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viva [34]
3 years ago
8

What is the special features of the rock chert?

Biology
2 answers:
tensa zangetsu [6.8K]3 years ago
5 0
Tbh irdk srry :-'''''''''''''''''''''''''''''''''''''''''''''''''''''''''''(
Sophie [7]3 years ago
4 0
Any good rockhound is bound to come across a rock that he or she has trouble identifying, especially if the location of where the rock was found is unknown. To identify a rock, think like a geologist and examine its physical characteristics for clues. The following tips and tables contain characteristics that will help you identify the most common rocks on earth.

Rock Identification Tips

First, decide whether your rock is igneous, sedimentary or metamorphic.

Igneous rocks such as granite or lava are tough, frozen melts with little texture or layering. Rocks like these contain mostly black, white and/or gray minerals.Sedimentary rocks such as limestone or shale are hardened sediment with sandy or clay-like layers (strata). They are usually brown to gray in color and may have fossils and water or wind marks.Metamorphic rocks such as marble are tough, with straight or curved layers (foliation) of light and dark minerals. They come in various colors and often contain glittery mica.

Next, check the rock's grain size and hardness.

Grain Size: Coarse grains are visible to the naked eye, and the minerals can usually be identified without using a magnifier. Fine grains are smaller and usually cannot be identified without using a magnifier.Hardness: This is measured with the Mohs scale and refers to the minerals contained within a rock. In simple terms, hard rock scratches glass and steel, usually signifying the minerals quartz or feldspar, which has a Mohs hardness of 6 or higher. Soft rock does not scratch steel but will scratch fingernails (Mohs scale of 3 to 5.5), while very soft rock won't even scratch fingernails (Mohs scale of 1 to 2). 

Rock Identification Chart

Once you've determined what type of rock you've got, look closely at its color and composition. This will help you identify it. Start in the left column of the appropriate table and work your way across. Follow the links to pictures and more information. 

Igneous Rock Identification

Grain SizeUsual ColorOtherCompositionRock Typefinedarkglassy appearancelava glassObsidianfinelightmany small bubbleslava froth from sticky lavaPumicefinedarkmany large bubbleslava froth from fluid lavaScoriafine or mixedlightcontains quartzhigh-silica lavaFelsitefine or mixedmediumbetween felsite and basaltmedium-silica lavaAndesitefine or mixeddarkhas no quartzlow-silica lavaBasaltmixedany colorlarge grains in fine-grained matrixlarge grains of feldspar, quartz, pyroxene or olivinePorphyrycoarselightwide range of color and grain sizefeldspar and quartz with minor mica, amphibole or pyroxeneGranitecoarselightlike granite but without quartzfeldspar with minor mica, amphibole or pyroxeneSyenitecoarselight to mediumlittle or no alkali feldsparplagioclase and quartz with dark mineralsTonalitecoarsemedium to darklittle or no quartzlow-calcium plagioclase and dark mineralsDioritecoarsemedium to darkno quartz; may have olivinehigh-calcium plagioclase and dark mineralsGabbrocoarsedarkdense; always has olivineolivine with amphibole and/or pyroxenePeridotitecoarsedarkdensemostly pyroxene with olivine and amphibolePyroxenitecoarsegreendenseat least 90 percent olivineDunitevery coarseany colorusually in small intrusive bodiestypically graniticPegmatite

 

Sedimentary Rock Identification

HardnessGrain SizeCompositionOtherRock Typehardcoarseclean quartzwhite to brownSandstonehardcoarsequartz and feldsparusually very coarseArkosehard or softmixedmixed sediment with rock grains and claygray or dark and "dirty"Wacke/
Graywackehard or softmixedmixed rocks and sedimentround rocks in finer sediment matrixConglomeratehard or
softmixedmixed rocks and sedimentsharp pieces in finer sediment matrixBrecciahardfinevery fine sand; no clayfeels gritty on teethSiltstonehardfinechalcedonyno fizzing with acidChertsoftfineclay mineralssplits in layersShalesoftfinecarbonblack; burns with tarry smokeCoalsoftfinecalcitefizzes with acidLimestonesoftcoarse or finedolomiteno fizzing with acid unless powderedDolomite rocksoftcoarsefossil shellsmostly piecesCoquinavery softcoarsehalitesalt tasteRock Saltvery softcoarsegypsumwhite, tan or pinkRock Gypsum

 

Metamorphic Rock Identification

FoliationGrain SizeUsual ColorOtherRock Typefoliatedfinelightvery soft; greasy feelSoapstonefoliatedfinedarksoft; strong cleavageSlatenonfoliatedfinedarksoft; massive structureArgillitefoliatedfinedarkshiny; crinkly foliationPhyllitefoliatedcoarsemixed dark and lightcrushed and stretched fabric; deformed large crystalsMylonitefoliatedcoarsemixed dark and lightwrinkled foliation; often has large crystalsSchistfoliatedcoarsemixedbandedGneissfoliatedcoarsemixeddistorted "melted" layersMigmatitefoliatedcoarsedarkmostly hornblendeAmphibolitenonfoliatedfinegreenishsoft; shiny, mottled surfaceSerpentinitenonfoliatedfine or coarsedarkdull

