Dating is Everything

An important study was just published in Science Magazine by Dr. Nicolás Young (Lamont-Doherty Earth Observatory; Wooster Geology class of 2005). We knew this paper was coming as Dr. Young was our most recent Osgood speaker and during his visit he presented some of these results.

Conventional wisdom has always been that the last Ice Age was over, and that ongoing anthropogenic warming would delay indefinitely the inception of the next Ice Age. Young et al., show that the end of the Ice Age was instead over about 3.6 ka and that the world was in the midst of the next Ice Age for about 2000 years until very recently about 1960 CE. The evidence is a clever and careful study of trimlines, cosmogenic isotope dating, and vegetation and radiocarbon studies at the margin of the remanent of the Laurentide Icesheet (LIS) – the Barnes Icecap. The Barnes Icecap is an amazing place.

This paper changes quite a bit about the framework of the recent Ice Age and underscores the idea that we have ended an ongoing Ice Age. We could argue over whether this is a paradigm shift – it clearly is on some level. These inferences about the past could not have been done without the remarkable and clever use of multiple dating techniques that can resolve these changes. An excellent commentary in Science on this paper can be found here and an interview press release from Lamont here.

 

The Barnes Ice Cap and its recent trimline. Image from GoogleEarth. The figure below is from the Young et al. (2026) article showing the location of the Barnes Ice Cap and a portion of the geochronological dataset.

 

Reference:

Young, Nicolás E. et al. Late Holocene reexpansion of the Laurentide Ice Sheet. Science 394,455-459(2026).DOI:10.1126/science.aed3379.

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New Paper on an Extreme Low Lake Level in the Great Lakes

It was great to help out Dr. Tim Fisher (University of Toledo) in this effort (the full publication is here). Dr. Fisher was vacationing in Georgian Bay on Lake Huron when he discovered a stump rooted ~0.5 below the historical low of 1985. This low stand based on radiocarbon and tree-ring analysis occurred during the late decades of the 1600s. Since Lakes Michigan and Huron are joined at the straits of Mackinaw we can infer that this drop was basin wide. Such a drop today would significantly affect the shipping and shoreline infrastructure of these international water ways.

Figure 1. Map showing the location of the stump in Georgian Bay.

Figure 2. Photographs of the in-place stump.

Figure 3. Dating of the stump is critical and the figure above shows the wiggle-matching of a series of radiocarbon ages with the help of a tree ring sequence. Radiocarbon ages matched to the radiocarbon calibration curve allows for a unique solution to the dating placing the age of tree growth into the late 1600s.

The late 1600s is a fascinating interval in Earth history and has been associated with large-scale changes in the ocean – atmosphere system worldwide. Work by colleagues in Scotland have linked this interval to major societal changes and the Scottish Ills. In the North Pacific our recent Keck Project, examined this interval, which is also associated with large glacier changes and dramatic cooling. The late 1600s climate anomalies and associated dramatic changes is particularly fascinating as we continue into the forecasted super El Niño in 2026-2027.

The Wooster Tree Ring Lab has ongoing efforts to reconstruct the levels of the Laurentian Great Lakes with past efforts resulting from a Wooster Independent Study, and a more recent study reconstructing Lake Erie levels initiated by a junior Independent study.   Pending work and publications on Lake Michigan and Huron levels includes the work of Wooster student Lynnsey Delio.

Many thanks to Nick Wiesenberg of the Wooster Tree Ring Lab for his contributions to this work.

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Browns Lake Bog and Dams Blog

Guest Bloggers: Eddie, Stephen, Nolan.

We drove by the historic Kister Mill to examine the low head dam setup and discuss the origin of the “legacy sediments examined in other streams’.

Figure 1: Hydrology Lab at Shreve Lake (in the background), note the white forest inundated in the lake – these trees are cottonwood and grew up between 2014 and 2025 when the lake was drained.

Location map (DEM) showing the location of Shreve Lake and the bog.

This Monday, October 26, 2026, the Hydrology team (Figure 1) headed into the field to better understand how groundwater moves through the landscape. The Team stopped at two locations, Shreve Lake and Brown’s Bog. Surveying both gave the team a chance to see how water behaves in a natural wetland, as well as the managed, human-built dam at Shreve Lake. Our first stop was at Shreve Lake, where we got to walk on and investigate the earthen dam that contained Shreve Lake (Figure 2).

