Looks like no one added any tags here yet for you.
small shallow earthquakes on boundaries
not many volcanoes
crust slightly shallower along plate boundary
symmetrical age — newer at boundary, gets older further away
Earthquakes get shallower on side going under, get deeper as earth descends
Volcanoes along top plate parallel to boundary
Volcanic arc next to deep sea trench
Likely no symmetry, geochronology not related to convergent boundary
Lots of shallow earthquakes along the boundary
No volcanoes forming
Off-set streams, physical cracks on landscape
No formation or recycling of crust
Quartz, k-feldspar and amphibole were present
Rocks were sedimentary
Poor sorting — rocks vary greatly in size and indications of flash floods (high energy)
Sedimentary
Granite, andesite, biotite, k-feldspar, quarts, sandstone, gneiss, diorite
There is less variety than there used to be in ancient times
Form when molten rock cools and becomes solid
Cool slowly —> larger minearls (macrocrystalline)
Cool quickly —> smaller minerals (microcrystalline)
Intrusive - tend to be macrocrystalline (cool inside Earth)
Extrusive - microcrystalline (cool outside Earth)
Porphyritic - microcrystalline with scattered large crystals
Granite (k-feldspar, biotite, quartz)
Basalt (pyroxene)
Diorite (plagioclase feldspar, amphibole)
Gabbro (pyroxene, plagioclase feldspar)
Peridotite (olivine)
Porphyritic andesite (amphibole)
Porphyritic rhyolite (quartz, muscovite, amphibole)
Detrial — made of fragments of pre-existing rocks that have been broken down through weathering erosion (mudtsone, shale, sandstone, breccia and conglomerate)
Organic — made of organic material produced by fossils (calcite)
Inorganic — formed from sediment that precipitates water — only chemical sediment (rock salt and gypsum)
Foliated — form as a result of regional metamorphism (usually directed pressure); greater degree of metamorphism → larger minerals; more metamprophism = more shiny
Non-foliated — macroscopic tecture, high temp WITHOUT direct pressure, likely consist of one mineral
Epicenter — point on Earth’s sruface above focal point
Focal point — underground origin of the earthquake
Plate tectonic motion builds up as strain within Earth taht releases along faults
Seismic waves originate at focal point and travel in all directions
Motion (slip) along fault is what people feel
Strike — line of intersection btwn inclinced plane of sedimentary bed and horizontal plane
Dip — maximum tilt angle of sedimentary bed
Topanga formation — sedimentary rock
Formed 13 million years ago (young)
Granite, quartz, k-feldspar, plagioclaste, biotite
Moved as the mountain eroded through landslides and then moved by streams/erosion to where they are
Fragments are buried and then lithification occurs → uplift happens
Crystallization of intrusive rocks
Uplift
Erosion
Sedimentation
Litification
Uplift