ANALYSIS of UTAH LANDFORMS

Know the "rules" of interpreting rock sections... older than, younger than... meaning... MATERIALS

 

Monument Valley exercise -- Rules to remember ... Super____; Cross-______; Tilting means _____.

 

Roll out the nine chapters of Utah's geologic past... for Salt Lake County... note... not to scale for time... Chapter 1 is over half of the timeline!

 

 

Now... shift to LANDFORMS that we see and the processes that have made them look the way they do.

MANTRA!! TECTONICS RULE... All landforms are the product of TECTONICS and Erosion/Deposition. .

 

Utah has three physiographic provinces . Why is that?

 

BIG CONCEPTS of PHYSICAL GEOGRAPHY

REGIONS – one of 5 "Great Themes" of geography

REGIONS are relatively extensive areas that are more similar within their boundaries than beyond their boundaries. They are drawn by people who have opinions as well as knowledge on the subject. Regions are based on spatial variation of a SPECIFIC CHARACTERISTIC. For example, regions based on surface water = drainage basins LINK.

 

Physiographic provinces are (by definition) regions based on LANDFORMS. LINK to HUNT; UT-HUNT

 

Repeat: TECTONICS RULE!! Landforms result from processes of TECTONICS and EROSION/DEPOSITION … usually both sets of processes working in tandem. Reminder... LINK

 

TECTONICS is the Great Cause of Earth’s Uplifts (and down-warps, down-drops… but not down-cuts) Reminder... Earth's crust is THIN "deep in Earth's crust" is not proportionately far. LINK

 

ISOSTASY (floats like an iceberg) is included in TECTONICS as is volcanism and other igneous activity. LINK http://www.see.leeds.ac.uk/structure/dynamicearth/topo/isostasy.htm LINK re NAm; LINK re Bonneville

 

So… today… we’ll discuss

TECTONICS

Global --

Regional --

Local –

Global -- DANCE of the PLATES. – USGS Dynamic Planet; DETAIL plates, USGS Plate Boundaries -- Look at the map.

Regional – Interactive UNAVCO http://www.unavco.org/software/visualization/GPS-Velocity-Viewer/GPS-Velocity-Viewer.html

Screen shots from the website: Basin and Range LINK; WesternUS LINK; WesternHemisphere LINK.

-- UNAVCO LINK And underlying mantle LINK and the result LINK

Local – evidence of GPS; evidence of seismic activity

Re-enact the spreading of the Basin and Range -- teams of two.

LINK; evidence of faults LINK Little Cottonwood; LINK to Utah Faults

 

 

LANDFORMS… how divide into regions? topography? LINK; same info, DEM? Sterner; physiographic provinces by landform; RiddAtwood; Ridd landforms, GA provinces.

 

BandR; RckyMth, ColoPlateau

and regions relate to human geography... cities... hospitals

 

ANALYSIS OF UTAH LANDFORMS by PHYSIOGRAPHIC PROVINCE

I. Basin and Range physiographic province

Tectonic setting – extensional and active… thin crust being ever stretched out and broken

BLOCKS

Landforms:

Big expressions: basins and ranges ... wonderful images by BOWEN (wendover looking east) or could do GOOGLE EARTH and, of course HAMBLIN House Range

Local expressions:

·       closed basins (and closed basin lakes, sediment depo-centers, shorelines, etc) LINK

·       fault related (scarp, chopped off mountain fronts with chopped off whatever-was-in-the-way, triangular facets, greatest snow on Earth, etc)

·       ranges (run north south because extension pulls east west, low at both ends and high in the middle, usually one side steeper than the other because range front faults are usually not equally active)

·       Low is depositional = basins with basin fill

Basin and Range characteristics LINK

 

II. Rocky Mountain physiographic province

Tectonic setting – very stable, thick crust, isostatic equilibrium… (does not play well with others)

Landforms: (plastic relief map) BOWEN Uintas looking west; HAMBLIN Uintas ; Google Earth (active)

Big expressions: major massive mountainous terrain with broad “parks”

Local expressions:

·       Mountains of many shapes and sizes (depending on erosion/deposition histories)

·       Drainages of many shapes and sizes

·       Lots of glacial activity (more farther north)

·       Both erosion and deposition. Both bedrock and sediments.

·       Low and erosional = valleys, “open” not closed, marshes, fresh water lakes

 

III. Colorado Plateau physiographic province

Tectonic setting – very stable…. And rising isostatically (not fast and pretty evenly) because so much material is being eroded, the “base of the iceberg” rises … may be confusing… land surface gradually lowering, but rock units rising. Careful… the upwarps and downwarps pre-date “today’s” conditions. HAMBLIN - Grand Staircase; HAMBLIN - Gr Staircase Sketch; HAMBLIN Monument Valley; BOWEN Grand Co; BOWEN San Juan; Google Earth (live)

Landforms:

Big expressions: big bold brassy red extensive, nearly-flat lying, relatively undisturbed, layered sedimentary bedrock exposed as plateaus, mesas, etc.

Local expressions:

·       Mesas, etc

·       Low and erosional = canyons

 

BIG QUESTIONS:

How did the high country get high? – By province…

How did the low country get low? – By province…

Is the high country getting higher?

Is the low country getting lower?

 

Tectonics sets the stage…

Erosion / deposition act on it

 

LAKE BONNEVILLE STORY.

What is essential for having a lake?

 

Great Salt Lake 1960s;

Great Salt Lake 1980s;

Concept of a hydrograph.

Concept of a closed basin... review... what has made the basins of the Basin and Range? Mantra!!

 

What if climate changed from hot and dry of the past 10,000 years to wetter and colder?

 

Present thoughts about why? and how often? Ice Ages have happened "recently"

Mantra!!

Global Glacial versus Global Interglacial times LINK NOAA conveyor belt LINK

Great Salt Lake and Lake Bonneville Map 73 LINK; Just Great Salt Lake LINK; Just Lake Bonneville LINK ; Shorelines - LINK

 

 

Calendar exercise (not for 2015)

Identify the province; point to (even if you don’t know their names) several landforms in the photo.