets converted to an isotope of Beryllium (10Be). The amount of nuclides generated this way is proportional to the length of exposure. By measuring the amount of 10Be and comparing it with other isotopes, an 'exposure age' is estimated. This is essentially the age of glacial recession and the deposition of glacial sediment.

Samples have to been selected carefully for this method to give a true estimate of surface exposure and deposition. Care must be taken to avoid sampling rocks that have been repeatedly buried and exposed. Rocks which show signs of being subjected to prolonged glacial erosion are selected since  erosion will remove outer shells of material that may have accumulated nuclides during an earlier period of exposure.  Debris with a polished surface or with striations and grooves generally suggest subglacial transport and prolonged glacial erosion and are preferred samples.

 The figure below taken from the same study shows the reconstructed glacial extents using exposure dates of the moraine sequences in the upper Tons Valley.

Source: Scherler et. al. 2010

Such dating of glacial deposits at other locations in the Garhwal Himalaya (ref) tell a similar story of glacial growth and decay over the Holocene. And what about the Pleistocene? Is there evidence of older glacial cycles in the Himalaya? There are many studies that have identified glacial phases during the Pleistocene as well. For example, in northwest Garhwal, the Bhagirathi Glacial Stage has been dated to 63 ka (ref). And in the Ladakh Himalaya the oldest glacial stage has been dated to 430 ka (ref). Pleistocene ice ages have impacted glacial dynamics in the Himalaya too although more work needs to be done to understand the specific mechanisms of glaciation.

Location 12: Its back to the Dhauliganga valley floor. This moraine ridge (arrows) may be the remnant of an older terminal moraine. It is located about 2 kilometers downstream of the glacier.

The Panchachuli and other glaciers in the Kumaon region to the east of the Garhwal will also have their own history of past glory and recession. How much of the retreat of the Panchachuli and other Kumaon glaciers due to recent global warming?  And what is its fate? Hopefully, someone will study them with more precision in the future.

Exploring India's Paleogeography And Fossils Using The Paleobiology Database Navigator

I was directed to the Paleobiology Navigator by a tweet from @avinashtn .

Great fun! The Paleobiology Database is being maintained by an international non-governmental group of paleontologists. Contributing members add to it fossil occurrences from scientific publications.  The Paleobiology Database Navigator is a web mapping application managed by the University of Wisconsin-Madison that allows you to explore the geographic context of these fossil locations. You can filter the data based on age, taxonomy and geography. You can also generate diversity trends for the selected set.

I played around a bit with India specific fossil locations.

Paleozoic versus Mesozoic Basins

The figure below shows the distribution of fossil localities for the Paleozoic Era. India is shown as it is today and in its Paleozoic geography.

Source: Paleobiology Navigator

You can clearly see that fossils in Peninsular India are predominantly located in one narrow band in the center and east of the country. These are the Permian Gondwana basins. They are, starting from the westernmost and going eastwards, Satpura Basin, Son Valley Basin, Damodar Valley Basin and the Ranjganj Basin.  These are continental interior basins comprising river, lake and swamp environments. Most of India's coal deposits come from these basins. These basins are rich in plant fossils, and reptile and amphibians remains.

Now take a look at India's geographic position (arrow) during the Permian (298-252 million years ago). Peninsular India occupies an interior location within Gondwanaland, far away from any ocean. Tectonic stability through most of the Paleozoic meant lack of crustal movements. During this time, peninsular India was an erosional landscape until the Permian basin formation in the east.

The one Paleozoic fossil location in Rajasthan shown here represents early Permian marine sediments formed by the flooding of the western region by an arm of the Tethys sea.

And this database has still not added one important fossil location. This is the early Cambrian age locality near Jodhpur where sediments of the Nagaur Group are exposed. They contain trilobite trace fossils.  No basin development and sedimentation took place in Peninsular India from Mid-Cambrian to Permian times (530 million years to 298 million years). 