Figure 2: Earthen dam that contains Shreve Lake.

An earthen dam is built from compacted soil rather than solid concrete, which makes it very different from the concrete dams most people picture. Soil is a porous medium, meaning water naturally seeps through it, and how professionals control that seepage was a focus of our conversation. The team discussed how large concrete walls were installed beneath the dam to control the flow of water. These walls lengthen the path the groundwater must travel, which reduces the force of the water moving beneath the dam. They can also concentrate that flow into one location, which at Shreve Lake is the culvert. Directing seepage to a single, known point matters because water that moves freely through a dam can carry soil particles with it, a process called piping, which can weaken the structure over time.

 

Schematic cross-section of the dam with its drain.

Map of the kame and kettle topography at Browns Lake bog. The wells shows below are at the northern end of the central Kame.

Figure 3: Nolan, Stephen, and TA Arjan with a tile probe pushing into the peat in the bog. Looks to be at least four rods of peat.

Our second stop was Brown’s Bog, which offered a sharp contrast to the Shreve Lake dam. Bogs form on thick layers of saturated peat, which trap water like a sponge and then slowly release it back into the environment, keeping the water table at or near the surface. This wetland environment is extremely important for flood mitigation, because the peat absorbs excess rainfall and snowmelt during wet periods and releases it gradually during dry periods. To get a closer look at the peat, the team pushed a probe down into the bog (Figure 3). The probe was almost completely absorbed by the bog, showing how loose and deep the peat was.

Covering the surface of the bog was Sphagnum moss (Figure 4), the plant that helps build the peat. Sphagnum can hold many times its own weight in water, as it dies, it accumulates in the low-oxygen conditions of the bog forming the peat layers we probed.

Figure 4: Photo of Sphagnum moss, the prime ingredient of peat, which is mined throughout the region.

We also stopped at two small wells within Browns bog that had been dug at 2 different depths (figure 5). These two wells were dry, so we got no data from the wells. The data that we were trying to get from the well was the different water levels that would be displayed from the two wells. The wells were installed to show a change in the hydraulic head in the vertical while being so close together. This is because water comparing the two would have shown whether groundwater was moving upward or downward through the bog. The deeper well would have a higher level of water than the well that goes down less.  This is because the deeper well would have a higher head, making the water rise more and more water get sucked in the well to go up in the sediment to the higher elevation/lower head well.

Figure 5: Classmate Leo Measuring the depth of water in 2 separate wells installed to 2 different depths.

Overall, this field trip helped us better understand how groundwater moves through the landscape and how water is stored in different environments. At Shreve Lake, we learned how earthen dams control seepage to prevent erosion and keep the structure stable. At Brown’s Bog, we saw how peat and sphagnum moss absorb and store water and helping reduce flooding and how it is well-preserved with a high water table. Even though we could not collect useful data from the two wells, the activity showed us how wells can help measure groundwater levels and understand groundwater flow. This trip showed us the important role groundwater plays in both natural environments and human-built structures.

On the drive out the dust from the ongoing corn harvest spread across the area which is having a role in fertilizing the nutrient – poor bog at Browns Lake.

The mostly well-behave group on the boardwalk at Browns Lake. Special thanks to Maddie for all the driving on our trips this semester and to Fred who took us on this trip. Keeping us on the best route and one time each lab period is gratefully appreciated.

 

 

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The Abbey Arboretum and The College of Wooster Campus

We are thankful of the generous gift to the College of Wooster that made possible the designation of our campus as an arboretum – The Abbey Arboretum. Paul Abbey (Wooster class of ’73) and his wife, Constance Norweb Abbey, have established the campus-wide Arboretum at Wooster. The campus consists of over 2,800 trees managed by the grounds staff lead by Phil Olsen. The Wooster Tree Ring Lab has recently updated the tree-ring record from the white oaks on campus and the tree centric organization lead by Paul Abbey – Rooted in Trees featured our class work (fall 2026) with the College updated oak tree-ring record in their newsletter excerpted below – the full text is here:

 

Many thanks to Jessica Wharton Travis of Rooted in Trees for great prose and compelling story.

