The Example of the Lake Missoula Flood

Similar documents
Channelized Flood Flow Cuts Water and Wind Gaps

Sculpted by Floods Learning Resource Guide

Hydraulic Modeling of the Missoula Ice Dam Failure. Christopher R. Goodell, P.E., D.WRE WEST Consultants, Salem, OR

One of the tasks of the Floods Study Team was to determine if any new facilities

Gravel Transport Can Determine Late Flood Tectonics

Inselbergs Left Behind on Planation Surfaces by Flood Runoff

The Puzzle of Large Natural Bridges and Arches

Uniformitarian Speculations on Gravel Transport East

EXTENSION MODULE A. Introduction. B. Dynamics of Glacial Lakes

Pediments Formed in the Retreating Stage of the Flood

Earth Science Chapter 6 Section 2 Review

Glacial Deposition and Groundwater in Dutchess County

Science EOG Review: Landforms

The Geology of Sebago Lake State Park

mountain rivers fixed channel boundaries (bedrock banks and bed) high transport capacity low storage input output

Weathering, Erosion, and Deposition

Chapter 12: River Systems and Landforms

ALBERTON GORGE WATER RIPPLE ROCKS

Eric Clausen 1. Correspondence: Eric Clausen, Independent researcher, Jenkintown, PA, USA.

Lecture Outline Lecture Outline Monday April 9-16, 2018 Questions? Announcements:

Title: A case for repeated outburst floods for the creation of the Channeled Scablands:

Columbia River Gorge Near Perfection... And Only 40+ Million Years in the Making

THE BEDROCK SURFACE AND FORMER DRAINAGE SYSTEMS OF MONTGOMERY COUNTY, OHIO 1

Cattaraugus Creek: A Story of Flowing Water and the Geology of the Channel It Flows Through Presentation to West Valley Citizen Task Force 4/27/16

The Little Colorado River

WISSAHICKON CREEK DRAINAGE BASIN ORIGIN AS DETERMINED BY TOPOGRAPHIC MAP INTERPRETATION INTRODUCTION

THE GEOLOGY OF SCULPTING STONE COLUMBIA RIVER BASALT

The Tualatin a n d Yamhill Valleys In Northwest Oregon

Why is Sebago Lake so deep?

Mystery of the Megaflood

CASE STUDY #9 - Brushy Fork Dam, Sugar Grove, West Virginia

Vantage/Columbia Basin Field Trip

Quartzite Gravel Locations in Oregon

Channeled scablands of eastern Washington: the geologic story of the Spokane flood

ACCUMULATED PRECIPITATION IN INCHES

Page 1. Name:

High Impact Forces of Nature Hazards in and Around Rocky Mountain National Park


Mountain Rivers. Gutta cavat lapidem. (Dripping water hollows out a stone) -Ovid, Epistulae Ex Ponto, Book 3, no. 10, 1. 5

Which landscape best represents the shape of the valleys occupied by glaciers? A) B) C) D)

COLUMBIA THE MAGAZINE OF NORTHWEST HISTORY SPRING 2005 $7.50

THE MISSOULA FLOOD OVERVIEW

Up to 45,000 Feet of Differential Vertical Tectonics Wyoming

Using topographic map interpretation methods to determine Tookany (Tacony) Creek erosion history upstream from Philadelphia, Pennsylvania, USA

Name: Which rock layers appear to be most resistant to weathering? A) A, C, and E B) B and D

Massive Erosion of Other Coastal Great Escarpments

The Grand Canyon is one of the world s most awesome erosional features.

Waterbury Dam Disturbance Mike Fitzgerald Devin Rowland

Chapter 3 Erosion and Deposition. The Big Question:

THE JUAN DE FUCA LOBE OF THE CORDILLERAN ICE SHEET

4. The map below shows a meandering stream. Points A, B, C, and D represent locations along the stream bottom.

Devil s Punchbowl -Virtual Field Trip-

Ch 10 Deposition Practice Questions

What is weathering and how does it change Earth s surface? Answer the question using

Running Water Earth - Chapter 16 Stan Hatfield Southwestern Illinois College

2. What type of rocks would you expect in this area, based on the topography? What is your reasoning?

1. What define planetary surfaces geologically? 2. What controls the evolution of planetary surfaces?

discussion of North America s physical features, including its landforms and bodies of

Part IV Quartzite Rocks Transported Long Distances Northwest States and Adjacent Canada

Today I will describe the groundwater/surface water interaction in the CRB in Mosier basin.

Possible Confusion in Identifying Surficial Planation Surfaces

Summary. Streams and Drainage Systems

Mount St. Helens. Copyright 2010 LessonSnips

PHYSICAL GEOGRAPHY. By Brett Lucas

WITTKOP, BENNETT, CHORMANN AND WUNSCH

1 INTRODUCTION AND MAJOR FINDINGS... 1

ES 105 Surface Processes I. Hydrologic cycle A. Distribution % in oceans 2. >3% surface water a. +99% surface water in glaciers b.