In contrast, look at the northern edge of India, where the Himalaya stand today. That margin was submerged under the Tethyan ocean. A thick pile of marine sediment accumulated right through the Paleozoic, forming the fossil rich Tethyan Sedimenary Sequence of the Himalaya.

Continental configurations changed in the Mesozoic (252 million to 66 million years ago). The figure below shows Mesozoic fossil locations and the Cretaceous paleogeography of India.

Source: Paleobiology Navigator

There is now a wide swath of fossil localities across Peninsular India. The dotted lines trace important linear depressions where sediments were deposited. The east west oriented Narmada rift zone (NRZ; Jurassic and Cretaceous) and the NW-SE oriented Pranhita Godavari zone (PGR; Triassic to Cretaceous) are important fossil repositories.  The eastern India basins continued accumulating sediment. To the west are the basins which formed in Gujarat and Rajasthan (Jurassic and Cretaceous). The Kutch rift (KR) is outline by dotted lines. And to the south east in Tamil Nadu, marine flooding of the eastern continental margin in the Cretaceous resulted in the deposition of richly fossiliferous sedimentary sequences.

All these basins ultimately owe their origin to the forces exerted on the crust as India pulled away (arrow) from Gondwanaland.  Seaways formed along these rifts and crustal depressions. The Mesozoic, especially the Jurassic and Cretaceous, was a time of global high sea levels. The western margin saw marine incursions from the nascent Indian Ocean, while the eastern margin was submerged by the waters of the newly formed Bay of Bengal.  River and lake systems also developed in more continental interior locations. The northern margin (Himalaya) was mostly a marine environment through the Mesozoic.

Marine versus Continental Interior Basins in Mesozoic Central India

The distribution of terrestrial organisms versus marine organisms can tell us about the extent of marine flooding into Peninsular Central India in the Mesozoic.

I created these maps by using localities of dinosaur fossils (above) to map the distribution of terrestrial sedimentary environments. I used localities of invertebrate marine organisms, namely,  brachiopods, echinoderms and ammonoids  to delimit the extent of marine environments along the Central Indian basins (below).

 Source: Paleobiology Navigator

You can see that terrestrial environments were present right across the Narmada rift zone, the Pranhita Godavari rift basin and in the western Indian basins also. In the western basins, some of the dinosaur fossils have been found in marginal marine settings comprising coastal and estuarine environments.

Deeper water marine environments as evidenced by brachiopod, echinoderm and ammonoid localities are however restricted to Gujarat, Rajasthan and western Madhya Pradesh. The Cretaceous Bagh Beds in Madhya Pradesh is the eastern most limit of Mesozoic marine flooding into Central India. Seaways did not extend into eastern parts of the Narmada rift basins.

Global and Indian Dinosaur Diversity Patterns

I used the Stats tool to create graphs of dinosaur diversity. The number of Genus per Stage is being used as a measure of diversity. Geologic time is subdivided in to bins. An Age is a bin spanning a few million years. Stage represents rock layers deposited in an Age. So, a diversity measure has been created by counting the number of dinosaur genus reported from successive bundles of rock layers, each representing a few million years of time.

Source: Paleobiology Navigator

The global diversity pattern shows episodes of diversification and decline in the Triassic, Jurassic and the Cretaceous. There appears to be a trend of increasing diversity through time with peak diversity in the Mid-Late Cretaceous. The Late Cretaceous extinction of dinosaurs forms the right side boundary.

The diversity measures in India show some differences with global trends. The number of Genus sampled are less. This is due to regional versus global sample. A smaller locale will generally have less of the total observed variation. The trends in diversity with time also is different from the global trajectories. There are a couple of reasons for this. First, this is a preservation artifact. Mesozoic terrestrial basins in India were receiving sediment only episodically. Depositional phases were interrupted by erosional hiatuses. Rock sections thus have been removed as well.   There was little to no sedimentation from Mid-Jurassic to Mid-Cretaceous in the Narmada rift basins. Hence, no fossils either. The lost diversity from this interval is irretrievable.

