Calcite Reaction Calcite is composed of calcium, carbon and oxygen CaCO 3 = Calcium Carbonate Found naturally as calcite and chalk Acid reacts and gives.

Slides:



Advertisements
Similar presentations
Formation of Calcium Carbonate
Advertisements

By Ryan Arthur and Kole Patton
Earth Science 13.2A Paleozoic Era : Life explodes
Common Missouri Fossils. Trilobites Trilobites are extinct sea creatures that were one of the first forms of life on earth. They ruled the world before.
How Sedimentary Rocks are Formed. Sandstone In an area where sand is deposited.
Sedimentary rocks. A. Formation: COMPACTION & CEMENTATION 1. Sedimentary rocks form from the COMPACTION & CEMENTATION of rock fragments/sediments 2. Lithification:
Sedimentary Rocks Sedimentary rock is formed by weathering and erosion
Rocks that are formed in flat layers called strata
 A rock is a naturally occurring solid mixture of one or more minerals, or organic matter  Rocks are classified by how they are formed, their composition,
Eathering rosion eposition HILL ROCK HILL BASIN. CHEMICAL WEATHERING ACTIVITY LIMESTONE ROCK Materials: limestone chalk vinegar pipette.
1Daily Warm-Up Exercises Day 43 What processes can be observed in a stream table? erosion, transport, and deposition What causes weathering? Weathering.
How the Grand Canyon Was Formed Erosion- water, wind, and ice Volcanism Continental Drift Erosion- ice will harden and make the land expand. When the.
By Jaleen,Daisy,Alejandro,Oscar &Nicolas About the Grand Canyon!
Determining the Age of Rocks
Fossils.  Latin- “have been dug up”  There are 3 things that make a fossil a fossil:  Organic- The remains or evidence of something once living. 
Weather And Erosion Project By Taylor, Hannah, and Aaron.
THE GRAND CANYON BECAME A NATIONAL PARK IN 1919 IN ORDER TO GIVE IT THE BEST PROTECTION WE (AS A NATION) HAVE TO OFFER.
بسم الله الرحمن الرحيم Modes of preservation
Historical and Stratigraphic Analysis of the Grand Canyon By: Jake Halfhill.
The Early Paleozoic Fauna: Ordovician radiation of the Cambrian survivors EPSC233 Earth & Life History (Fall 2002)
The Early Paleozoic Fauna: earliest animal reef formers
Paleozoic Life Invertebrates. Major invertebrate phyla evolved in the Cambrian Trace fossils common Echinoderms diverse Trilobites, inarticulate brachiopods,
Section 2: Precambrian Time and the Paleozoic Era
Reading the Rocks! Geologists read layers of rocks like pages in a book! Each rock tells a story of the environment in which it formed! Tropical Ocean.
Why learn about Sedimentary Rocks Source of building materials Source of fossil fuels (oil,coal,etc) Fresh water source Evidence of past surface conditions.
Cambrian Period.
Late Paleozoic Seas EPSC 233 Earth & Life History (Fall 2002)
Daily Warm-Up Exercises
The Grand Canyon NATIONAL PARK By Allyson Curran.
Quick-write Why do you think some rocks fizzed with acid?
FOSSILS By: Brianna McCormick, Hannah Feder, and Natalie Gabel.
Fossil Lab. Hypothesis Question: –What do these different ‘rocks’ that are millions of years old tell us about the history of life on Earth? Answer: CHANGES.
Fossil Lab: Grand Canyon. A Little Photo Gallery from the Canyon….
S E D I M E N T A R Y R O C K.
Ammonites Jurasic Age approx. 146 – 200 million years old Class: Cephalopod Modern Relatives: squid, snails.
Geological age of rocks by animal & plant remains.
Kyle Howard Martha Flores Jonathon Blackmore Dykinga, J. (Photographer). (n.d.). 125 years of grand canyon photography. [Print Photo]. Retrieved from
FOSSILS IDENTIFICATION AND CLASSIFICATION. Linnean Classification Geologists classify fossils using the same classification for living things: Kingdom,
+ Fossils. + Goals Compare and contrast fossils. Use descriptions to determine the type of fossilized organisms. Use an index fossil guide to infer the.
Paleontologist: studies life that existed in pre-historic times.
Today’s Plan: -Rock Correlation -Vocab -Acid Test 01/20/11 Rock Correlations#3 Learning Target: - I can create a model showing the rock layers in the Grand.
Precambrian Time and the Paleozoic Era
Diversity of marine animals, and extinction events over geologic time.
Daily Warm-Up Exercises
Section 2: Precambrian Time and the Paleozoic Era
Earth History Limestone
Lesson 2 Date: LT: I can make observations, analyze data, and identify patterns to make inferences about the history of a place. Sponge: What is the.
Sedimentary rocks.
Section 2: Precambrian Time and the Paleozoic Era
Sponges do not have a digestive system, circulatory system, or nervous system. They do not have organs. Sponges.
Section 2: Precambrian Time and the Paleozoic Era
WU: As a group put the Nankoweap rocks in order from upper
Inarticulate brachiopods survive today with shells very similar to those of their early Ordovician relatives. Most use their long pedicle to anchor themselves.
Fossils Earth Science 11.
Sedimentary Rock Environments
And changes in organisms
Section 2: Precambrian Time and the Paleozoic Era
The atmosphere and the ocean surface are the largest reservoirs of easily obtained Carbon dioxide. These serve as the sources of Carbon dioxide for plants.
Fossils in Missouri By: Miss Barnes.
4-3 Sedimentary Rock—usually forms under water
LECTURE 4: PALEOZOIC ERA Cambrian/Ordovician Periods
How Sedimentary Rocks are Formed
Nitrogen, Oxygen, Carbon and Water
Illinois Ecosystem Was It Always Like This?.
Determining the Age of Rocks
4-3 Sedimentary Rock—usually forms under water
4-3 Sedimentary Rock… usually forms under water
Fossils Earth Science 11.
How Sedimentary Rocks are Formed
Presentation transcript:

Calcite Reaction Calcite is composed of calcium, carbon and oxygen CaCO 3 = Calcium Carbonate Found naturally as calcite and chalk Acid reacts and gives off carbon dioxide (CO 2 )

Formation of limestone Calcium carbonate becomes so concentrated in the sea water that calcite crystallizes out of the sea water to form limestone. Most limestone forms with organisms usually found at the bottom of shallow seas.

Fossil Groups Corals Sea creatures Live solitary or in colonies Brachiopods Shellfish Attached to sea bottom Bivalves Shellfish Two hinged shells Examples are clams and mussels Gastropods Snail like animals Single shell

More Fossil Groups Trilobites Extinct sea creatures Earliest form of arthropod Crinoids Known as sea lilies Marine creatures that attach to a seabed Plant Fossils Ferns are typical of floodplains and swamps

Fossil Evidence Kaibab Formation Braciopods/ sponges 260 million years old Toroweap formation Brachiopods, bryozoans 260 million years old

Coconino Sandstone Fossils of animal tracks Lizard tracks 270 million years old Hermit Shale Fern and insect wings 275 million years old

Supai Group No Fossils million years old Redwall Limestone Braciopods 360 million years old

Temple Butte Limestone Primitive armored fish, conodonts 385 Million Years Muav Limestone Brachiopods, trilobites 530 million years old Bright Angel Shale Trilobites, burrows, tracks and trails of snails worms and trilobites 540 million years old Arthropods- insects, arachnids, crustatians

Tapeats Sandstone Tubeworm burrows 545 million years old Vishnu Schist No fossils 1.7 billion years old