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Geologic formation in Arizona, USA
The Redwall Limestone is an erosion-resistant, Mississippian age, cliff-forming geological formation that forms prominent, red-stained cliffs in the Grand
Redwall_Limestone
Cambrian geologic formation found in the Southwestern United States
the limestones of the Muav Limestone are the result of such transgressive and regressive events. Muav Limestone cliff example, below Redwall Limestone cliff
Muav_Limestone
Landform
Redwall Limestone, large cliff. Also being a cliff-former, the curving "tail-of-the-alligator" is a flat-topped platform of the Redwall Limestone. The
The_Alligator_(Grand_Canyon)
Landform in the Grand Canyon, Arizona
locally karsted topography and caves developed in the top of the Redwall Limestone. The Surprise Canyon Formation and associated unconformities represent
Surprise_Canyon_Formation
Summit in the Grand Canyon, Arizona
cliff-forming, typically massive Redwall Limestone, (as in the connected Tower of Set southwards). The base of the Redwall has a short, but resistant cliff
Horus_Temple
Geologic formation in the Grand Canyon
siltstone and gray limestone and fills small erosion channels cut into either the Surprise Canyon Formation or Redwall Limestone. The upper and lower
Supai_Group
Landform in the Grand Canyon, Arizona
up about one fourth of the battleship landform. The striking west Redwall Limestone cliffs, surmounted by the orange-reddish slopes of Supai Group “redbeds”
The_Battleship_(Grand_Canyon)
Ridgeline summit in the Grand Canyon
bright-red, tall Redwall Limestone. Being a cliff-former, the Redwall is also a platform-former. The upper platform of the Redwall Limestone supports a remainder-debris
Swilling_Butte
Landform in the Grand Canyon, Arizona
cliff-former, (and therefore platform-former), of Redwall Limestone. The Supai Group (and Redwall), massifs are also found on the parent (and connected
Dunn_Butte
Summit in Coconino County, Arizona
cliff-former massif of the Redwall Limestone. Interestingly, two rock units, commonly thin layers, are found, one on top of the Redwall platform (a cliff-former
The_Howlands_Butte
Landform in the Grand Canyon, Arizona
Asbestos Canyon. At the southwest of Krishna, on an extending arm of Redwall Limestone is a short unnamed drainage; (at the southwest is Newberry Butte at
Krishna_Shrine
Landform in the Grand Canyon, Arizona
Pyramid is a flat-topped erosional remnant composed of Mississippian Redwall Limestone, overlaying the green shale slopes of the Cambrian Tonto Group, and
Cheops_Pyramid
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at creek
Vishnu_Temple_(Grand_Canyon)
Aspect of geology
column is the cliff-forming Redwall Limestone, which is 400 to 800 feet (120 to 240 m) thick (see 4b in figure 1). Redwall is composed of thick-bedded
Geology of the Grand Canyon area
Geology_of_the_Grand_Canyon_area
Landform in the Grand Canyon, Arizona
Sandstone (Supai unit 4) Manakacha Formation (Supai unit 2) Redwall Limestone Muav Limestone (short platform & cliff) all sitting on slopes of dull-greenish
Dragon_Head_(Arizona)
Topics referred to by the same term
Football Team Redwall Limestone or Redwall Formation, rock layer that forms prominent, red-stained cliffs in the Grand Canyon, Arizona Redwalls, The Homestead
Red_wall
Landform in the Grand Canyon, Arizona
sequence of 'redbeds', the cliff-forming Redwall Limestone sits above highly eroded slopes of Muav Limestone and Bright Angel Shale. These slopes are
Isis_Temple
Landform in the Grand Canyon
cliff-forming Redwall Limestone, with vegetation growth. The east flank of the Redwall is slightly arcuate, and the prominence, upon the Redwall Limestone, is also
Whites_Butte
Cambrian geologic unit in the Grand Canyon region, Arizona
(peak) to its left). Vertical erosion in cliff of Redwall Limestone, upon horizontal Muav Limestone cliff. The Tapeats Sandstone sits in foreground on
Tonto_Group
Landform in the Grand Canyon, Arizona
cliff-erosion-remnants of Redwall Limestone, (very vertical and very narrow, ~north-south aligned), upon a platform of Muav Limestone; as unit three of the
Sheba_Temple
Summit in the Grand Canyon, Coconino County, Arizona
wide); (See here:) both units are on the top platform of the Redwall, the Redwall Limestone upper platform being a common rock unit throughout the Grand
Wallace_Butte
Landform in the Grand Canyon, Arizona
trail ends at a viewpoint on the upper surfaces of a Redwall Limestone ridge. The Redwall Limestone is seen prominently below the East Rim, and is the cliff-forming