The second reason gives more hope. A couple of years ago, Dr. Dhananjay Mohabey of the Geological Survey of India gave a talk in Pune on Late Cretaceous dinosaurs of India. He mentioned that there are roomful of dinosaur fossils in government archives that are yet to be studied and catalogued. There is scope then to enhance our understanding of at least late Cretaceous dinosaur diversity of India.

I have barely scratched the surface. There are many more stories and patterns and trends in the Indian fossil record waiting to be teased out from this database. Dive in!

Map: Thickness Of The Crust

A ten km contour interval? Well yes, if  you are mapping the thickness of the earth's crust!

This map brings out beautifully the distribution of the two distinct types of crust on earth. Crust making up the continents is granitic to andesitic in composition, buoyant and is old. Crust making up the ocean basins is mafic in composition, gravitationally unstable (it is heavier and it subducts) and is young.

The 30 km contour outlines roughly the continental crust:

I got this from - The Continental Record and the Generation of Continental Crust (open access)

How does the earth look in terms of its topography? There is a bimodal distribution of the surface elevations on earth. This is a consequence of the contrasting chemical-mechanical properties of the continental and oceanic crust. The figure below brings out the distribution.

Why is there some continent  below sea level? Plate tectonic configuration can be such that at different coastlines continents could be in the act of converging with an oceanic plate. Or, having long broken away from another continent, they posses a passive or divergent margin. At such passive margins, continental crust does not end at the present day coastline, but extends further out until the edge of the continental shelf where there is a sudden deepening of the sea floor. That is roughly where the ancient continent broke up. As it drifted away, new oceanic crust formed between its conjugate continent on the opposite side. Sea level rise after the last glaciation has flooded continents, thereby submerging portions of these passive margin low gradient shelves.

Source: The Continental Record and the Generation of Continental Crust.

Sometimes, a single map or a graph can bring out a fundamental truth about the making of the earth.

Early Chinese History Told Through Maps And Poetry

I am really enjoying Jerry Brotton's A History Of The World In 12 Maps. One richly rewarding chapter is on early Chinese map making traditions and inevitably you end up learning quite a bit of history as well.

The Song dynasty (907- 1276 AD) struggled with keeping the empire unified and intact and faced particularly strong challenges from the Jurchen Jin a confederacy of Tungusic tribes from northern Manchuria. In the middle of the 12th century the Song were forced to sign a peace treaty with the Jurchen Jin ceding to them nearly half their northern territory.

Subsequent imperial maps drawn up by the Song never showed this division. Rather, an idealized geography that the Song kept dreaming of based on earlier classical texts like Yu Gong, that of a unified empire to which foreign barbarian rulers paid tribute was portrayed. Using maps as a tool for political propaganda is an old trick! 

What maps did not depict though, poetic license did.

This beautiful passage from the book:

Poetry describing maps either side of the traumatic division of the Song also captures their power to first acknowledge, and then lament the loss of territory. Writing more than 100 years earlier, the ninth century Tang poet Cao Song describes 'Examining " The Map of Chinese and Non Chinese Territories"':

With a touch of the brush the earth can be shrunk;
Unrolling the map I encounter peace.

The Chinese occupy a prominent position;
Under what constellation do we find the border areas!

On this occasion the almost meditative act of unrolling the map and seeing a unified Chinese dynasty at its center evokes emotions of security and assurance. Later Southern Song poets used a similar conceit, but with very different emotions. Writing in the late twelfth century, the celebrated Lu You (1125-1210) lamented:

I have been around for seventy years, but my heart has 
remained as it was in the beginning, 
Unintentionally I spread the map, and tears come gushing forth.

The map is now an emotive sign of loss and grief, and perhaps a 'template for action', a call to unite what has been lost.

