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How did Block Island form. How is it changing now

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Presentation on theme: "How did Block Island form. How is it changing now"— Presentation transcript:

1 How did Block Island form. How is it changing now
How did Block Island form? How is it changing now? What will it look like in the future?

2 Block Island: a product of Erosion and Deposition
weathering: the change/breakdown of rock on Earth’s surface erosion: movement or transportation of weathered materials agents of erosion: gravity, wind, glaciers, and water (ocean currents and waves, streams, groundwater) deposition: the leaving behind of materials carried by erosion agents of deposition: gravity, wind, glaciers and water (same as for erosion)

3 Background Information

4 Wind Erosion Wind: erodes land by carrying away rock particles
mostly smaller particles: sand and rock dust (silt and clay) are carried by wind

5 Wind Deposition deposition by wind: most common – dunes (mounds of wind-blown sand) gentler slope of a dune – faces wind

6 Slumping: erosion from groundwater and gravity
Large block falls off a cliff or bluff forms- sea cliffs/bluffs

7 Erosion by ocean waves physical weathering: force of the water weathers and erodes the shoreline affecting beaches

8 Ocean Wave Deposition beaches: deposits of sand or larger particles on ocean (or lake) front beach changes seasonally – remember beach profile?? berm: top of the sloping surface (above is part for recreation) sand bar: long underwater ridge of sand carried away from beach

9 Wave anatomy Wavelength: distance between 2 crests or 2 troughs
Wave height (2 X amplitude): height from trough to crest How could you determine these??

10 Wave characteristics Wave period: the time is takes for a wave to pass a fixed point Wave frequency: the number of waves that pass by in a given time. How could you determine these??

11 Wave characteristics 2 Wave speed: the distance traveled by a given point on the wave (such as a crest) in a given interval of time. In equation form:

12 Longshore Currents general movement of sand along beach: in same direction that waves hit shore longshore current: movement of water and sediment parallel to, and near shoreline animation: Real video:

13 Features from longshore current deposition:
Headland: land surrounded by water on three sides spit: long narrow deposit of sand connected at one end of shore tombolos: ridge of sand deposits connecting islands to mainland

14 Glacial Erosion Glaciers are “rivers of ice” slowly flowing, moving sediments and changing the surface and shape of the ground beneath it Last glacial ice age in NE ended about 18,000 years ago

15 Glacial Deposits glacial till:  unsorted glacial materials
stratified drift:  sorted and deposited in layers by meltwater Glacial erratic

16 Features from glacial deposition:
Glacial moraines: landforms made from glacial till terminal (end) moraine: deposited at the end

17 More features from glacial deposition:
moraine erratics: large boulders transported by glaciers

18 More Glacial Deposition features
drumlins: low tear-shaped mounds of till kettles: depressions left from melting ice

19 Stratigraphy Stratigraphy is the study of strata, or layers
Stratigraphy can tell us about how the soil was deposited, they are clues to the land’s origin

20 Your tasks in the field (gathering evidence for your big 3 questions)

21 Task 1: create a topographic map of Block Island

22 Another look

23 Converting an island into a “topo” map

24 Hawaii topo

25 Creating a Contour/Elevation Map
Use your elevation observations to determine the higher/lower points on BI Draw contour lines onto the map

26 Try a sample map

27 Task 2: Sieving soil, to tell particle size
You will collect soil samples to sift with “sieves” These will separate the soil into different sized particles – gravel, fine gravel, coarse sand, fine sand and silt and clay Sieving Purpose: this tells how the soil got there

28 Soil sizes

29 Soil horizons, or strata

30 Sand, different sizes deposit by different ways
How is sand classified? If you classify sand by size, you look at the diameter of each sand particle. Very coarse sand, like you might see in a sand box, has the largest particles. The diagram below shows the actual size of sand particles from 0.5 to 2 mm in diameter. very fine   mm fine   mm medium   mm coarse   mm very coarse   mm

31 Conclusions from sieving and soil profiling:
The bigger the sand particle size, the steeper the beach typically is: Steep, big particle beaches are formed from strong deposition forces and erosion This makes them less stable Flat, small particle beaches are formed from gentle deposition forces, and are more stable

32 Task 3: create a beach profile
Beach profiling provides clues as to: how the beach formed how is it changing now


34 General beach anatomy

35 How does the beach change over time?
The shape of the beach is in continual change due to the weather and tides. In calmer weather with regular tides, sand is gradually deposited onto the beach from sand bars out in the ocean, dunes and berms may form. In stormy weather, the beach erodes and sand is brought from the beach to sand bars, which run parallel to the shore (provides better surfing).

36 More of the same

37 Task 4: Measuring wind speed and direction
Wind speed: use an anemometer Wind direction: use the compass

38 Good luck geologists!

39 Review: Fill in the characteristics for each type of change

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