Paleoclimate
plate technics
Dissecting
ocean zones
coral
100

what is paleoclimatology 

its the study of past climates 

100

what is divergent boundaries

where new crust is generated as the plates pull away from each other 

100

whats a prob

slender pointed tools with one or both ends tapered to a fine point

100

where is the epipelagic zone located  

the top layer 

100

what are the 2 kinds of coral

stony and soft

200

why is paleoclimatology important

its important for the past and future issues 

200

what is it called when plates come together 

convergent boundary 

200

whats a scalpel

a small sharp knife with fine pointed blade

200

what does abysso stand for

extreme depth

200

what way does pillar coral grow 

up and down

300

how are other proxies used 

combinations of proxy data are generally used to reconstruct records for past climate

300

where do most movements happen in the earths crust

Atlantic ocean

300

what are dissecting pins for

used to secure specimens within the dissecting pan and hold specimens in place 

300

where is the bathypelagic located 

under mesopelagic the 3rd layer in 

300

how many kinds of soft coral that we learned about

3

400

why do we keep these records 

they can be integrated with earths observations of earths modern climates
400

why do earthquakes shake California 

tectonic plates are close to California  

400

why do we use dissecting pans 

fluids and debris from spilling

400

what is the depth rang for hadopelagic 

 19,700-36,070 feet

400

how many kinds of stony coral that we learned about

4 kinds 

500

Where do we keep the climate records 

there places into a computer model to infer past as well as the future 

500

what is the San Andreas fault 

Boundary between the pacific and north American plates

500

are there a typer of scissors used for dissections

yes sharp pointed blades designed to cut tissues

500

what is the pressure in the bathypelagic zone

1,500-6,000

500

Encrusting coral are spreading a lot or not

low spreading.