On The Consequences Of A One To One Scale Map

 My Book Shelf # 30

I have just started reading A History Of The World In Twelve Maps by Jerry Brotton, an exploration of influential maps through our history that shaped the way we viewed the world and in turn how our cultural habits, religious beliefs and political power equations of the day shaped decisions of how and what to represent. Each period in our history argues Jerry Brotton gets the map it deserves. It promises to be a really interesting read.

Early in the introduction I came across this passage on the use of scale:

The only map that can ever completely represent the territory it depicts would be on the effectively redundant scale of  1:1. Indeed, the selection of scale, a proportional method of determining a consistent  relationship between the  size of the map and the  space it  represents is closely related  to the problem of abstraction, and has been  a rich source of pleasure  and  comedy for many writers. In Lewis Carroll's Sylvie and Bruno Concluded (1893), the other worldly character Mein Herr announces that 'we actually made a map of the country, on a scale of  a mile to the mile!' When asked if the map has  been used much,  Mein Herr admits, 'It has never been spread out'. and 'the farmers objected: they said it would cover the whole  country,  and shut out the  sunlight! So we now use the country itself, as its own map, and I assure you it does  nearly as well.' The conceit was taken a stage further by Jorge Luis Borges,  who, in his one-paragraph short story 'On Rigour in Science' (1946), recast Caroll's account  in a darker key. Borges describes a mythical empire where the art of mapmaking  had reached such a level of detail that 

the Colleges of Cartographers set up a Map of the Empire which had the size of the Empire itself and coincided with it point by point. Less Addicted to the  Study of Cartography, Succeeding Generations understood that this widespread Map was useless and with Impiety they abandoned it to the Inclemencies of the Sun and of the Winters. In the deserts of the west some mangled Ruins of the Map lasted on, inhabited by Animals and Beggars; in the whole Country there are no other relics of the Disciplines of Geography.

Borges understood both the timeless quandary and potential hubris of the mapmaker: in an attempt to produce a comprehensive map of their world, a process of reduction and selection must take place. 

Wonderful passage! (but i wonder not having  read the story -if the map was as large as the empire, where did they keep it? :) )  If you want a shorter summary of the book do listen to Jerry Brotton on BBC Pop-Up Ideas podcast -  Mapping History. It is an enjoyable talk.

Now,  back to reading!

When California Was An Island And Other Stories

Economist Tim Harford is hosting a fun podcast series on BBC Pop-Up Ideas. There are 3 episodes on maps which make great listening:

1) Tim Harford- The Power of Maps

2) Jerry Brotton - Mapping History  He is the author of the book A History Of The World In 12 Maps which is definitely of my reading list.

3) Simon Garfield- Maps And Mistakes.. which tells us the story of how in the late 1600's California became an island on the maps of the day..

Very fun to listen to..

What A Porphyry Copper Ore Body Tells Us About How India Was Assembled

Nature Geoscience has some interesting articles on giant magmatic ore deposits  ( 1 , 2 ) with a focus on porphyry copper- molybdenum deposits which occur within magmatic arcs above subduction zones.

Ever since I found that copy of Tyrrell I've been reminiscing a bit about my early days in geology. These papers on copper ores started another chain of thought. We were preparing for our first year M.Sc. field trip which is really supposed to be a tour to learn field mapping. So the area selected is usually one where rock bodies are exposed clearly, have lateral continuity, where relations and contacts between geological units can be observed, basically an area where principles of field mapping are relatively easy to learn. As it happens our department at Pune University had gotten a big grant from ONGC to do a reconnaissance of Gondwana rift basin sediments of Carboniferous-Permian age just north of Itarsi in Madhya Pradesh. Our department chair organized our field trip to this area, reasoning that we could use this for training as well as contribute to the project.

