fig. 12-co, p. 315
DESCRIPTION
Fig. 12-CO, p. 315. Fig. 12-1a, p. 317. Post-Glacial Sea Level Rise. 0. 0. 20. 75. 40. 150. Sea level change (m) from present day. 60. Sea level change (ft) from present day. 225. 80. 300. 100. 375. 120. 450. 140. 20. 18. 16. 14. 12. 10. 8. 6. 4. 2. 0. - PowerPoint PPT PresentationTRANSCRIPT
Fig. 12-CO, p. 315
Fig. 12-1a, p. 317
Fig. 12-1a, p. 317
Post-Glacial Sea Level Rise0 0
75 20
150
60
40
22580
300100
Sea
lev
el c
han
ge
(ft)
fr
om
pre
sen
t d
ay
375 120
450 140
18 16 14 12 10 8 6 4 2 0
Thousands of years ago
Sea
lev
el c
han
ge
(m)
fro
m p
rese
nt
day
20
Fig. 12-1b, p. 317
Fig. 12-1b, p. 317
Sea Level Projections
30 80
7025
60
20
15
1030
20 Sea
lev
el r
ise
(cm
)
40
50
Sea
lev
el r
ise
(in
ch)
5 10
−5 −10
0Observations
0
1950 1975 2000 2025 2050 2075 2100
Fig. 12-2a, p. 318
Fig. 12-2b, p. 318
Fig. 12-3, p. 319
Fig. 12-4a, p. 319
Fig. 12-4a, p. 319
Blowhole
HeadlandSea cliffs Sea stack
Sea caveExposed beach
Sea arch
Wave-cut platform
Sediments
Fig. 12-4b, p. 319
Fig. 12-4c, p. 319
Fig. 12-4c, p. 319
Wave-cut platform
Original land surface
Sea cliff
Notch eroded by waves
Fig. 12-4d, p. 319
Fig. 12-5, p. 320
Fig. 12-5, p. 320
Wave crests
Wave energy converging on headlands
Wave energy diverging
Sediment movementQuiet beach
Quiet beach
Fig. 12-6, p. 321
Fig. 12-7, p. 321
Fig. 12-8, p. 322
Fig. 12-9, p. 322
Fig. 12-10, p. 322
Fig. 12-11, p. 323
Fig. 12-12, p. 323
Table 12-1, p. 324
Fig. 12-13, p. 324
Fig. 12-13, p. 324
Shallow-water wave
A
To shoreB
Fig. 12-14, p. 325
Fig. 12-14, p. 325
Back-shore Fore-
shore Nearshore (through breakers)
Dunes
Berms Beach scarp
Offshore
Berm crest
Longshore trough
Longshore bars
High tide
Low tide (dotted line)
Fig. 12-15a, p. 325
Fig. 12-15b, p. 325
Fig. 12-16a, p. 326
Fig. 12-16a, p. 326
Upper limit of wave actionSurf
zone
Longshore current
Path followed by sand grains
Direction of wave approach
Fig. 12-16b, p. 326
Fig. 12-17, p. 327
Fig. 12-18a, p. 328
Fig. 12-18a, p. 328
Coastal cellCliff
erosion River input Major river forming
a delta
Longshore transport Rocky
point
River inputSubmarine
canyon
Sediment entering longshore transport system
Sediment movement down continental shelf and slope
Sediment transport to ocean basin within a submarine canyon
Fig. 12-18b, p. 328
Fig. 12-18b, p. 328
Santa Monica
NMalibu
RedondoLos Angeles
Long Beach
Palos Verdes
HuntingtonNewport
Santa Cruz Island
Submarine canyon OceansideLongshore drift
Santa Catalina IslandRocky headlands
0 50 San Clemente Island
Laguna
km
Fig. 12-18c (1), p. 328
Fig. 12-18c (1), p. 328
W–
Cliff
C+Surf
zone
V+O+
Beach
V–
O–
Fig. 12-18c (2), p. 328
Fig. 12-19, p. 329
Fig. 12-19, p. 329
Longshore current
Sand spitBay mouth bar Barrier
islandBay
Inlet Sea island
Lagoon Bay Tombolo
Beach
Fig. 12-20, p. 329
Fig. 12-21, p. 329
Fig. 12-22, p. 330
Fig. 12-22, p. 330
Isle of Wight Bay
Fenwick Island
N
Ocean City
Ocean City InletMARYLAND
Upper Sinepuxent Neck Atlantic Ocean
Position of shoreline
19801849Assateague
Island
Sin
epux
ent B
ay
km0 1 2
0 .62 1.24mi