 

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The Wooster Tree Ring Lab and Archaeology Day at the Wayne County Historical Society, Wooster Ohio

The College of Wooster Tree Ring Lab (WTRL) participated in Archaeology Day. It was a beautiful day exchanging views and data between archaeologists, historians, Wooster Earth Scientists and the public.


Li and Leo explain the extraction of local information from tree-ring in Wayne County that is relevance to the Settlement of Wayne County Ohio.

Local collectors, historians and Archaeologists from surrounding counties share their expertise.

Trees as witnesses was common theme and many of the participants grew up around the old growth on The College of Wooster campus as well as Cornerstone Elementary School campus, Browns Lake Bog, Barnes Preserve and Johnson Wood, all in Wayne County.Li worked with the younger participants assembling Tree Ring Lab necklaces (see lower right) and handing out stickers. Before the kids can get a necklace they needed to identify the species of the wood making up the necklace pendant. The log building in the background – the Naftzger cabin, has been dated using tree rings by the WTRL. Here is the report.

Nik shows the group a core from the oldest living tree in Ohio (so far discovered). It is chestnut oak from Stebbins Gulch, which is part of Holden Arboretum. He successfully identified his necklace as a historical piece of white oak from an Ohio barn. White oak is a favorite of the lab and makes up most of the beams of the historic building on the Historical Society campus. Oak truly is the “Frame of Civilizations”.

Local historian (lawyer and College of Wooster graduate) Jeff Musselman stands next to the sign of the Historical Society’s flagship Beall House. It was the tree-ring dating of the Beall House along with Jeff’s historical detective work that determined the exact years that the house was built. Here is the WTRL report on the dating of the Beall House.

Many thanks to Li and Leo for taking a portion of their Saturday to volunteer at Archaeology Day. Li is a senior Earth Scientist working on a field guide for Browns Lake Bog for their thesis and Leo, as a sophomore, is exploring his options. Special thanks to the Historical Society and Roger Rowe for organizing the day and all those volunteers that operate the activities and maintain this amazing campus.

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GSA2026 Denver – Student Work

Four Wooster undergraduate students traveled to the Annual Meeting of the Geological Society of America in Denver for three days of presentations, networking and learning. They reported on preliminary results of their Independent Study thesis work.

Cheyenne gears up for some lively conversation – she has taken on the task of comparing Northern and Southern Hemisphere coastal tree-ring records aiming to better understand the role of the ocean-atmosphere system in the Pacific that is symmetric across the tropics.

Adam is looking at the signal in old growth (>250 years old) forests across Ohio that “witnessed” European Settlement in the early 1800s. This is a timely study coinciding with 250 Anniversary of the Nation.

Anika is reporting on a discovery that Western Red Cedar have a winter signal in their ring-widths – explaining this is a big part of her work. She is the first to report on the first red cedar chronologies developed from Alaska. Another first for the Wooster Tree Ring Lab.

Anna has taken on a study of lake cores and the interval in time that coincides with Settlement and changes in diatom communities over the past few hundred years in two lakes in the Sierra Nevada, CA.

Anna shares an inside diatom perspective with an interested fellow scientist.

Anika explains that the last several decades in Southeast Alaska were the warmest winters over this several hundred year record.

Adam explains the signal in witness trees of multiple tree-ring records from different species in NW Ohio.

The Patagonia/ Gulf of Alaska comparison has not been done for over 15 years (originally done by Ricardo Villalba and others in 2011). We know more about the dynamics of mid-high latitude climate variability and the tropics now, and the results are revealing.

Alumni and students at the get together. Alumni who stopped by included former professors in Wooster Geology, Dori Farthing (SUNY-Geneseo; second from left), Jade Star Lackey (Pomona; and his son Finn) and Stephanie Sparks (Northern VA Community College); alums included Katherine Nicholson Marenco (Bryn Mawr; left above), Mary Palmieri (middle above), Abe Springer, Nicolas Young, Jack Whitehouse (who is a new graduate student of Abe Springer’s, both at Northern Arizona Univ.) and George Davis.