Temple_Butte
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, and finally the Cambrian Tonto Group. Precipitation runoff from Shiva
Shiva_Temple_(Grand_Canyon)
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at creek
Wotans_Throne
Landform in the Grand Canyon, Arizona
towards the Colorado. The mesa is a mostly flat upper platform of Redwall Limestone, with its tall cliffs elevating the mesa. A peak of Supai Group is
Horseshoe_Mesa
Landform in the Grand Canyon, Arizona
Interestingly the Redwall Limestone also sits on a short cliff-section of the Muav Limestone, (forming a platform); thus the Redwall-Muav Limestones are a double-platform
Tuna_Canyon
Landform in the Grand Canyon
Group ridgeline, and the spire of Dana Butte sits on the cliff-former Redwall Limestone that creates not only massive cliffs, but platforms that support younger
Dana_Butte
Cambrian geologic formation found in the Southwestern United States
between the top of the Muav Limestone and the base of either the Devonian Temple Butte Formation or Mississippian Redwall Limestone. Because of unidentified
Frenchman_Mountain_Dolostone
Grand Canyon hiking trail
switchbacks to descend the 1,200 feet (370 m) through the Redwall Limestone, Muav Limestone, and Bright Angel Shale to the junction with the Tonto Trail
South_Kaibab_Trail
Geologic formation in the southwestern United States
Reeside characterized and named the Rock Canyon Conglomerate, Virgin Limestone, and Shnabkaib Shale members in 1921. Salt Creek (later replaced by Wupatki
Moenkopi_Formation
Geologic formation of Permian age in the southwestern United States
the De Chelly Sandstone in Utah. In this area, it underlies the Kaibab Limestone. Further eastward, the Coconino Sandstone likely correlates with and is
Coconino_Sandstone
Cambrian geologic formation found in the Southwestern United States
sequence beneath the tall cliffs of the Redwall Limestone (the Redwall sits upon a short resistant cliff of Muav Limestone); the Tonto Group is also easily seen
Bright_Angel_Shale
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, the Cambrian Tonto Group, and finally granite of the Paleoproterozoic
Tower_of_Ra
Geologic formation in the Four Corners, US
and conglomerate beds alternating with reddish mudstone or clay-rich limestone. Further west, the unit shows great lithological diversity, and can be
Cutler_Formation
Landform in the Grand Canyon, Arizona
River in half a mile (1 km). Marsh Butte is composed of Mississippian Redwall Limestone, overlaying the Cambrian Tonto Group, and finally granite of the Paleoproterozoic
Marsh_Butte
Jurassic sandstone formation of the southwestern United States
The limestone appears as solid gray-blue beds, a few inches to a few feet thick, and as lenses of limestone conglomerate. Most of the limestone lenses
Kayenta_Formation
Landform in the Grand Canyon, Arizona
above photo. At the base of the large, red Redwall Limestone cliff, is the short cliff of Muav Limestone. The slope-forming, soft dull greenish Bright
Kwagunt_Butte
Section of the Colorado River in Arizona
finally abandoned in 1968. Exploratory holes, which were drilled in the Redwall Limestone of the canyon walls in an early phase of the abortive project, can
Marble_Canyon
Landform in the Grand Canyon, Arizona
the slopes of the red Supai Group members and the red cliffs of the Redwall Limestone. The slopes of the dull greenish Bright Angel Shale are the bases
Nankoweap_Mesa
Landform in Coconino County, Arizona
resistant cliff at the base of the massive cliffs of the Redwall Limestone, the Muav Limestone. Sumner Butte is a notable 5,126-foot-elevation geographical
Zoroaster_Temple
Landform in the Grand Canyon, Arizona
Supai Group. This overlays the cliff-forming layer of Mississippian Redwall Limestone, which in turn overlays Cambrian Tonto Group. According to the Köppen
Apollo_Temple
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at creek
Buddha_Temple_(Grand_Canyon)
Mesa in Arizona (western Grand Canyon)
platform of the Redwall Limestone, (a cliff-former, with massive cliffs in East Grand Canyon). Below the Redwall, is a short cliff of Muav Limestone, (but also
Fishtail_Mesa
Landform in the Grand Canyon, Arizona
they tend to merge with cliffs of the much thicker and overlying Redwall Limestone. Within the western and central parts of the Grand Canyon, the Temple
Temple_Butte_Formation
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at creek
Manu_Temple
Landform in the Grand Canyon, Arizona
peak is an erosional remnant composed of Cambrian Muav Limestone and Mississippian Redwall Limestone. Topographic relief is significant as Diamond Peak towers
