The landslide history of the Riverside Ave area in Burlington, Vermont.
In this image, Riverside Ave is seen running parallel to the Winooski River. The north side is very steep, and the south side includes a ditch with a stream valley cutting through it. A flow of streamwater combined with steep slopes is an indication of potential landslides if the area is not maintained properly!
The area surrounding Riverside Ave was filled and the road was paved and widened by about five to six feet. This addition of fill is very important later on. A Telford Stone base underlies the paved road. Several years later, the road was widened again in order to make it nicer.
First aerial imagery of Burlington becomes available.
The first of the three 1955 washouts occurred at the end of August.
A second, larger washout breaks a water main and carries many yards of dirt. The likely blame was an unused culvert about 65 feet below the level of the road. The road foundation was eroded by water from the culvert. A new asphalt road was built around the damage.
Thousands of yards of fill and several large pine trees slid down into the Winooski River. Nearby workers repairing damage from the September landslide had a narrow escape.
Shown above are three images from the landslides in 1955. The damage occurred very close to multiple buildings and appears extensive.
Photo credit hereTorrential downpoars result in a landslide off of Manhattan Drive, close to Riverside Ave.
Aerial imagery reveals that a huge section of trees by the stream valley was cleared. Without trees to absorb rain water and groundwater, more water will travel downslope towards the filled section on the north side of Riverside Ave. Additionally, this section north of Riverside Ave does not look as densely packed with trees and more buildings have been added. There are consequences for an area with a decreased ability to hold water and steep slope.
A landslide occurs in the same area on Riverside Ave as the most recent 2019 slide. The VT Highway Department later tested soil borings and asked for engineering aid to figure out the best way to prevent future landslides.
Looking between these two images, there are several changes in the treeline, including one just east of Hillside Terrace. Given the time of year and looking at when other landslides in the area occurred, it is possible that there was a small landslide sometime between August and September of 1972.
A landslide spills ~4000 yards of earth, trees, and garbage into the Winooski River as a result from heavy rainfall. The landslide occurred about 35 feet from Riverside Ave next to BJs Variety Market.
A resident of Riverside Ave illegally deposited debris from a landfill excavation to his property to serve as fill. The material caused the bank to give way, resulting in a landslide of dirt, trees, and garbage. Further erosion was caused due to poor work done by a contractor who had been hired by the man who was illegally dumping the fill.
The city of Burlington searches for a consultant to find a method or preventing future landslides at Riverside Ave. Health and Safety officer Steven Goodkind wants to study the long term erosion of the area, as he is worried about another collapse. Street department workers began digging to find and analyze the drains that were installed under the road in the 1950s. Additionally, there was controversy between whether it was the responsibility of the state or the city too keep the road safe.
Steve Goodkind says that the engineering report for the Riverside Ave area will be available shortly. It was also determined that the landslides were occurring because the land was steep and people had been dumping fill illegally.
There is increasing concern about the safety of Riverside because the cliff is gradually getting closer to the road. Steven Goodkind says the area needs immediate work, because if the banks freeze during the winter and the water table builds up, a thaw could result in a major landslide. The previous dumping of fill did not help this cause.
Photo credit: HereWorkers begin to make the slope off of Riverside Ave more stable. The plan was to remove clay from the bank and replace it with a combination of 3000 cubic yards of stone and 2000 cubic yards of sandy fill in order to make the bank more stable and less steep. The goal was for the area to have a 1:2 slope. This project was completed with the intention to fix the hazard permanently.
Photo credit: HereAerial imagery reveals that more houses have been built on top of the stream channel. The top image is a color IR image from 1984, and the bottom image is a black and white orthophoto from 1999. The stream channel runs just outside of the new development.
Hillshade DEMs of 2004 (top) and 2014 (bottom) are seen to the left. A hillshade DEM provides a better look at the area's topography. Looking just under the Winooski River, several areas on the slope look uneven or cracked, indicating that landslides occurred sometime in the past. There is not a noticeable change between these images, indicating that the area appeared stable for the time being.
Photo credit: HereUnpermitted filling occurrs between 2017-2019. The latest addition of fill was added during spring/summer of 2019.
UVM geology professor Paul Bierman notices cracks in a parking lot on the north side of Riverside Ave. The car wheels had sunk down as well, indicating that this was a recent occurrence.
A landslide occurs in the same section as the 1968 landslide off of Riverside Ave following a large rainstorm. This is an indication that that area in particular is unstable. Additionally, this is the last piece of information we have, at least for now.
For decades, Riverside Ave has had the unfortunate pleasure of dealing with landslides. The main issues which have caused these landslides are the placement of fill along a steep slope combined with water. The removal of trees later on was an additional contributor. Going back to the 1872 topographic map, a large stream valley is visible on the south side of Riverside Ave. This is an important detail to pay attention to, because more water will travel into the stream valley and impact the steep slope on the north side of Riverside Ave.
In the early 1930s, the first placement of fill along Riverside Ave was recorded. At this point in time, there are trees on both sides of the road, but the road itself sits on top of fill which does not appear to be as stable as it should be. Moving forward to fall of 1955, three landslides were recorded in the span of several months and caused extensive damage. All of these occurred in areas where fill had been placed back in the 30s. It was likely that heavy rains triggered the already unstable slope repeatedly until the ground was too saturated and the material slid down the steep slope.
In 1962, aerial imagery shows a huge removal of trees within the stream valley. While this did not have immediate consequences, there were not as many trees in the area to absorb rainwater and groundwater. This resulted in more water moving downslope, north of Riverside Ave, to an area that had been filled. Several years later in 1968, another landslide occurred just northwest of the area where the trees had been cleared. It is important to note that this was the same area where the 2019 landslide occurred. Although there did not appear to be as much damage as the 1955 landslides, it raised enough concern that the state looked into preventing future landslides. Shortly afterwards between August and September of 1972, a small landslide potentially occurred in a similar area. Looking at aerial imagery, there is a slight difference in the tree canopy which is a possible indicator of a landslide.
In late summer of 1976, a landslide carried approximately 4000 cubic yards into the Winooski River. The material is visible protruding in the Winooski in the 1981 imagery. It was not visible in the 1974 imagery, indicating that it resulted from the 1976 landslide.
The last major landslide that occurred before the Halloween slide in 2019 took place in 1981 as a result of filling. A private landowner illegally dumped fill on his property, causing a landslide of trees, dirt, and debris along with further erosion of the slope. This event really opened the eyes of the city and state, who finally took action in 1983 to repair the area for good, or so they thought. Clay was removed from the slope and replaced with sand and rock. The new slope that was created was not as steep as the previous one either in order to reduce the hazardous risk.
Finally, on October 31st of 2019, a landslide triggered by heavy rains occurred in the same spot as the one in 1968. A second landslide occurring in the same spot suggests that that area is unstable to begin with. An already unstable area is more vulnerable, which is what happened in this case.
It has been almost 100 years since filling began on Riverside Ave, and while there have been large gaps in the timeline, Riverside Ave is still experiencing the same issues today as it has been over the century.