Unfortunately, it was a disaster. The area was thickly forested, rock exposures limited to few stream cuttings and occasional road cuts, just not what you want for a rigorous training in mapping. The one bright spot was the copper mine we visited at Malanjkhand. This is an open pit mine.

Google Interactive Map of Malanjkhand Copper Mines:


View Larger Map

We were allowed to walk right up to the exposed walls of the pit and observed the stringers of copper and molybdenum sulphide ore embedded in networks of quartz veins. The host rock was a granodiorite. It was altered to various clay assemblages but you could make out blobs of relatively unaltered textures. Overall, after two weeks of tramping through forests it was great to be looking at massive walls of rock and glistening ore!

Ok, so what does this copper ore body have to do with ideas of how India was assembled and what does that even mean?

Interactive Geologic Map And Cross Section Of Kumaon Lesser Himalayas In Shama Gogina Region

This has been pending. As I posted earlier this month I returned from a trek in the Kumaon Himalayas along the Ramganga river in the Namik Valley just west of the town of Munsiyari in Pittorgarh district. The terrain is mostly the Lesser Himalayas made up of the Lesser Himalayan Sequence (LHS) composed of  late Proterozoic to early Palaeozoic metasediments.

The red line on the map below shows my location with respect to the regional Lesser Himalayan structure and stratigraphy.

Source: Celerier et. al. 2009

A quick recap of the geology:

Trekking Amongst The Stratigraphy And Structure Of Lesser Himalayas In Kumaon And Gharwal

(Update November 29 2012: See my new post on the geology I saw on this trek!).

Yes.. I know Geology Map Day was last week, but although late, I have put up this map and a schematic cross section... I'm leaving on a hiking trip to the Kumaon Himalayas and have been reading up on the geology of the area. After many years of being confused about the stratigraphy and structure, I finally got some clarity on Lesser Himalayan geology reading some recent work. The paper that helped me most was:

The Kumaun and Garwhal Lesser Himalaya, India: Part 1. Structure and stratigraphy- Julian Celerier et. al. 2009 GSA Bulletin

and its companion paper

 The Kumaun and Garwhal Lesser Himalaya, India. Part 2: Thermal and deformation histories

Two other papers also were quite useful:

1) Patel, R.C. and Carter, Andrew (2009) Exhumation history of the Higher Himalayan Crystalline along Dhauliganga-Goriganga river valleys, NW India: new constraints from fission track analysis. Tectonics 28

2) Revisiting Central crystallines in Pindar and Ramganga valleys, Kumaon Hills,Uttarakhand – an expedition based case study - Geological Survey of India Mapping Report. The report describes the lithologies very near my trek route along the Ramganga river sourced from the Namik glacier, near the village of Namik.

Base camp for the trek is going to be a campsite on a ridge across the small village of Tejam. Looking at geological maps I found out that I am going to be in the Lesser Himalayas, but very just south of the Main Central Thrust which structurally juxtaposes the Greater or High Himalayas over the Lesser Himalayas. The first paper I mentioned by Celerier et.al. explains quite well the stratigraphic and structural evolution of the Lesser Himalayas.

A quick recap:

The Most Divisive Maps In America

More on the art and science of map making. This time it is Robert Draper in The Atlantic writing about the history and politics of gerrymandering:

....as works of art, redistricting maps continue to evoke a crazed but symbolically rich dreamscape of yearnings, sentimentality, vendettas, and hyper-realism in American political life. Districts weave this way and that to include a Congress member’s childhood school, a mother-in-law’s residence, a wealthy donor’s office, or, out of spite, an adversary’s pet project. When touring Republican strongholds, Tom Hofeller enjoys showing audiences the contours of Georgia’s 13th District, as proposed after the 2010 census, which he likens to “flat-cat roadkill.” (The map that was ultimately approved is shaped more like a squirrel that hasn’t yet been hit by a car.) This redistricting cycle’s focus of wonderment, in Hofeller’s view, is Maryland’s splatter-art 3rd District, which reminds him of an “amoeba convention.” He tends not to mention the gimpy-legged facsimile that is his own rendition of North Carolina’s 4th District.