Diamond_Peak_(Arizona)
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at creek
Thor_Temple
Geologic formation in North America
Formation Pakoon Limestone Queantoweap Sandstone Toroweap Formation C ⁋ Callville Limestone M Monte Cristo Limestone Redwall Limestone D Muddy Peak Formation
Willow_Tank_Formation
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group, and further down the Mississippian Redwall Limestone layer. Precipitation runoff from Brahma Temple drains south into the
Brahma_Temple_(Grand_Canyon)
Landform in the Grand Canyon, Arizona
Group. Further down are strata of the cliff-forming Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at creek
King_Arthur_Castle
Landform in the Grand Canyon, Arizona
above photo. At the base of the large, red Redwall Limestone cliffs, is the short cliff of Muav Limestone. The slope-forming, soft dull greenish Bright
Malgosa_Crest
Landform
siltstone, mudstone, sandstone, shale Rock type(s) Supai Group, Redwall Limestone, Muav Limestone, Bright Angel Shale Climbing First ascent September 3, 1961
Juno_Temple_(Grand_Canyon)
transgression and the formation of thick limestone. The Redwall Limestone in the Grand Canyon and the Esabrosa Limestone in southern Arizona, both date to this
Geology_of_Arizona
Landform in the Grand Canyon, Arizona
and famous platform-former in the Grand Canyon, is the top of the Redwall Limestone cliffs, which supports many prominences in the Grand Canyon. The prominence
Scorpion_Ridge
Steep-sided canyon in Arizona, US
area of substantial fracturing through the Redwall Limestone, Temple Butte Formation and Cambrian Muav Limestone of the Tonto Group. Five individual systems
Grand_Canyon
Landform in the Grand Canyon, Arizona
Further down are strata of the conspicuous cliff-forming Mississippian Redwall Limestone, the Cambrian Tonto Group, and finally granite of the Paleoproterozoic
Vesta_Temple
Mountain in the Grand Canyon, Arizona
from the east aspect. This butte is an erosional remnant composed of Redwall Limestone overlaying the Tonto Group. Geology of the Grand Canyon area "Fan
Fan_Island
Landform in the Grand Canyon, Arizona
Supai Group, which sit on upper platforms of the cliffs of Redwall Limestone. The Redwall sits on units of the Cambrian Tonto Group. Geology of the Grand
Mescalero_Point
Landform in the Grand Canyon, Arizona
units of Kaibab Limestone, Toroweap Formation, Coconino Sandstone, and Hermit Shale, down to Supai Group on red-cliffs of Redwall Limestone. These are the
Topaz_Canyon
Landform in the Grand Canyon, Arizona
Names. This butte is an erosional remnant composed of Mississippian Redwall Limestone, which overlays the Cambrian Tonto Group. Precipitation runoff from
Newberry_Butte
Triassic geologic unit
Mountains, and China Mountain. Calcareous shale, mudstone, and black limestones are the most common lithologies present within the unit. The member was
Fossil_Hill_Member
Topics referred to by the same term
River (at mile 35.6, approx 57.3 km on the right); it is located in Redwall limestone and has a span of 4 metres (15 feet) and a height of 9 metres (30
Bridge of Sighs (disambiguation)
Bridge_of_Sighs_(disambiguation)
Geologic formation in the Grand Canyon
Pennsylvanian-Permian strata, mostly red beds, lying between the Redwall Limestone and the Coconino Sandstone in the Grand Canyon region. In 1922, Noble
Hermit_Formation
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group which overlays cliff-forming Mississippian Redwall Limestone, which in turn overlays Cambrian Tonto Group. According to the Köppen
Explorers Monument (Grand Canyon)
Explorers_Monument_(Grand_Canyon)
Geologic formation in Utah and Arizona
Formation Pakoon Limestone Queantoweap Sandstone Toroweap Formation C ⁋ Callville Limestone M Monte Cristo Limestone Redwall Limestone D Muddy Peak Formation
Moenave_Formation
Landform in Utah and Arizona, United States
Kaibab Limestone Toroweap Formation Coconino Sandstone Hermit Shale Supai Group Surprise Canyon Formation Redwall Limestone Temple Butte Limestone Muav
Grand_Staircase
Early Jurassic geological formation in the Mojave Desert, United States
Formation Pakoon Limestone Queantoweap Sandstone Toroweap Formation C ⁋ Callville Limestone M Monte Cristo Limestone Redwall Limestone D Muddy Peak Formation
Aztec_Sandstone
Geologic prominence in northern Arizona, United States
Prominence and rock units: Coconino Sandstone-prominence, Hermit Formation, Supai Group (4-units), Redwall Limestone, Muav Limestone, Bright Angel Shale.