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Hydrology Lab (HYDRO26) Stream Gauging

Guest bloggers: Anika Knowles, Ellie White, Leo Casalini and Cheyenne Wentz

The HYDRO’26 Stream Gauging Team

Objective: On Monday, September 28th, students of the Wooster Hydrology course returned to Apple Creek for a second time. The main goals of the trip were to measure the stream velocity of Apple Creek and to determine whether Apple Creek is a gaining or losing stream by comparing discharges along a reach of the stream. A gaining stream is a stream which intersects with the water table and receives water from the groundwater system. On the other hand, a losing stream is a stream with the water level above the water table and  it “loses” water to the water table. Whether a stream is gaining or losing water can be affected by the stage of the stream, the amount of clay present in the surrounding soil which can acts as an “aquitard” to keep water from flowing downwards to the water table as well as other factors. The class was joined by Peter Quent, a project manager with EnviroScience, who provided insight on how stream channels develop and change overtime, in turn, affecting a stream’s velocity. Nick Wiesenberg, the Earth Science Department technician aided students in the gathering of data and the operation of various instruments.

Two of the HYDRO ’26 Team and Nick Measuring Depth and Velocity

The HYDRO ’26 Team Collecting Clay

Methods: We split up into various teams: water gauging, well installing, and clay collection. The water gauging team had two people hold a measuring tape across the river channel, and another two took measurements of water depth and velocity each meter across a cross-section to get a total discharge at two reaches along the stream.

Measuring well levels relative to the stream level – gaining or losing?

The HYDRO ’26 Team Using the Well Probe (in the distance) and observing velocity measurements being taken. The group is perched on the point bar.

The well-probing team drove a well probe into the bottom of the stream, then measured the water level with a water level indicator relative to the stream stage. Hydraulic head is the height of the water table in this unconfined system, so looking at the head of a stream relative to the well we can determine if the stream is gaining (effluent) or losing (influent). The clay collection team dug out clay from the bank using an auger. This clay was transported back to the lab in a bag for further investigation – we suspect it is lacustrine clays similar to the confining layer in the Wooster Aquifer just downstream.

There was quite a bit of geology along the creek – here the cutbank is composed of bedrock and a fining-upward channel fill with gravels at the base and about 60% overbank silts and clays overlaying the section. Note the walnut tree behind Cheyenne that has developed adventitious roots in response to overbanck aggradation.

Results: Based on the streamflow measurements, the velocity of the stream in the wider, upstream section was much lower than the narrower, downstream section. Further calculations of the stream profile and discharge will be done by the class over the next week. In addition, the well probing measurements showed that the hydraulic head within the well probe was lower at three sites along the stream. This indicates that Apple Creek is a losing stream. Finally, the clay collection showed that there is a series of fining upward sequences, indicating flood events that increased the stream’s competence. A greater competence allowed larger grain sizes to travel farther, and smaller grain sizes to deposit on the overbank, leading to the large amount of clay deposits. The exposure of these fining upward sequences is due to the erosion of Apple Creek as it moves laterally across the floodplain and old chutes and channels are infilled.

Ellie’s notes Over the Depth and Velocity of Site 1 and Site 2

End of the day – hauling out all the equipment. We thank Nick, Peter and our bus driver Maddie for their help.

 

 

 

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The fossil record of bioerosion: a new paper decades in the making

I am very pleased to announce the appearance of “The fossil record of bioerosion“, an invited review paper now on the Journal of Paleontology FirstView server. My excellent team of coauthors includes Paul Taylor (Natural History Museum, UK), Ursula Toom (Department of Geology, Tallinn University of Technology, Estonia) and Olev Vinn (Department of Geology, University of Tartu, Estonia). This paper was invited for a special volume of the Journal of Paleontology to mark its centennial anniversary in 2027. It is open access and thus available to anyone. The following description is modified from the abstract.