Box 12-1a, p. 331
Box 12-1b, p. 331
Fig. 12-23a, p. 332
Fig. 12-23b, p. 332
Fig. 12-23c, p. 332
Fig. 12-24a, p. 333
Fig. 12-24b, p. 333
Fig. 12-25, p. 334
Fig. 12-26, p. 334
Fig. 12-26, p. 334
0 10
km
Massachusetts
Elizabeth Islands
Recessional moraine Atlantic
OceanTerminal moraines
Martha's Vineyard
Moraine Present land
Nantucket
Cape Cod
Fig. 12-27, p. 334
Fig. 12-28a-c, p. 335
Fig. 12-28a-c, p. 335
Fringing reef Barrier reef Atoll
a b c
Fig. 12-28d, p. 335
Fig. 12-29, p. 336
Fig. 12-30, p. 337
Fig. 12-30, p. 337
a Drowned river mouth b fjord
c Bar-built d Tectonic
Mainland
Lagoon
Barrier islands
Ocean
Fig. 12-31, p. 338
Fig. 12-31, p. 338
River
Seawater
a Salt wedge
Fig. 12-31, p. 338
River
Seawater
b Well-mixed
Fig. 12-31, p. 338
River
Seawater
c Partially mixed
Fig. 12-31, p. 338
River
Seawater
d Fjord
Fig. 12-32, p. 338
Fig. 12-32, p. 338
Lat
itu
de
38.0 24.00
0.00
Longitude–76.0
Fig. 12-33, p. 339
Fig. 12-34, p. 340
Fig. 12-35a, p. 341
Fig. 12-35b, p. 341
Fig. 12-36, p. 342
Fig. 12-36, p. 342
(a) Groin Groins are structures that extend from the beach into the water. They help counter erosion by trapping sand from the current. Groins accumulate sand on their updrift side, but erosion is worse on the downdrift side, which is deprived of sand.
Current
(b) Seawall Seawalls protect property temporarily, but they also increase beach erosion by deflecting wave energy onto the sand in front of and beside them. High waves can wash over seawalls and destroy them and property.
(c) Importing sand Importing sand to a beach is considered the best response to erosion. The new sand often is dredged from offshore, can cost tens of millions of dollars, and can disturb aquatic biodiversity. Because it is often finer than beach sand, dredged sand erodes more quickly.
Fig. 12-36, p. 342
(a) Groin Groins are structures that extend from the beach into the water. They help counter erosion by trapping sand from the current. Groins accumulate sand on their updrift side, but erosion is worse on the downdrift side, which is deprived of sand.
Current
(b) Seawall Seawalls protect property temporarily, but they also increase beach erosion by deflecting wave energy onto the sand in front of and beside them. High waves can wash over seawalls and destroy them and property.
(c) Importing sand Importing sand to a beach is considered the best response to erosion. The new sand often is dredged from offshore, can cost tens of millions of dollars, and can disturb aquatic biodiversity. Because it is often finer than beach sand, dredged sand erodes more quickly.
Stepped Art
Fig. 12-37, p. 342
Fig. 12-38, p. 343
Fig. 12-38, p. 343
Alaska region Great Lakes region
28
66North Pacific region
1310 1391
14 North Atlantic region
5 7 1390California region
8180
3 9
Hawai’i regionPuerto Rico and the Virgin Islands (included in South Atlantic – Gulf region)
Percent stableTexas Gulf region
182
Percent noncritical erosion Lower
Mississippi region
Percent critical erosion
86 80
South Atlantic – Gulf region
6
74
88
72
104