 My speciality, Geographic Information Systems plays a role too:

“There’s an old saying: Give a child a hammer, and the world becomes a nail. Give the chairman of a state redistricting committee a powerful enough computer and block-level census data, so that he suddenly discovers he can draw really weird and aggressive districts—and he will.”

Fascinating article..

Building Google Deep Maps

After Apple's epic fail, its worth reading about how much effort Google has put into the making of accurate digital maps available for navigation and other location based services.

Alexis Madrigal writes in The Atlantic:

The sheer amount of human effort that goes into Google's maps is just mind-boggling. Every road that you see slightly askew in the top image has been hand-massaged by a human. The most telling moment for me came when we looked at couple of the several thousand user reports of problems with Google Maps that come in every day. The Geo team tries to address the majority of fixable problems within minutes. One complaint reported that Google did not show a new roundabout that had been built in a rural part of the country. The satellite imagery did not show the change, but a Street View car had recently driven down the street and its tracks showed the new road perfectly.

..and on Google's extended vision of capturing geographic information:

It's common when we discuss the future of maps to reference the Borgesian dream of a 1:1 map of the entire world. It seems like a ridiculous notion that we would need a complete representation of the world when we already have the world itself. But to take scholar Nathan Jurgenson's conception of augmented reality seriously, we would have to believe that every physical space is, in his words, "interpenetrated" with information. All physical spaces already are also informational spaces. We humans all hold a Borgesian map in our heads of the places we know and we use it to navigate and compute physical space. Google's strategy is to bring all our mental maps together and process them into accessible, useful forms.

Hyperspectral Mapping Of The Geology Of Afghanistan

This post submitted to the Accretionary Wedge # 48 hosted by Earth-like Planet. The theme is "Geoscience and Technology" and this post is on the use of multi and hyperspectral remote sensing for geological mapping.

Coinciding with the 40th anniversary of the Landsat series of remote sensing satellites, two maps of the surface distribution of several distinctive minerals covering a large portion of Afghanistan has been released by the USGS.

 Source: USGS Pub A

These maps have been prepared by processing the reflectance properties of surface materials captured by sensors aboard a plane. Conventional satellite mapping like that prepared from Landsat data does the same thing but it generally captures less information. For example, most conventional commercial satellites will capture reflected energy in the visible and the near infra red portion of the spectrum in 4 - 7 bands.

This type of remote sensing of the reflected and emitted energy from surface material is termed multispectral sensing. Recently, new satellites have started capturing hyperspectral data. Here, the energy from the visible to infrared spectrum is collected at very narrow intervals or channels. For example, NASA's Hyperion sensor aboard the EO-1 satellite is capable of collecting spectral information in 220 spectral bands from between the 0.4 to 2.5 µm (micrometer) bandwidth with a 30-meter ground resolution.

Map Of Potential Carbon Dioxide Storage Sites In U.S. Sedimentary Basins

via Nobel Intent:

Potential carbon dioxide sequestration sites are shown in blue.

Carbon capture and sequestration (CCS) is a climate change mitigation measure. Carbon dioxide emitted by power plants is compressed into a supercritical fluid and injected in deep saline aquifers with an impermeable geological capping layer that prevents the liquid CO2 from escaping.

Does U.S. sedimentary basins have enough storage capacity to make a difference in emissions? From the abstract published in PNAS:

We show that in the United States, if CO2 production from power generation continues to rise at recent rates, then CCS can store enough CO2 to stabilize emissions at current levels for at least 100 y.  This result suggests that the large-scale implementation of CCS is a geologically viable climate-change mitigation option in the United States over the next century.

Will it be economically viable though? There seems to be no hurry in the climate change policy environment in making CO2 emissions expensive enough for companies to turn to CCS.