Dating Techniques and Varnish. Dating Rock Art Relative Dating –Degree of weathering –Superimposition analysis –Stylistic analysis –Spatial Analysis (Inter-Site.

Slides:



Advertisements
Similar presentations
How do soils form? Soil Profiles
Advertisements

UNIT C. Section 1 Basic Principles of Agricultural/Horticultural Science.
Basic Principles of Agricultural/Horticultural Science
Soil Physical Properties – Colour, Texture, Structure
Soil formation begins with weathering of bedrock
WELCOME BACK!.
What Did I See at Vasquez Rock? Follow-up to our class trip to Vasquez Rock.
Soil Horizons. Organic Layer (O-horizon) The uppermost layer; it is rich in organic material. Plant litter accumulates in the O- horizon and gradually.
SOIL. WHAT IS SOIL? SOIL IS A MATERIAL THAT FORMS THE CRUST OF THE EARTH. IT COMES FROM THE WEATHERING OF ROCKS AND DECOMPOSITION OF ORGANISMS. IT IS.
Weathering and Soil Formation
Chapter 2 Section 1 Pages Rocks and Weathering Chapter 2 Section 1 Pages
Do You Remebmer? Sedimentary Rocks Chapter 6. What Are Sediments? ______________________ In order of decreasing size.
Physical weather reduces the particle size of rocks and in doing so prepare the material for chemical weathering. The rate of all chemical reactions involving.
Chapter 2 continued 2:1 phyllosilicates (Chlorites) Non-silicates.
1 Important/significant foundation soil physical properties Color Redoximorphic features Texture Structure Consistence Coarse fragments Reaction.
Weatheri ng Weathering is the physical and chemical breakdown of rocks at the Earth’s surface. The pieces or particles of rock (large and small) that are.
Weathering and Erosion
Soil as a Resource Chapter 11. Figure 11.8 Soil Formation Soil – several ways to define –Unconsolidated material overlying bedrock –Material capable.
Soil Color GES 394 Revised by Mr. Brian Oram
Weathering and Erosion Weathering is… When rocks are broken apart and create sediments.
Formation of Sedimentary Rocks
Jeopardy Rules A square can only be selected once. Write your responses on the answer sheet. You must respond with a question.
Weathering and Soil. Types of Weathering Chemical Weathering: a rock being changed into 1 or more new compounds Oxidation- turns the rock into a rusty.
Igneous and Sedimentary Rocks SWBAT explain how extrusive and intrusive igneous rocks are different; describe how different types of sedimentary rocks.
Weathering and Erosion. Weathering The process that breaks down rocks and other materials of Earth’s crust into smaller pieces.
Chapter 7- Weathering, Erosion and Soil
Weathering,Soil and Glacial Movement
Ocean-Floor Sediments (19.3)
Soil as a Resource Chapter 12. Soil Formation Soil – several ways to define –Unconsolidated material overlying bedrock –Material capable of supporting.
Weathering,Soil and Glacial Movement Ch. 14,15. What Physical Properties Affect Rocks Near the Surface? There are many processes that break rocks apart.
Soil Evolution Field Biology CCTI Mrs. Conway. Directions Read through the following slides while completing your lab packet. Be sure to answer all question.
AIM: What causes weathering and erosion?. Weathering is the physical and chemical breakdown of rocks into smaller pieces called sediment. Due to: Air.
Sedimentary Rocks Chapter 6. What Are Sediments? Loose particulate material In order of decreasing size.
Chapter 12 Soil Resources.
Chapter 10 - Soil Fertility. Essential Plant Nutrients - 14 are Mineral Based Macros - N, P, K, Ca, Mg, S Micros - B, Cu, Cl, Fe, Mn, Mo, Zn, Ni.
Soil Origin and Development
Topic 5 Part 1 soil.
Weathering and Erosion
Weathering Weathering is the physical breakdown and chemical alteration of rocks and minerals. Weathering happens on or near the surface. Weathering is.
Weathering of Rocks. Why we see weathering 1.Most minerals are not stable at the Earth’s surface 2.The Earth wants to be flat – lowest energy state Topography.
Chapters 4 & 5 Weathering and Erosion Weathering Weathering is the breaking down of rocks and other materials 2 types of weathering –Mechanical –Chemical.
Soils. Formation of Soils Physical Weathering Rain, wind, abrasion Chemical Composition is not altered Influenced by climate Chemical Weathering Acid.
Ch 5 - Soils Important effect of weathering for people!
Weathering Chapter 10. Essential Questions What causes mechanical weathering? What causes chemical weathering? What factors determine how fast weathering.
Soil is made of loose, weathered rock and organic material.
Soils.
Soil Section 5.2.
AIM: What characteristics are used to identify rocks and what are the three main groups of rocks? OBJ: Given notes and activity sheet SWBAT explain the.
Rocks and Weathering Chapter 2 Section 2 6 th Grade Team.
What is chemical weathering?
Chapter 37 Plant Nutrition. Uptake of nutrients in plants: Leave and roots.
Origins- parent material; mixtures of eroded rock, mineral nutrients, decaying organic matter, and billons of living organisms (mostly decomposers)
Soil By: Alejandro Meza Moreno Lina Lovera Valeria Morales.
SOIL: A RENEWABLE RESOURCE Soil is a slowly renewed resource that provides most of the nutrients needed for plant growth and also helps purify water. Soil.
Frost Heaving. Plant Roots (Root Pry) Talus Water.
ROCKS & MINERALS.  Minerals are always solid with particles in repeating patterns- crystals  They are only found in Nature.  They are formed in the.
Weathering and Erosion. 1.Weathering – The chemical and physical processes that break-down rock at Earth’s surface. 2.Mechanical weathering – The type.
Soils: A brief introduction
Chapter 14: Weathering.
CHAPTER 4: Marine Sediments at ECC
Weathering Weathering is the physical and chemical breakdown of rocks at the Earth’s surface. The pieces or particles of rock (large and small) that are.
CHAPTER 4: Marine Sediments at ECC
Rocks and Minerals Sedimentary rocks.
Vocab Riddles.
Rocks & Weathering Chapter 3.
Weathering: Chemical Weathering: the breakdown of rock into sediments
Weathering Chemical and Physical & Erosion.
How Soil Forms Types of Soil
Classifying Rocks 6.E.2.1 Summarize the structure of the Earth, including the layers, the mantle and core based on the relative.
Three Basic Definitions
Presentation transcript:

Dating Techniques and Varnish

Dating Rock Art Relative Dating –Degree of weathering –Superimposition analysis –Stylistic analysis –Spatial Analysis (Inter-Site Patterning)

Dating Rock Art Absolute Dating –Historical information –Subjects –Stratified art –Association –Direct dating

ROCK ART DATING TECHNOLOGIES Amino Acid Racemisation AMS OSL Lichenometry Micro-erosion analysis

Rock / Desert Varnish Explained

Rock / Desert Varnish a biogenic deposit produced by mixotrophic bacteria living on rock surfaces, digesting organic debris. Layers may reach ages of 10^3 10^5 yrs Tiny Elvis Layers

Rock / Desert Varnish Environment –Arid – Semiarid environments are optimal for growth Hyper-arid environments lack water for bacterial growth Mesic environments: lichen growth destroys rock varnish

But what is it? It is a coating of clay particles with minerals deposits of iron and manganese oxides. Mostly wind blown. Other Minerals Include- –hydroxides plus silica and calcium carbonate

So how’s it formed? Nobody knows. Theory is… –Manganese oxides in rock varnish block the transmission of ultraviolet radiation. –SPF 300 for microbes?

Why the variety in color and appearance? Rate of bacterial growth relative to clay accumulation produces appearance –dark dull varnish = bacterial dominant light shiny varnish = clay dominant Fluctuations in clays and Fe and Mn oxides and hydroxides produce color –black: manganese-rich red: iron-rich