Escalante_Butte
Landform in the Grand Canyon, Arizona
Further down are strata of the conspicuous cliff-forming Mississippian Redwall Limestone, the Cambrian Tonto Group, and finally granite of the Paleoproterozoic
Confucius Temple (Grand Canyon)
Confucius_Temple_(Grand_Canyon)
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, and Cambrian Tonto Group. Whereas most strata of the Grand Canyon
Sinking_Ship_(Grand_Canyon)
Sinkhole in Arizona
sinkhole was formed by subsidence into caverns of paleokarst composed of Redwall Limestone of the Pennsylvanian subperiod. After the second collapse, a large
Devil's_Kitchen_Sinkhole
Geologic formation in the western United States
named the Pahasapa Limestone in the Black Hills, Leadville Limestone (Colorado), Guernsey Limestone (Wyoming), and Redwall Limestone in the Grand Canyon
Madison_Group
Landform in the Grand Canyon, Arizona
Group. This in turn overlays the cliff-forming layer of Mississippian Redwall Limestone, which in turn overlays Cambrian Tonto Group, and finally Neoproterozoic
Butchart_Butte
Landform in the Grand Canyon, Arizona
orange-red Supai Group on the upper platform of the cliff-forming Redwall Limestone, upon the Cambrian Tonto Group. Members of the Grand Canyon Supergroup
Venus_Temple
Landform in the Grand Canyon, Arizona
its depth. Beneath the Supai Group, is the platform and cliff of Redwall Limestone, and below, the three Cambrian units. When Rama Shrine is viewed from
Rama_Shrine
1942 film
Dam Isis Temple Kanab Plateau Newton Butte Ochoa Point Prospect Dam Redwall Limestone Tanner Graben Temple Butte Tonto Group Bright Angel Shale Toroweap
Desert_Wonderland
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group overlaying the conspicuous cliffs of Mississippian Redwall Limestone, in turn overlaying the Cambrian Tonto Group. Masonic Temple was named
Masonic_Temple_(Grand_Canyon)
Landform in northern Arizona
Rock type(s) Kaibab Limestone, Toroweap Formation, Coconino Sandstone, Hermit Shale, Supai Group, Redwall Limestone, Muav Limestone, Bright Angel Shale
Powell_Plateau_(Arizona)
Landform in the Grand Canyon, Arizona
Group. Further down are strata of the cliff-forming Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at river
Mount_Huethawali
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group overlaying the cliff-forming Mississippian Redwall Limestone, and Cambrian Tonto Group. Evans Butte was climbed solo by Harvey
Evans_Butte_(Grand_Canyon)
Landform in the Grand Canyon, Arizona
watershed. Hubbell Butte is composed of Supai Group units, sitting upon Redwall Limestone cliffs. The west flank of Hubbell Butte is on a north section of Lava
Hubbell_Butte
Geologic formation in Utah, United States
Formation Pakoon Limestone Queantoweap Sandstone Toroweap Formation C ⁋ Callville Limestone M Monte Cristo Limestone Redwall Limestone D Muddy Peak Formation
Nopah_Formation
Geologic unit found in the Grand Canyon
Watahomigi Formation D – Redwall Limestone – large (vertical) red cliff C – Muav Limestone – grayish-cliff (attached at base of Redwall cliffs – 40%) B – (light-greenish
Esplanade_Sandstone
in limestone caves in the inner canyon indicate ages of 3,000 to 4,000 years. In the 1950s split-twig animal figurines were found in the Redwall Limestone
History of the Grand Canyon area
History_of_the_Grand_Canyon_area
City in Arizona, United States
Shale and Muav Limestone, Martin Formation, Redwall Limestone, Supai Group, Coconino Sandstone, Toroweap Formation, and Kaibab Limestone. The last three
