The Fundamental Principles of Relative DatingRelative dating involves placing events in their proper chronological sequence, that is, in the order of their occurrence (Dutch 1998). This type of dating tells us which geologic event happened first, but does not give an exact date to which something happened. There are several different methods that are used in relative dating. These are the fundamental methods that are used in the field by geologists' and earth scientists to gather information about the relative age of rock bodies and other cool geologic stuff. These principles are the principle of superposition, the principle of original horizontality, the principle of cross-cutting relationships, and the principle of inclusions.The principle of superposition is defined as in the environment of an undisturbed layer of sedimentary rocks; the layers on the bottom are older than the layers towards the top. The pictures I have taken show very good examples of this.
By using the principle of superposition we can know that the layers toward the bottom are older than the layers toward the top. The rock body shown in the pictures attached, started out as one layer, as millions and millions of years passed more layers of sedimentary rock were placed on top of each other one after another, each layer was deposited at a later time than the one before it. The youngest layer is on the top, and the oldest layer is on the bottom. This principle was founded by the Danish anatomist Nicolas ...
This sedimentary rock has hardened over the many years with sand shells, small pebbles, grains of sand and rocks of various sizes. In comparison to our 4.5 billion year old Earth, these sand shells might as well be brand new, when in reality they could be up to 1,000 years old. If the sandstone were to be replaced with calcite it would completely change the subclass of rock, it would then be chemical & organic limestone. The variation in sand stone is due to different rates of deposition and change in patterns of the sediment movement (Mc Knight, p. 384). These tightly compacted varying stones and shells will be weathered away by wind and waves over time and could eventually be reduced to a rock the size of your hand.
"Sedimentary Rocks." Backyard Nature with Jim Conrad. N.p., 18 May 2015. Web. 25 Oct. 2015.
Charles Lyell Charles Lyell was a British lawyer and one of the smartest geologists known at his time. He was known as the author of the Principles of Geology, which helped popularize the theories and concepts of uniformitarianism. The Principles of Geology was the first book written by Lyell and explained the changes in the earth’s surface. He used the research and information in the book as his proof to determine that the earth was over 6,000 years old. The central argument in his book was “the present is the key to the past”, this meant that to find out what happened in the past you had to look at what was happening now.
While the carbon 14 method provided approximate dates for the stone rings it was no use
1. Since interracial marriage became legal in 1967, only 7.5 percent of marriages are between people of different races. This means America is progressing, but it is not yet “color-blind”. People of different races are starting to date more (which shows the progression) but it is less likely to lead to marriage, compared to same race couples. Henderson and Rockquemore talk about how Americans believe we have developed a “color-blind” society, but they don’t specify what American think that or where the information comes from. This means the Americans they are referring to could all be in same race relationships. If that is the case, then the people who it matters to the most, the people in interracial relationships, might not think the same. Henderson and Rockquemore then go on to say, people in interracial relationships feel unique external pressures due to racism,
The Don Valley Brickwork consists of many different layers of geological deposits, allowing us to observe and have a better understanding of how the sediments we see today are formed. The most bottom layer in the Brickworks are from the Georgian Bay Formation, and consists of grey- shale bedrocks. Fossils are often found in this layer and it is estimated that this deposit of sediments is around 445 million years old. Above the bedrocks is a thin layer of grey clay sand and gavels left behind by the Illinoian Glacier. This layer is called the York Till and occurred around 135,000 years ago. The next layer consists of a sandy deposit called the Don Formation, which is formed by the Sangamonian Interglacial Stage. Many plant and animal fossils are found in this layer due to warmer climate around 120,000 years ago. Above it lies the Scarborough Formation, which consist of clay and sand. This sediment likely occurred 115 - 106,000 years ago. The next layer above is the Poetry Road Formation, and consist of sand and gravel. This layer is likely formed during the early Wisconsin glacial substage around 106- 75,000 years ago. Higher is the Sunnybrook Drift which was formed 60 – 75,000 years ago. And on the surface, is the Halton Till, which was left behind by the final push of the Wisconsin Glacier.
regions of the earth can indicate which rock layer is older than the other. Trilobite fossils
The Permian Period occurred around 298 million years ago. It stretched from the Carboniferous Era to the Triassic. Sir Roderick Murchison in the early 1800’s noticed a differentiation among the overlay of the rock formation in the Ural Mountains in Russia. These rocks differed from the older Carboniferous rocks in Britain, and seemed younger than the Triassic rocks of Europe. Murchison named this differentiation after the prehistoric kingdom of Perm, thus the Permian Period.
