Presentation is loading. Please wait.

Presentation is loading. Please wait.

Tennessee Field Diamonds 2 A treasure 485 million years in the making. Please view in edit mode to see notes.

Published byFelix York Modified over 9 years ago

Similar presentations

Presentation on theme: "Tennessee Field Diamonds 2 A treasure 485 million years in the making. Please view in edit mode to see notes."— Presentation transcript:

1 Tennessee Field Diamonds 2 A treasure 485 million years in the making. Please view in edit mode to see notes

2 Weathering of carbonate bedrock Crystals freed from carbonate bedrock now in residual clay.

3

4

5

6

7

8

9 Tennessee Field Diamonds A treasure 485 million years in the making.

10

11

12

13

14 Tennessee Field Diamonds A treasure 485 million years in the making.

15 Tennessee Field Diamonds A treasure 485 million years in the making.

16

17

18 Fincher Farm area (Locality 12) Kingsport Formation, Knox Group dolomites.

19

20

21

22

23

24

25

26

27

28

29

30

31

32

33

34

35

36 Crystals from a small deposit near I-81 Exit 8 (locality 10) Jefferson County, TN Quartz_crystals_3.ppt Quartz_crystals_3.ppt

Download ppt "Tennessee Field Diamonds 2 A treasure 485 million years in the making. Please view in edit mode to see notes."

Similar presentations

Soil The product of weathering of rocks

Soil The product of weathering of rocks
Richmond's Weathering A GIS Lesson.

Richmond's Weathering A GIS Lesson.
How do soils form? Soil Profiles

How do soils form? Soil Profiles
How Do Soils Form? CLORPT for short

How Do Soils Form? CLORPT for short
Chapter 2 Weathering & Soil

Chapter 2 Weathering & Soil
Renewable and Nonrenewable Resources Environment and Ecology Standards 4.2 – A.

Renewable and Nonrenewable Resources Environment and Ecology Standards 4.2 – A.
Hydrologic Cycle Aquifer—a body of rock or sediment that stores, filters, and transmits water through pore spaces and openings in the rocks.

Hydrologic Cycle Aquifer—a body of rock or sediment that stores, filters, and transmits water through pore spaces and openings in the rocks.
The Rissa Landslide By Peter Salvin & Oliver Daffarn.

The Rissa Landslide By Peter Salvin & Oliver Daffarn.
Sedimentary Rocks Chapter 4 Section 4.

Sedimentary Rocks Chapter 4 Section 4.
Sedimentary, my dear Watson

Sedimentary, my dear Watson
Gully Erosion and Freeze-Thaw Processes in Clay-Rich Soils, Northeast Tennessee, USA Nicolas Barnes, Ingrid Luffman, and Arpita Nandi, Department of Geosciences,

Gully Erosion and Freeze-Thaw Processes in Clay-Rich Soils, Northeast Tennessee, USA Nicolas Barnes, Ingrid Luffman, and Arpita Nandi, Department of Geosciences,
Soil Processes on Hillslopes Based on work by Arjun Heimsath (Dartmouth), Bill Dietrich (UCB), and Kyungsoo Yoo (UCB) Physical movement of soil occurs.

Soil Processes on Hillslopes Based on work by Arjun Heimsath (Dartmouth), Bill Dietrich (UCB), and Kyungsoo Yoo (UCB) Physical movement of soil occurs.
Class 8a: Weathering and mass wasting. Gradational processes 1.Weathering 2.Mass wasting 3.Erosion/deposition.

Class 8a: Weathering and mass wasting. Gradational processes 1.Weathering 2.Mass wasting 3.Erosion/deposition.
The “Master” horizons O A E B C R organic horizon on the soil surface

The “Master” horizons O A E B C R organic horizon on the soil surface
Weathering and Soils The Rotting Earth Physical weathering processes Chemical weathering processes Factors affecting weathering Soil: The residue of weathering.

Weathering and Soils The Rotting Earth Physical weathering processes Chemical weathering processes Factors affecting weathering Soil: The residue of weathering.
Soil as a Resource Chapter 11. Figure 11.8 Soil Formation Soil – several ways to define –Unconsolidated material overlying bedrock –Material capable.

Soil as a Resource Chapter 11. Figure 11.8 Soil Formation Soil – several ways to define –Unconsolidated material overlying bedrock –Material capable.
1 Tennessee Higher Education Commission Tennessee’s Outcomes-Based Funding Formula: An Analysis of the First Two Years For more information, visit tn.gov/thec.

1 Tennessee Higher Education Commission Tennessee’s Outcomes-Based Funding Formula: An Analysis of the First Two Years For more information, visit tn.gov/thec.
Soil Formation Soil – weathered particles of rock, minerals and organic material (from living things) 1. Residual Soil – formed from the local bedrock.

Soil Formation Soil – weathered particles of rock, minerals and organic material (from living things) 1. Residual Soil – formed from the local bedrock.
Key Terms: weathering, mechanical weathering, chemical weathering, sediment, erosion, deposition, compaction, cementation.

Key Terms: weathering, mechanical weathering, chemical weathering, sediment, erosion, deposition, compaction, cementation.
Landforms change by processes A process is the act of doing or making something by following a set of steps Example of a process.

Landforms change by processes A process is the act of doing or making something by following a set of steps Example of a process.

Similar presentations

Ads by Google