%0 Report %D 2011 %T Preliminary field report on the November 13th-14th, 2011 landslide near Steam Mill Road, Deerfield, Massachusetts %A Joseph P Kopera %A Stephen B Mabee %K #Deerfield %K #Landslides %K #MGSPub %K #NaturalHazards %K #Reports %K flooding %K hazards %K Irene %K landslide %K mudslide %K natural hazards %K swamp %X On November 13th and 14th, 2011, residents and business owners in the area of Wapping Road in Deerfield, Massachusetts, began to notice light-gray, clay-rich mud appearing in the streams and wetlands east of State Route 5/10. The mud quickly clogged culverts under Wapping Road, Route 5/10, and the Pan Am Southern Railway tracks, partially filled in wetlands on both sides of Route 5/10, and partially filled in drainage ditches upgradient of these wetlands. This resulted in localized flooding of property along the east side of Route 5/10. Prepared for the Deerfield Board of Selectman and Board of Public Health 19 pages. A NEPR radio interview with Joe Kopera about the landslide can be found at http://nepr.net/news/2011/12/02/fallout-2011s-extreme-weather-landslides-ice-jams/. %B Open File Report %I Massachusetts Geological Survey %P 19 %G eng %U http://www.geo.umass.edu/stategeologist/Products/reports/Deerfield_LS_Report_final.pdf %0 Report %D 2011 %T Preliminary field report on the Route 2 landslides of tropical storm Irene, August 28, 2011 %A Stephen B Mabee %A Joseph P Kopera %K #Landslides %K #MGSPub %K #NaturalHazards %K #Reports %K Cold River %K hazards %K Irene %K landslide %K Mohawk State Forest %K natural hazards %K Rt 2 %K Savoy %X The Massachusetts Geological Survey accompanied Massachusetts Department of Transportation personnel in the field on Tuesday, September 6, 2011, to observe the landslide and flooding damage along the Route 2 corridor caused by Hurricane, which struck the area on August 28, 2011. The purpose of the visit was to: 1) identify the type of slides that occurred; 2) estimate the dimensions and volume of material moved; 2) estimate the geological and environmental conditions leading to the slope failures; and, 4) determine the propensity for future occurrence. Four landslides were observed. Slide 1 is immediately east of the confluence of Trout Brook with the Cold River and Slides 2, 3, and 4 are clustered together on a north- facing slope about 1850 feet east of the confluence of Black Brook with the Cold River. Report prepared for Massachusetts Department of Transportation. %I Massachusetts Geological Survey %P 18 %G eng %U http://www.geo.umass.edu/stategeologist/Products/reports/Rt2_Irene_FieldReport.pdf