Unit 1 Flashcards
To engineers, soils included
Layers of earth and rocks below the topsoil
We need to know if layers of soil
Can support what we’re building
Soils has been studied for
200 years
Tower of Piza mistake is
It’s location, built on area of acient river with varying river bottoms.
Soil boring (drilling)
To investigate/evaluate the subsurface conditions in the area of proposed structure
We investigate soils for
1) stability of soils in Excavation and Trenchs
2)Stability and Erosion in Slopes
3)Flow of Water through soils
4)Consolidation and Strengths of underlying soils
5) Lateral Strength of Soils and Retaining Walls
Shear Resistance
The strength of soil that resist one layer from sliding over the adjacent layer
Spread footings
Spread the load over a larger area, in competent soils
Piles or Caissons
Used to support load when competent soils are encountered at founding depth
How many Ice Age
5
Last Ice Age name and year of activities
Wisconsin advance, 85000-12000
During Ice Age, global temp and sea level drops
6°C, 120 m
Most landforms we see today were formed by
Advancing/retreating glaciers, glacier meltwater and glacier lake.
Glaciers are natural bulldozer
Stripped existing soils, ground up exposed rock surface.
Type of glacier
Alpine(Valley) glacier and continental glacier
3 Main Process of Erosion
Direct Erosion, Abrasion, Plucking
Glacier deposition method
1) Direct deposition
2) by meltwater
3)Drifting ice rafts
4) by wind
Direct Deposition: Till
Jumble of many diff types of rocks and soils, Unsorted and unstratified
Till contains
Typically silts and clays, good for earth fill (if sorted good for road building granulars)
By meltwater: Outwash
Sorted and stratified, ahead of glacier. Often low in slits/clays, smoothened rocks
Rock flour
Finely grounded rocks suspended in meltwaters
Ice Drift Rafts deposits
Lacustrine Deposits ( bed of glacier lakes)
By wind deposits
Loessian deposits. Mostly silts with some fine sands and clays. Loosely held together by calcium carbonates
Glacier landforms (9)
Moraine, Outwash, Lacustrine, Erratic, Drumlins, Kames, Kettles, Eskers, Marine
Moraines
Long, Rolling Hills. Some by Direct Deposits, Many by Outwash
Oak Ridges Moraine
Cadelon to Peterborough (160 km). Granular material, water source.