Bioerosion is the biological removal, abrasion, or dissolution of hard substrates. It has produced a rich and behaviorally informative trace fossil record spanning the Archean to the Recent. We wrote a comprehensive review of the fossil record of bioerosion based on an exhaustive survey of the ichnological literature through August 2026. Building on earlier syntheses, we compiled and critically evaluated all currently valid bioerosional ichnogenera and ichnospecies, documenting their original authorship, substratum preference, inferred trace makers, architectural design, ichnofamilial assignment, and stratigraphic ranges resolved to, where possible, the stage level. The resulting database recognizes 151 valid bioerosional ichnogenera and 419 ichnospecies. Analyses of ichnodiversity and ichnodisparity of the bioerosion record shows that the most fundamental architectural designs of bioerosion were established by the end of the Great Ordovician Biodiversification Event (GOBE), with relatively limited innovation thereafter. Ichnogenus diversity increased overall through the Phanerozoic, punctuated by major diversification pulses in the Late Ordovician, Late Triassic, Jurassic, and especially the Cretaceous. In contrast to body fossil patterns, most mass extinctions, including the end-Permian event, are only weakly expressed in the bioerosional ichnogenus record; the Cretaceous-Paleogene boundary shows the most pronounced decline. These patterns underscore the resilience and recurrence of bioerosional behaviors through deep time.

We believe our primary contribution to the ichnological literature is our extensive database, which we linked as an online resource with Dryad ( https://doi.org/10.5061/dryad.d51c5b0kg ). Future researchers are invited to download these spreadsheets and then correct, augment and otherwise edit them as desired to reveal more patterns in the stratigraphy and paleoecology of bioerosion. The paper, its extensive bibliography and its database are all open access. We also encourage professionals and anyone else interested to visit the Bioerosional Trace Fossil Database ( https://tracefossils.info/ ) , a richly-illustrated and updated website envisioned and maintained by our coauthor Ursula Toom.

Finally, I’d like to repeat here my line in the paper’s acknowledgements: “MW thanks The College of Wooster for decades of supporting paleontological research.”

Reference:

Wilson, M.A., Taylor, P.D., Toom, U. and Vinn, O. 2026. The fossil record of bioerosion. Journal of Paleontology (FirstView). https://doi.org/10.1017/jpa.2026.10285

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Updating The College of Wooster Oak Tree Ring Record

Guest blogger: Adam Wood

The Modern Climate Change course in the fall of 2026 (MCC26) took on the task of updating the campus oak ring-width tree ring chronology. It was last cored over a decade agoand is one of he few sites of Ohio’s remaining old growth (those trees greater than 250 year old). Not only is 2026 the 250th anniversary of the nation, it is also the first year of the College campus as an arboretum – the Abbey Arboretum.

Nick Wiesenberg (center) directs the coring operation.

Coring Trees on Campus:
Home to several old growth white oak trees, The College of Wooster has “tree witnesses” to the last 250 years of changing climate and land use. Old growth trees, specifically those of the white oak (Quercus alba) have been found to date back to the late 1600s CE in Ohio. Using dendrochronology the  MCC26 class were able to count the individual tree rings in each tree core and assign calendar years to each growth band and combine this data with previous year’s efforts to update the college’s tree ring chronology to 2025.

Methodology:
On September 28, 2026, the MCC class with the help of COW technician Nick Wiesenberg used increment borers to core the oaks. In total, 22 trees were sampled for the update.

Adam, who is working on assembling all the old growth sites across Ohio for his
senior Independent Study, cores one of the 300 year old oaks on the campus.

Li logged in the coordinates of each of the trees sampled and mapped them here. The Oak Grove was targeted and the individual trees are the black and red dots on the map. This photo is looking north.

Li, our cartographer, takes a core using an increment borer.

Maddie extracts an additional core as Li records the vital meta data.

We recruited Arjan (left) and Cooper also Earth Science majors to help the effort.
Arjan is doing his IS on natural springs in the Wooster area and Cooper is mapping
and working out the geologic history of Fern Valley, The College of Wooster Field
Station in Holmes County. Many thanks for their help.

Lab work:
The cores from these sites were then sanded and the ring widths measured in the COW Tree Ring Lab. Cores were initially dated by manually counting the number of rings. For precise ring-width measurements (0.01 mm) we used the VELMEX measuring tables in the lab, computer software tracked the distance between the ring boundaries writing the data to digital files. The cores were then crossdated with previous collections from the campus to produce the indices of the ring-width chronology.

Madeline measures one of the older oak cores.

Maddie’s first core.


Li marks a core prior to measuring.

Adam is a veteran in the lab, here marking one of the campus cores.

