... Using the right-click menu isthe easiest way to add new addresses to the list However, you'll need to use this dialog to remove or edit addresses from the list The list doesn't support ... in the format of @*.microsoft.com You have to enter the entire text following the @ when you add addresses to the list After you've created a Safe Senders list, you can export it for use on other ... a Safe Senders list, you can export it for use on other computers where Outlook 2003 is installed or use it as a backup copy if you need to reinstall Outlook or Windows [ Team LiB ] ...
... three classes of antagonist, the binding of AVP was dramatically affected by the substitution of Arg46, with the affinity of AVP for all Fig Schematic diagram ofthe V1aR The V1aR is illustrated ... N-terminus ofthe V1aR; this revealed that a single residue (Arg46) located in the distal segment of this domain is critical for high affinity agonist binding but not antagonist binding [14] The corresponding ... in which the N-terminus ofthe OTR is replaced with the corresponding sequence ofthe V1aR [10] The role ofthe N-terminus has been addressed recently by alanine-scanning mutagenesis ofthe N-terminus...
... needed The cell cycleis a developmental process not a cycle If everything oscillates and does so with a period thatis an integral submultiple ofthe cell cycle, then the cell cycle, as itis conventionally ... analysis ofthe distribution of cell age at mitosis in a population of presumptive identical cells in which there is some limiting material Events within thecycle are initiated when this material ... information content ofthe system as expressed in the vectors and itis clear that in all three experiments the system is globally oscillatory The disadvantage of SVD analysis isthe difficulty of getting...
... French Ministry of Agriculture and were designed to limit animal pain and distress Infections were performed intradermally in the right ear with × 103 FFU of either virus Rabbits were monitored daily ... signs (Figure 1B) This experiment suggests thatthe main function of MNF is preserved even when MNF is fused to GFP To identify the partners of MNF, immunoprecipitations of GFPMNF were performed BGMK ... performed All the rabbit sera obtained by immunization against partof or the whole MNF protein were specific to the MYXV infection but allowed the staining of cells infected with the MYXVΔMNF...
... mineral is this? MUSCOVITE Review of Minerals What mineral CALCITE is this? Review of Minerals What mineral HALITE is this? Review of Minerals What mineral GARNET is this? Review of ... precipitate around deposited particles and bind them together The sedimentary stages oftherockcycle Weathering breaks down rocks Erosion carries away particles Transportation moves particles ... mineral is this? AMPHIBOLE HORNBLENDE Review of Minerals What mineral BIOTITE is this? Goals for this lab Learn the basics ofrock identification Learn how to distinguish between rock...
... by level of foliation: Slate-Phyllite-Schist-Gneiss • Slate: splitting surfaces at an angle to bedding • Phyllite: Phyllite similar, with platy mineral growth • Schist: segregation of platey ... are a function of P, T and rock & fluid compositions (X) at time ofthe reaction • Used to define metamorphic zones • Demonstrates progress of metamorphism REGIONAL METAMORPHISM OF SHALES LOW ... CHLORITE BIOTITE GARNET STAUROLITE KYANITE SILLIMANITE Index Minerals formed: controlled by original rock (X), P, and T ISOGRADS: lines on a geological map showing locations of first appearance of...
... -COMPOSITION= what minerals therockis made of -TEXTURE=sizes, shapes and positions of grains in the rocks TYPES OF ROCKS • THE COMPOSITION OF ROCKS IS DETERMINED -BY THE KIND OF MINERALS & -THE ... through theprocessof changing from one type ofrock to another THEROCKCYCLE Gneiss Schist (m) Phyllite (m) (m) Siltstone Shale Slate (s) (s) (m) THEROCKCYCLE Granite Sandstone (s) (i) Quartzite ... The color of rocks may be different because ofthe Breccia Sedimentary minerals or other substances that make it up Gneiss Metamorphic Quartzite Metamorphic Granite Igneous TheROCKCYCLE • Rock...
... the hot magma of batholiths L.Gardiner/Windows Original Regional Metamorphism Tectonic forces smash continents together The rocks get heated and become semi-molten The added pressure causes the ... even flow before cooling again! Common Metamorphic Rocks Parent Rock Metamorphic Rock Granite Gneiss Shale Slate Sandstone Quartzite TheRockCycle ... Crystals! Main Rock Types How to make a clastic sedimentary rock Sedimentary Main Rock Types Metamorphic rocks form from HEAT&PRESSURE Contact Metamorphism Deep underground, zones of metamorphism form...