Final Exam. Running Water Erosion and Deposition. Willamette Discharge. Running Water

APPENDIX 3B OCCURRENCE OF SIGNIFICANT RIVER ALLUVIUM AQUIFERS IN THE PLATEAU REGION

GEOL 1121 Earth Processes and Environments

GIFFORD PINCHOT STATE PARK DIABASE (MOLTEN LIQUID ROCK)

Erosion and Deposition

STAAR Science Tutorial 40 TEK 8.9C: Topographic Maps & Erosional Landforms

Pat Dryer Half Moon Lake: A True Oxbow Lake? Geography 364 April 1 st, 2007

EROSION AND DEPOSITION

11/12/2014. Running Water. Introduction. Water on Earth. The Hydrologic Cycle. Fluid Flow

Erosion Surface Water. moving, transporting, and depositing sediment.

Changes to Land 5.7B. landforms: features on the surface of Earth such as mountains, hills, dunes, oceans and rivers

Why study physical features? How does it help me during the course of studying Geography Elective?

Think about the landforms where you live. How do you think they have changed over time? How do you think they will change in the future?

The subject paper is being submitted for approval for publication in the annual volume entitled Geological Survey Research.

Multi Hazard Evaluation of a High Voltage Transmission Network. John Eidinger 1 and Leon Kempner 2

STREAM SYSTEMS and FLOODS

Precipitation Evaporation Infiltration Earth s Water and the Hydrologic Cycle. Runoff Transpiration

Extra Credit Assignment (Chapters 4, 5, 6, and 10)

Essential Questions. What is erosion? What is mass wasting?

THE TOPOGRAPHY AND GEOLOGY OF THE GRAND PORTAGE^

ACCUMULATED PRECIPITATION IN INCHES

Aerial Views of Lakes. Michael Collier, Image Source: Earth Science World Image Bank

STUDENT NAME. Science Grade 5. Read each question and choose the best answer. Be sure to mark all of your answers.

Analyzing Rivers with Google Earth

APPENDIX E. GEOMORPHOLOGICAL MONTORING REPORT Prepared by Steve Vrooman, Keystone Restoration Ecology September 2013

Streams. Stream Water Flow

Principles of Geology

Fluvial and Glacial Landforms of West-Central Wisconsin

Thin, Widespread, Sedimentary Layers

Basin & Range / Mojave Desert

KRIS wsbssm. IBHiiilll

W he natural resources of Adams

UNSTOPPABLE COLLAPSE OF THE WEST ANTARCTIC ICE SHEET IS NOT HAPPENING

Transcription:

Chapter 85 The Example of the Lake Missoula Flood As already noted, uniformitarian hypotheses rarely, if ever, can be supported by extensive geological evidence. Part of this is due to the nature of the features, since they originated in the past. The same charge could be leveled against Flood explanations. However, geomorphological evidence for the Retreating Stage of the Flood is strong, as this ebook shows. Whereas uniformitarian scientists have to invent speculative secondary hypotheses to salvage their paradigm in the light of conflicting evidence, the Flood paradigm does not need to invent secondary hypotheses, because the evidence is consistent with the paradigm. Furthermore, the Flood paradigm has an example of how a well-substantiated catastrophic flood at the peak of the Ice Age created a water and wind gap. 1 The Lake Missoula flood (earlier called the Spokane or the Bretz flood) demonstrates catastrophic floods can easily produce water and wind gaps. Figure 85.1. Glacial Lake Missoula as shown on a kiosk sign at Lake Pend Oreille. 1 Oard, M.J., 2004. The Missoula Flood Controversy and the Genesis Flood, Creation Research Society Monograph No. 13, Chino Valley, AZ.

The Lake Missoula Flood One of the largest lakes ever ponded by an ice dam was glacial Lake Missoula (Figure 85.1). After this lake deepened to 2,000 feet (610 m) at the dam site in northern Idaho, the bursting ice dam initiated one of the largest floods on earth, except that described in Genesis. Glacial Lake Missoula contained 540 mi 3 (2,210 km 3 ) of water and emptied in two days. It rushed through eastern Washington and the Columbia River gorge at velocities over 65 mph (100 kph). It spread through eastern Washington at a width of 100 miles (160 km). The water was about 600 feet (180 m) deep as it sped across Spokane, Washington; 1,000 feet (300 m) deep channeling through the Columbia gorge; and 400 feet 9120 m) deep when it flowed over the Portland, Oregon area. Figure 85.2 is a satellite image of the flood path. It shows well because the flood eroded the lighter silt and exposed the dark basalt below. What you see is a braided drainage pattern over 100 miles (160 km) wide in eastern Washington! Figure 85.2. Satellite picture of the flood path. Many geologists today conjecture dozens of Lake Missoula floods at the peak of the last ice age because of the uniformitarian paradigm. However, the evidence is abundant that there was only one major flood possibly followed by a few minor ones. 2,3,4,5,6 2 Oard, Ref. 1, pp. 37-57. 3 Oard, M.J., 2003. Evidence for only on gigantic Lake Missoula flood. In, Ivey, Jr., R.L. (editor), The Fifth International Conference on Creationism, technical symposium sessions, Creation Science Fellowship, Pittsburgh, PA, pp. 219-231. 4 Oard, M.J., 2000. Only one Lake Missoula flood. Journal of Creation 14(2):14-17. 5 Oard, M.J., 2012. Further evidence of only one large Lake Missoula flood. Journal of Creation 26(3):3 4.