Flagstaff,_Arizona
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, and finally Cambrian Tonto Group at river level. The Butte Fault
Chuar_Butte
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at creek
Deva_Temple
Landform in the Grand Canyon, Arizona
layered cliff-former Kaibab Limestone, and is mostly buff, or tan-white. The rock at the point is distinctive with its limestone erosion-holes, and is broken
Mather_Point
Landform in the Grand Canyon, Arizona
Below is the Supai Group, on cliffs of Redwall Limestone, on members of the Tonto Group, namely, Muav Limestone, Bright Angel Shale, and closer to the
Cocopa_Point
United States historic place in Arizona
copper minerals in a breccia zone along a monocline flexure in the Redwall Limestone, which is bleached, brecciated and marbleized below the overlying
Grandview_Mine
Summit in the Grand Canyon, Arizona
Butte, upon the Supai Group, until the trail drops down through the Redwall Limestone, at the Supai ridgeline terminus. Cardenas Butte and Escalante Butte
Cardenas_Butte
Landform in the Grand Canyon, Arizona
Pennsylvanian-Permian Supai Group. Further down are strata of Mississippian Redwall Limestone, Cambrian Tonto Group, and finally Proterozoic Unkar Group at creek
Angels_Gate
(Triassic); Redwall Limestone, Arizona (Mississippian); Coeymans, Keyser, and New Creek limestones, Pennsylvania (Devonian); Edgecliff Limestone, New York
Encrinite
Perennial stream in Arizona, US
the canyon cuts through Paleozoic sedimentary rocks including the Redwall Limestone, Naco Group, Supai Group, Schnebly Hill Formation, Coconino Sandstone
Fossil_Creek
Landform in the Grand Canyon, Arizona
Group. Further down are strata of the cliff-forming Mississippian Redwall Limestone, and Cambrian Tonto Group. According to the Köppen climate classification
Grand_Scenic_Divide
Landform in the Grand Canyon, Arizona
This isolated butte is an erosional remnant composed of Permian Kaibab Limestone and Coconino Sandstone. This sandstone, which is the third-youngest stratum
Mount_Sinyella
Cambrian geologic formation found in the Southwestern United States
slopes that rise from the Tonto Platform to cliffs formed by limestones of the Muav Limestone and dolomites of the Frenchman Mountain Dolostone. In 1875
Tapeats_Sandstone
Rock formation in the Grand Canyon, Arizona, United States
Pennsylvanian-Permian Supai Group overlaying cliff-forming Mississippian Redwall Limestone, which in turn overlays slope-forming Cambrian Tonto Group. Precipitation
Alsap_Butte
Landform in the Grand Canyon, Arizona
the Redwall Limestone. Across the Colorado River and just downstream from Plateau Point, is the Tower of Set, with its beautiful points of Redwall Limestone
Plateau_Point
Sequence of sedimentary strata
Plateau). The base of the largely flat-topped Redwall Limestone monolith sits upon cliffs of Muav Limestone, then Bright Angel Shale, and Tapeats Sandstone
Grand_Canyon_Supergroup
REDWALL LIMESTONE
REDWALL LIMESTONE
Boy/Male
English
Variants of Randolph 'Wolf's shield.' Surname.
Surname or Lastname
English
English : variant of Randall.English : variant spelling of Rendall 2.
Surname or Lastname
English (chiefly East Anglia)
English (chiefly East Anglia) : apparently a habitational name from an unidentified place, perhaps named with the Old English personal name Hroda (see Rodney) + Old English well(a) ‘spring’, ‘stream’.