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The big bang produced an imprint of leftover heat called _____.
Ilia_Sergeevich [38]

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The big bang produced an imprint of leftover heat called CMB radiation

Explanation:

CMD is short for Cosmic Microwave Background

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After a huge meal how does the pancreas help maintain homeostasis
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After a large meal, the pancreas helps by producing insulin, which helps break down sugars.
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Which of the following has the most potential of experiencing background extinction based on the natural disruption described?
Neko [114]

The option that has the most potential of experiencing background extinction based on the natural disruption is : ( C ) A species that will not grow during a specific season every year

<h3>What is Background extinction </h3>

Background extinction is the gradual extinction of species due certian environmental factors such as change in weather conditions, disease, competitive disadvantage and habitat loss.

A population that will not grow during a specific season every year will experiences a gradual extinction process while other options will experience a fast and sudden extinction process.

Hence we can conclude that the most potential of experiencing background extinction based on the natural disruption is :  A species that will not grow during a specific season every year.

Learn more about background extinction : brainly.com/question/11872946

6 0
2 years ago
Describe how the changes in the temperature of water, during the change of season affect the organisms that live there? Dissolve
mestny [16]

hanges in temperature affect aquatic life. Temperature determines which organisms will thrive and which will diminish in numbers and size. For each organism there is a thermal death point. Also there is a range of temperature of that produces optimal abundance. The effects of temperature upon life of a cold blooded or poikilotherm are profound. Poikilothermic animals, such as fish, are those whose body temperatures follow closely the temperature of their medium.

These animals have coped with temperature problems in different ways. Not only the organism survival, but growth and reproduction of each organism have critical temperature ranges. Each organism must be favored by the proper temperature if the individual or its population are going to survive. For instance, temperature influences enzymatic reactions through hormonal and nervous control to digestion, from respiration and osmoregulation to all aspects of an organism’s performance and behavior.

High and low temperatures that are lethal to individual organism of a species determines the distribution and abundance it’s populations. However, more often the distribution and abundance of populations is determined by less than lethal temperatures interacting with other environmental factors that either tend to favor or not to favor reproduction and growth.

Increased water temperature is an important consideration when toxic substances are present in water. Many substances (i.e. cyanides, phenol, xylene, zinc) exhibit increased toxicity at elevated temperatures. These toxicities and other physiological interactions are also influenced by temperature acclimation or history of the species.

We can gain a clearer understanding of these interactions through consideration of lethal temperature levels. In relation to the survival of individual organisms, the upper and lower lethal temperatures define the total temperature gradient. Within this temperature gradient, there is a range as shown in Figure 4 in which the species can function at or near optimum. In this range, growth and reproduction temperature requirements are met and the species will be found in greatest abundance. Outside the optimum range, there are zones of physiological stress. In these zones, organisms become infrequent because activities are limited more by temperatures that produce discomfort or stress. The period of time an organism can live under physiological stress is a function of how far the temperature is from the lethal level.

Most changes in water temperature as a result of land use activity generally trend upward. An exception is the release of cold bottom water from stratified artificial impoundments that may alter the flora and fauna for many miles downstream from a dam. Most other activities generally raise the temperature of receiving waters with the following effects:
(a) Higher temperatures diminish the solubility of dissolved oxygen and thus decrease the availability of this essential gas.
(b) Elevated temperatures increase the metabolism, respiration and oxygen demand of fish and other aquatic life, approximately doubling the respiration for a 10° C. rise in temperature. Hence the demand for oxygen is increased under conditions where oxygen supply is lowered.
(c) The solubility of many toxic substances is increased as well as intensified as the temperature rises.
(d) Higher temperatures militate against desirable fish life by favoring the growth of sewage fungus and the putrification of sludge deposits, and finally
(e) even with adequate dissolved oxygen, there is a maximum temperature that each species of fish or other organism can tolerate. Higher temperatures produce death. The maximum temperatures that adult fish can tolerate vary with the species of fish, prior acclimatization, oxygen availability and the synergistic effects of other pollutants.

Median Tolerance Limits (MTL)have been reported are shown in the following table. Species have been arranged in the order of heat tolerance. As shown by this table, Goldfish, Bass and Carp are relatively tolerant of high temperatures, whereas Trout and Salmon are more sensitive. These temperatures, however, apply to adult fish. For spawning and hatching of eggs, much lower temperatures are required. Many species spawn only above or below certain temperatures. Several species of fish and their spawning temperature ranges are shown in Figure (Cooper).



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