The New Chronology:
The resulting standardized indices compiled into chronologies end in 2025 the final full ring measured. Due to low sample depth in the earliest dates the series was truncated at 1720 CE. The chronology now spans 1643-2025 and is a combination of 57 cores. A release (marked increase in ring-widths) at 1is clear (graph below), as well as the 1895 drought. The release coincides with the establishment and initial construction of The College of Wooster campus. Prior to the establishment of the College, the land was a 20-acre hilltop of oak trees grassland (Gasbarre 2019). The construction of the College is likely the reason for the release in 1866, as cutting of the canopy would have permitted access to greater sunlight and nutrients for the oaks, and thus wider rings. Prior to 1866, the trees did not exceed a width of ~1.3 mm. The sudden rise in width, nearly reaching 2.5 mm, also records other events like in 1895 drought.

The ring-width chronology – this is truncated at 1720. The oldest tree on the campus is 383 years old. We truncate the series because only a few series extend past 1720.

Next steps:
The class is now examining the tree ring series as a record of droughts, past volcanic events linked to changes in hydroclimate, identification and significance of the releases, as well as the possible changing climate signal in the tree growth. In addition, thanks to the assistance and guidance of the Special Collections librarian, Rebecca Roper, the MCC26 class was able to review items from the college archives pertinent to the history of the college and its trees. Additional linkages can be made by comparing our tree ring data to archival records.  For example we know that the college faced a deadly onset of Dutch Elm disease around 1968 and into the 70s’. According to a report at the time from the Wooster Reporter, in the spring of 1970, the college was forced to cut down multiple of their elms which sat on Quinby Quadrangle (the front of Kauke Hall) which may be evident in our record. Furthermore, reports of the Chapel construction affecting the water table and documented lightening strikes on trees may be link to some of the tree ring variability.

Removal of elm trees in spring of 1970 by the College of Wooster due to outbreak of Dutch Elm disease. The College has a long history of preserving the campus trees and only when necessary are trees removed.

Acknowlegements:
Special thanks to Nick Wiesenberg (Departmental technician) for his help. Special Collections librarian Rebecca Roper helped our historical efforts and Phil Olsen, director of grounds, granted us permission to core these oaks.

The collection archived in the Wooster Tree Ring Lab. The data from this update will be contributed and added to the existing tree-ring data archived here.

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Fern Valley 2026 – HYDRO26

Fern Valley is The College of Wooster field station in Holmes County. The HYDRO26 class ventured to the site for a quick walk on a spectacular day. The mission was to learn some basic geology and examine sediments that we need to learn to recognize in water well logs when we build cross-sections across this buried valley site.

The Wilkin Run water levels were low and somewhat murky after some intense rains a few days prior to the trip. “Wood is good” in streams, yet it can be challenging to navigate. There was relatively little whining in the group, which was surprising.

Gabe (above) exploring an entrenched tributary along an alluvial fan. One of the Wooster students is mapping the Fern Valley Station as part of his thesis and below is a map of some of his sites.

3200 feet below the Fern Valley field station is oil and gas production in the Clinton Sandstone, one of the big oil plays drilled in the 1950s and 60s and still active today. Now the wells on the property serve as a gas storage field maintained by Columbia Gas.

A photo above taken a few years ago that illustrates the various sediments described in water well logs in the area. We classify this as ice-contact stratified drift from the last advance of the Laurentide Icesheet.

The clay contact shown in the photo above is at the stream bed level at this site and is easily penetrated with a tile probe.

Further downstream (down section) the clay is more deeply incised.

Taken together after visiting several out crops and examining well logs a cross-section of the valley can be constructed. The stratigraphy along with ongoing mass movement are shown above.

The group is photographed on the scarp of the main normal fault – the photographer is standing on the footwall. Some classify this fault as a sort of listric normal fault.

The mass movement starts as a downdropped block “sliding” along the underlying clay. With distance from the fault the overlying ice-contact stratifield drift transitions into a sediment gravity flow shown above. The sediment is then fed into the river which takes it away. This is an ongoing process and the mass movements have the potential to impact the pipelines and other infrastructure in the region.

Maddie had the bus ready when we returned and took us on a tour on the way back to Wooster including a viewing of the newly renovated Shreve Lake (show below) with its new dam.

 

 

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