Download presentation
Presentation is loading. Please wait.
Published byAnissa McBride Modified over 7 years ago
1
Warm-up Week 2 # 2 ______ are associated with mid-ocean ridges.
a. rift valleys c. extreme temperatures b. mountainous topography d. volcanic structures The gently sloping submerged surface extending from the shoreline toward the deep ocean is called ____. a. continental shelf c. continental rise b. continental slope d. submarine canyon Differences in ocean-surface height can be measured by ____. a. sonar c. submersibles b. satellites d. none of the above
2
“Composition of Seawater”
15.1
3
Q: How is ocean water different than fresh water?
Dissolved substances Taste! Smell!
4
Composition of Seawater
What it’s ________ of. 3.5% dissolved minerals Salts! MADE
5
“Salinity.” “Salinus” = salt
Salinity = amount of salt dissolved in water Parts per 1000 = ‰ Most of the salt in seawater = common table salt.
6
Sources of Salts Weathering! Earth’s interior!
Chemical weathering of rocks on continents Erosion by rivers Deposition in ocean Earth’s interior! Volcanic eruptions
7
What affects Salinity? Amount of salt is constant
Amount of water changes
8
Ocean Tempo Variation. Tempo changes with Solar Radiation.
Latitude. Tempo changes with depth. Thermocline = “heat” + “slope” Layer of ocean water with fast change in tempo.
9
Density Variation Density = Mass ÷ Volume ↑ Dense = Sinks ↓
How heavy for size… ↑ Dense = Sinks ↓ ↑ Salinity = ↑ Density ↑ Tempo = ↓ Density
10
THERMOCLINE PYCNOCLINE
11
Ocean Layers Layered by density. Transition Zone Surface Zone
Thermocline Pycnocline Deep Zone No sunlight Cold & Dense Layered by density. Surface Zone Shallow Mixed (waves & wind)
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.