Description
Peamen
otus
tuft
-
praps gas
a temp
Composedon MAFIC
Agruous Rocks: textures: Glassy. Vesianlar to o porous Cooling: Slow Modrats fast slantun first
Porphyritie wased o n B
loumpy graim
a I Felsicl intermedian
cause of melting: weating, decompression,
Mafic Phra Manic" coarse I Gran
addition of water Diorite I Gabbro Peridotte / source of incama: mantle mafic. conto cristal Fine / Rngolite Andente Basalt Komatite
. Occon consts felsic intermediate Pacollian Pumice If you want to learn more check out What are the six types of hypothesis-testing?
Storat
I meltinge mid atlantic nage & decompession
1 magnal "& amante & Ooerustifte Volearriz breccia
S&MATIC Rock Besalt & gabbro Ocean Contental subduction - Addition of water magma (matic) T melting = Add water & Heat - Picks up Felste minerals making and esite Don't forget about the age old question of What does locard's principle state?
Aesthenosphere rises * Source of Mayma Mantle, cont, crust
Decompression melting
Intrusive * qut Felsic Intrusive rocks (granite) vintravediate Andesite
Porote Extrusive Intermediate
Andestur- Extruse intrmediate * Rhyolite forms al Decamp. & Heating Melts manter ocen crust If you want to learn more check out What were the highlight during the jim crow era?
Cranite- Intrusing frelsis
Photo •ENu64ң с Volcanoes varies wide * Viscosity , Trapped cases, tectonie setting a viscosity: Tviscosity = 1 Resistance
MAFC ERUPTIONS = Hotspots Midocean Ridge
Hazards Ashy Debris, Pyroclastic Flow, Lahar EX & Matic : Shielda Lava Flows (Fountain), Volcanic Ash
Lassvisous = easy flow, MONITERANLY
gases escape Intermediate composite vis, convergent boundenes
Magna - More explosions, Ash Fall
INTER. FELSIC
Tectonic
brem Ridge Kubduction continental Felic = High visce osity, Dome, Caldera Vis (Yellowstone) setting Hotspot tone Hotspot - Highly explosive @ continental Hotspots If you want to learn more check out Why do seasons occur?
Volcano, a g Composite couldron, Dome
Explosion sheila TRA Malle MOST Rav New earthquakes? •Volcano swelling
1. Marthe Mix marthat groundsnelliy Magna
Continental
teatens cont.crust METAMORPHIC ROCKSE Heat + Pressure transform, recrystall zaten Rocks, Besett Andesite Rhyolite Forces push pull shess & Furce Area Contiming. All directions same l rocks If you want to learn more check out What were the challenges faced by the media agencies in 19th century?
becera Differentiala diff. dift directors inermisive Gabbro Diorite Granite 3Types DFF Stress (u) compersoner snetto FRACTURE
tu a deep a Flow-can metamorphis by recrystalication L (3) Shear TYPES OF FRACTURES : Brittle deformation crack where pulled apart="JoiNE"
LING WALL If you want to learn more check out Why did the mesopotamians invent the ziggurats?
fracture where she past the other & FAULT Chemical Proc.
During Metan.. in Normal = tension stress
Syneling room Toutwall
s pressure Schating &T
Greisst Highest grade &
Remobilization Rhyoliteschist movespest
Physical proc. + Gneiss
Climate + Streams flivers : BASALT Greens chist + Gnation
Deformation - Rotation
longer wavelengting: less energy 5 andstone
. Quartz Igneous)
luuses : foressure relaystal
it greenhouse gase tim long wavelengh Aug umestone Marble Co. River-largest in co
•Teet. Sress Poles colder ble of smaller flux sun
Fluids Jo East us : mon niver systems / Amosonore pressure weight of atmosenere
Temp. River Approrance due brownage Besin - Cache La parare
Athlude to press the
CONTACT: Just Heat to • Velocity . soins south Platte.