The Lake Missoula flood produced many water and wind gaps along the flood path. Paul Bishop stated in regard to the Lake Missoula flood: Catastrophic divide breaching and drainage rearrangement are prominent features of the Channeled Scabland of northwest USA 7 I will focus on only one prominent water and wind gap. Figure 85.3. Map of ridge between Washtucna Coulee and the Snake River, showing Palouse Canyon, a water gap, and Devils Canyon, a deep wind gap, cut during the Lake Missoula flood (redrawn from Bretz, 1928, p. 205 by Mark Wolfe). Palouse Canyon Water Gap One major pathway of the Lake Missoula flood was the Cheney-Palouse scabland tract in the eastern part of the flood path. The southern portion of this tract includes Washtucna Coulee. Prior to the flood, the Palouse River rising from the mountains of northern Idaho flowed westward through this coulee and then into the Columbia River. The Snake River flows parallel to the Washtucna Coulee about 10 miles (16 km) south. There is an east-west basalt ridge that was covered by about 100 feet (30 m) of the Palouse silt between the Snake River and Washtucna Coulee. This ridge is about 500 feet (150 m) above the Snake River. The Lake Missoula floodwater rushed south into the head of Washtucna Coulee. It overtopped the ridge between Washtucna Coulee and the Snake River at generally four locations, forming a water gap and one deep wind gap (Figure 85.3). At the head of one Palouse Canyon its width was initially around 8 miles (13 km), and left behind a number of currentaligned silt hills just west of Palouse Canyon between the water and wind gap (Figure 85.4). But 6 Oard, M.J., 2014. The Lake Missoula flood clues for the Genesis Flood. Creation 36(2):43 46. 7 Bishop, P., 1995. Drainage rearrangement by river capture, beheading and diversion. Progress in Physical Geography 19(4):461.

the flow narrowed, cutting a vertically-walled, meandering canyon 500 feet (150 m) deep down to the level of the Snake River (Figure 85.5). The narrow canyon likely was formed by a retreating waterfall from above the Snake River north to Washtucna Coulee. After the flood, the Palouse River, instead of continuing its flow westward through Washtucna Coulee as before, took a 90 left hand turn and flowed through what is now called Palouse Canyon and into the Snake River. Palouse Canyon is therefore a water gap formed during the Lake Missoula flood. Palouse Falls would then represent one of the last knickpoints of the retreating waterfall (Figure 85.6). Figure 85.4. Current aligned silt hills just west of Palouse Canyon.

Figure 85.5. Narrow-walled, meandering Palouse Canyon downstream from Palouse Falls.

Figure 85.6. Palouse Falls in Palouse Canyon, southeast Washington.

Devils Coulee Wind Gap The Lake Missoula flood also breached the ridge between Washtucna Coulee and the Snake River 15 miles (24 km) west of Palouse Canyon. A narrow notch called Devils Coulee, 500 feet (150 m) deep was eroded through the ridge (Figure 85.7). However, the Lake Missoula flood did not eroded this coulee deep enough at its entrance from Washtucna Coulee. The entrance to Devils Coulee is approximately 100 feet (30 m) above Washtucna Coulee (Figure 85.8), and no stream can flow through it. So, Devils Coulee remains a wind gap. Figure 85.7. Devils Coulee looking north from near the Snake River. Large Floods Cut Downstream Water and Wind Gaps Therefore, Palouse Canyon and Devils Coulee are examples of how large volumes of energetic floodwaters can rapidly excavate water and wind gaps in hard rock. 8 The carving of these gaps occurred well downstream from the breach and was caused when the flow overtopped the ridge between Washtucna Coulee and the Snake River, very similar to the schematic shown in Figure 84.1. Like all analogies, the Lake Missoula flood situation is a bit different than the Flood situation. In the Lake Missoula flood, the water rose to overtop the ridge at low points, while in the Genesis Flood the water was subsiding when it carved gaps through the low points in the ridge. The main point though is: water and wind gaps formed during the Flood in much the 8 Oard, Ref. 3, pp. 228-229.

same way as the Lake Missoula flood by flood water racing and channelized across a rock barrier. Figure 85.8. The entrance to Devils Coulee looking south from Washtucna Coulee. Note the rise at the entrance of the canyon prevents water from flowing from the coulee down Devils Canyon to the Snake River.