Boy/Male
Anglo Saxon
Name of a king.
Surname or Lastname
English
English : from an Old English personal name, either Rǣdweald or Rǣdwulf. The first element in each is rǣd ‘counsel’, ‘advice’; the final elements are weald ‘rule’ and wulf ‘wolf’.English : topographic name, from Old English (ge)ryd(d) ‘cleared’ + weald ‘woodland’, ‘high woodland subsequently cleared’.
Surname or Lastname
English
English : habitational name from Beadnell in Northumberland or Bednall in Staffordshire, both named with the genitive case of the Old English personal name Bēda + Old English halh ‘nook’.
Boy/Male
American, Australian, British, English
Wolf's Shield; Variants of Randolph; Surname
Surname or Lastname
English
English : variant spelling of Edsall.
Boy/Male
American, Anglo, British, English
Strong Counsel
Surname or Lastname
English
English : habitational name from Yearby in Cleveland (formerly in North Yorkshire), which Ekwall derives from Old Scandinavian Efribýr ‘upper village or homestead’.
Boy/Male
American, British, English
Sea Powerful
Surname or Lastname
English
English : variant of Randall.Scottish (Orkney) : habitational name from Rendall in Orkney.Probably also an Americanization of Swedish Rendahl.
Surname or Lastname
English
English : habitational name from a place called High Edser in Ewhurst, Surrey.It is possible that in some cases the name may be an Americanized form of the German family name Etzel.
Boy/Male
American, British, English
Lives by the Spring Near the Road
Surname or Lastname
English
English : habitational name from Trowell in Nottinghamshire, named in Old English with trēow ‘tree’ + wella ‘stream’. Ekwall suggests that this may have referred to a tree bridge. Compare Trowbridge.
Surname or Lastname
English
English : variant of Bidwell.
Boy/Male
American, British, English
Wealthy Ruler
Surname or Lastname
English
English : variant of Sewell.Samuel Sewall (1652–1730) came with his parents from Bishop Stoke, Hampshire, England, to Newbury, MA, as a nine-year-old boy. In 1676 he married Hannah Hull, a wealthy heiress, and in 1681 he was appointed printer to the Council in Boston. He served as a judge in the infamous Salem witchcraft trials of 1692—the only one of the judges to admit publicly that he had been wrong. In 1700 he published The Selling of Joseph, which argues that all men are created equal and presents theological arguments against slavery.
Surname or Lastname
English
English : habitational name from Ledwell in Oxfordshire, named in Old English as ‘loud spring’ or ‘loud stream’, from Hl̄de (a river-name derived from hlūd ‘loud’, i.e. ‘roaring stream’, ‘torrent’) + wella ‘well’, ‘spring’, or ‘stream’.
Boy/Male
Australian, British, English
From the New Hall
REDWALL LIMESTONE
REDWALL LIMESTONE
REDWALL LIMESTONE
REDWALL LIMESTONE
REDWALL LIMESTONE
REDWALL LIMESTONE
REDWALL LIMESTONE
n.
The European bee-eater. See Bee-eater.
n.
The gadwall.
n.
The American redpoll warbler (Dendroica palmarum).
n.
A large duck (Anas strepera), valued as a game bird, found in the northern parts of Europe and America; -- called also gray duck.
n.
The European redstart.
n.
Recall.
v. t.
To recall; to call back.
n.
The gadwall.
v. t.
To call back to mind; to revive in memory; to recollect; to remember; as, to recall bygone days.
n.
Any one of several species of small northern finches of the genus Acanthis (formerly Aegiothus), native of Europe and America. The adults have the crown red or rosy. The male of the most common species (A. linarius) has also the breast and rump rosy. Called also redpoll linnet. See Illust. under Linnet.
n.
A plant formerly valued for its restorative qualities (Valeriana officinalis, or V. Pyrenaica).
n.
The common European linnet.
n.
Same as Redpoll.
v. i.
To recall an oath.
v. t.
To revoke; to annul by a subsequent act; to take back; to withdraw; as, to recall words, or a decree.
v. t.
To call back; to summon to return; as, to recall troops; to recall an ambassador.
n.
Recall, as from exile.
n.
Recall, as from banishment.
v. t.
To recall, as former laughter.
n.
The red-tailed hawk.