... mixture of minerals The edges of this rock are very sharp Metamorphic Rock • Metamorphic rocks are rocks that have "morphed" into another kind ofrock These rocks were once igneous or sedimentary rocks ... layers of sediment are added The weight of all the layers presses them together and they eventually harden forming sedimentary rock 2 The sedimentary rockis pushed deeper into theearth This adds ... pebbles The sediment is so large that pressure alone cannot hold therock together; itis also cemented together with dissolved minerals Sedimentary Rock - Gypsum • Gypsum rocks are sedimentary rocks...
... Harcourt Publishing Company Unit Lesson TheRockCycle What are the classes of rocks? • Each rock class can be divided further, based on differences in the way the rocks form • Sedimentary rockis composed ... Publishing Company Unit Lesson TheRockCycle What are the classes of rocks? • Igneous rock forms from molten rockthat cools • As molten rock cools, crystals form The longer the cooling takes, the ... types can be changed into another ofthe three types • The series of processes by which rock changes from one type to another is called therockcycle • A rock s identity can be changed by factors...
... factor that can transform rocks isthe pressure caused by tons of other rocks pressing down on it from above Heat and pressure usually work together to alter the rocks under theearth' s surface This ... cools quickly on the surface Rock formed in this way is called extrusive igneous rockItis extruded, or pushed, out oftheearth' s interior and cools outside of or very near theearth' s surface ... Magma that gets pushed up toward theearth s surface cools at a much slower rate than lava The kind ofrock formed in this way is called intrusive igneous rockIt intrudes, or pushes, into theearth' s...
... all sides The pressure pushes new minerals into therock and drives other minerals out; the result, of course, isthattherockis chemically changed Weathering Theprocess in which rocks are ... parts ofthe rocks get taken all the way down to the mantle where they slowly mix with the rest ofthe mantle – this isthe only way that rocks formed on the continent get recycled with the mantle ... physical mechanisms into smaller particles There are three types of weathering Physical weathering: physical action which breaks up rocks An example of this is freethaw weathering Chemical Weathering:...
... Lee RockCycle Rap the story of Louey a piece of quartite the follows him through the 3:51 rockcycle 3:45 TheRockCycle – Reading Activity Possible! TheRockCycle – In Legos 2:20 4:29 Misc ... Misc Information and Sites Animated RockCycle Interactive RockCycle Interactive RockCycle This PPT based on this site Article for Kids – RockCycle Article for Kids – RockCycle http://education.usgs.gov/lessons/schoolyard/RockSedimentary.html ... Erosion Deposition TheRockCycle n io Er os k rlin pe y H Igneous Rock to am yJ ud t S 3:0 EROSION – the removal of soil and rock by natural processes such as Igneous rockis formed through...
... Metamorphic Rock Melting Magma/Lava Rockcycle website RockCycle Song (Sing to the tune of "Row, Row, Row Your Boat") SEDIMENTARY rock Has been formed in layers Often found near water sources With fossils ... crystals The Three Types ofRock Sedimentary Sandstone Shale Conglomerate Form when grains ofrock (sediments) collect and harden into new rocks The Three Types ofRock Metamorphic Schist Gneiss ... So…what isthe difference between a rock and a mineral? A mineral is a naturally formed solid material with a crystal structure Quartz Biotite mica Feldspar So…what isthe difference between a rock...
... THEROCKCYCLE Relative proportions ofrock groups Sedimentary rocks: larger proportion of land surface The greater proportion created by weathering, erosion & deposition These are ... Textural maturity refers to: – The degree of roundness ofthe grains – The amount of sorting ofthe grain sizes • Texturally mature sandstones have well-rounded and well-sorted grains, immature ... Evaporite (chemical) sediments • halite, gypsum and anhydrite • Dolomite, also as dolomitisation of calcite Classification of clastic sediments: The Wentworth Scale Grain Size Sediment Grade >256 mm...
... -COMPOSITION= what minerals therockis made of -TEXTURE=sizes, shapes and positions of grains in the rocks TYPES OF ROCKS • THE COMPOSITION OF ROCKS IS DETERMINED -BY THE KIND OF MINERALS & -THE ... PRESSURE RockCycle Animations • You choose the path • Rocks forming THEROCKCYCLE • One ofthe cycles of nature that continually recycles rocks & limestone materialsthat make up Earth s crust ... slate gneiss ROCKCYCLE • There are many different paths a rock may follow to go through theprocessof changing from one type ofrock to another THEROCKCYCLE Gneiss Schist (m) Phyllite (m)...