Paleogeologist knows a fossilization process only begins when an organism dies and immediately covers with mud or silt before it gets ruined by scavengers. After being covered under earth’s surface, minerals in the water replace the minerals in the organism’s tissues, and bones are the most common tissues for mineral replacements. Because the soft parts of the body usually decays and left with the hardest parts to be buried. After much time has passed the body of the organism will slowly turn into a sedimentary rock. This process would sometimes take up to millions of years; therefore fossils do not form easily.
The cycles of the ocean waters rising (transgressing) and receding (regressing) are known as transgressive-regressive cycles. The mid- to Upper Cretaceous rocks in the Big Bend area of southwest Texas encompasses rock ages from approximately 70 to 100 million years ago (mya). During this time the sea transgressed and regressed a number of times. The final regression of the Cretaceous sea occurred about 70 million years ago, during the Late Cretaceous period, at the time of the Aguja Formation deposition. By observing the transgressive and regressive cycles of the Mid to Upper Cretaceous period a reasonable prediction of ocean depth over time can be made. Fossil data from the mid to Upper Cretaceous period predicts the sequence of rock strata in Big Bend National Park to be from bottom to top: limestone (containing clams, oysters, and ammonites), shale and clay (containing shellfish and marine reptile bones), limestone again, and sandstone and clay (both containing fossil wood and dinosaur bones) (Maxwell, 1967). Assuming that the rocks on the bottom are the earliest layer, it may be concluded that the earliest layer of rock was deposited in a relatively deep marine environment, then the ocean regressed to produce the next layer, then transgressed to produce the last.
The geologic history of the Rocky Mountains has come about as an aggregation of millions of years. Briefly speaking, the formation of the Rockies transpired from hundreds and millions of years of uplift by tectonic plates and millions of years of erosion and ice have helped sculpt the mountains to be what we see today. The majority of the rocks that make up the Rocky Mountains began as simple shale, siltstone, and sandstone accompanied by smaller amounts of volcanic rock which formally built up for approximately 1.8 to 2 billion years in the ancient sea. By 1.7 to 1.6 billion years, these sedimentary rocks got caught in the zone of collision between parts of the earth’s crust and its tectonic plates. The incredible heat at the core of the mountain range then recrystallized the rock into metamorphic rock by the heat and pressure of the collision forces. Eventually, the shale would be transformed into both schist and gneiss. It is believed that granite found in the Rocky Mountain parks came from pre-existing metamorphic rock created shortly after the formation of the earth. Ultimately, the high mountains of the period were slowly eroded away to a flat surface exposing metamorphic rocks and granite. This process occurred around the period of 1,300 to 500 million years ago. This flat surface would become covered with shallow seas and rocks from the Paleozoic period and would be deposited and eventually cover the surface. There is...
Because these creationists call their endeavors scientific, the question arises as to their method for making the claim of a young earth. Creation-science discussions of the age of the earth usually contain several standard items. The first is usually a criticism of the standard evolutionist methods for age determination, radiometric dating.
Thousands of years ago when sea levels dropped over years at the Southern end of Muriwai, the sedimentary rock and sandstone was exposed to the air. Rock from volcanic activity mixed with the sedimentary rock; this is called Breccia -- a mixture of all rock. An example of this is at Maori Bay.
Radiocarbon dating is used to tell how old something is. When some normal carbon gets hit by the rays of the sun it turns into carbon 14. Plants absorb this radioactive carbon in the form of carbon dioxide. Animals receive this carbon from eating the plants. When the organism is dead it loses the carbon 14. Scientists can tell how old something is based on the amount of carbon 14 in a dead object. Carbon dating is accurate if the amount of carbon 14 in the atmosphere has remained the same throughout time. The second is if carbon 14 has always decayed at the same
The field of geology has many different branches. Some of these areas have hardly anything in common. The one thing that they all include, though, is that each one concentrates on some part of the Earth, its makeup, or that of other planets. Mineralogy, the study of minerals above the Earth and in its crust, is different from Petrology, the st...