Regional = FLUIDS. STRESS Coriolis effect.Earth rotates East, vegitation prost important topography Lock Isoil tye
Higher precipitation geomorphology
Air risestcookt. J WHE- Nora Hemopanese deflects (R) Volume of the discharon
Dry where air dessends-Poles a feequator geel E-W (rastenies) climate
Air teses equator sinks @ 30°
Sourg Hamigohesso deflects (L) Iponce size
Streame Slope
Velout
ring niners - erode outside, build up inside Sediment
Sediment
n* DISCHARGE: Area * Velouty
Dise Remoral scale omloup . (Q) gradient honzontal anstence
volcanic
BAB
O LÚNE Recrystalizatora
sheering.
Sediment
Buildupa
SEO
Oron
Ocecco
1. Plate Tectonics: Thickest layer = Mante. ronniced core Ocean Ocean convergent
1 Lithosphere = plek
Alfred wegner-Father. Quan crust Danger-colder Asthenosphase not/weak, mostly solid Continental
Eartnquakes @ ant. ocean convergent Volcanoes @ocean ocean divergent
ocean-ocean divergent
odcen cont. convergent transform
• hotspots acord cont, cont. convergent
Mountains a cont. collision
- conto ocen convergent No volcanoes @ Cont.cont. collians, no subductus
theek corest "can" but rare.
DIVERGENT
Cont. cont. = RIFTING Ocean Ocean Divergend. Ridge
Oleme ocean. EARTHQUAKES
Convergent: Ocean continental
Trench-Sehrent can become Rift where they
new cruto se a que nosphere diverge.
Crust
continental crust MINERALS (1) Defried (2) Solid
water relesed (3) Natural (1) Inorganic (5) ordered
- Atombound w/4 oxygen Internal structure (6) Speatic Chemical Comp. atoms, bound to elements ...
CO3 Calcite silicatetrahedron? Silicate concept Map: Carbonates selecated most common
oBicooks. Feldoppen Mica pu scome. Native ar telasses tee 504 Querte ich fFelse Silicates Biotite
Sulfaut
frelsies L
Sheets Loxidest Halides sulfidel-Metal & suffer (31) Framemarly 5:04 Double Amphobite
Metal oxygen & Halogens.
pyrite
Chain
(Matic) thematite Naci (salt)
individually single 2 Breaks
Olivine (ona Fesou) Fe2O3
[chaint Pyroxen
en (Music)
Mafic) . Cleavage. Mineral break in certain directions Other: calcite dissolved in acid ço. Minerals Molybdenum Alloying for steel & Gold/siwer Gypsum-plaster Ceramics :
subducts
ca Makovile Felse
Typsum
conoido..
Geologictime Prinuple of super position - older deposits under younger deposits Nenconformity forms by Panuple of original Horizontality-deformations happen
w Rock uploféesleroded
Fossils preserved in looking Center Grosir buried beneath Poneipe of inclusion included rock is older - Bones Replacement Pisconformity forms: Panciple of cross-cutang relationships Fractures younger
o castimold impressions •Weaturing erodes surfence
thin Film Amber Deposit of horizonted lovers Principle of contact dark rock is younger, clikes younger
65 Mateo Cenozoic - Mammals + grasses. 11- Fauet offsets lava flow al zsinat Mesozoic - Dino's + flowering plants
& corp canyon Carved in the it. -10 adaug
42Mt Paleozoic - wral, plants, insects Plowf
4500 a younger Precambrian simple creatures " RADIOACTIVE DECAY G Odisconformity Potassium Argon Half-Lifes Parent Isotope=1
Corban ly & Mitron
D.Ebanghe quant zo lake thonunt Uranium & lead on 2 Rubidium Stronium
0.75 Dauchle 0.25 panty rzlit WUDZUMU
Radioactue Isotopes unstable I LAD Reservoir rocka a guifer Isclopes Sure protons, vie, electrons] Coal: plant materia Ilored
- seal - impermeable (shale)
different # of neutrons.
Traps = Anticlines OILFIELDC limestones sandstone
ne Nuclea-figsinn splite uzrsus production micreased then
deeneased bc Natural G Deswoire sandstone under limestona hor zortead online more efhcient: Rousront Ain growinter
Cheapert more efhcient potentrant Sources: DA KOTA TNIOBRARA hydromlie freekinga intreenselen Palotity by
Rexerrois = LYONS, DAKOTA
- infection Guronium ore vo concedo Oil Shale - low q. Tareenas.
Source rocka orgingtonique isotope: Semua peptons
N
un
carbonico